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On page 1, the arrows are red for surface currents and blue for deep currents. The colors are a bit hard for me to see, but note that in the North Atlantic, a surface current flows north and a deep current flows south. This means that deep water forms in the North Atlantic.
Gulf Stream, warm ocean current flowing in the North Atlantic northeastward off the North American coast between Cape Hatteras, N.C., U.S., and the Grand Banks of Newfoundland, Can. In popular conception the Gulf Stream also includes the Florida Current (between the Straits of Florida and Cape
Jul 18, 2018 · The Atlantic Meridional Overturning Circulation, or AMOC, is a conveyor belt that brings surface water northward in the Atlantic; from there, the heavier salty water sinks and returns at depth from the Labrador and Nordic seas, near the North Pole, all the way south to the Southern Ocean. Most people are interested in what happens at the ...
Upwelling is an oceanographic phenomenon that involves wind-driven motion of dense, cooler, and usually nutrient-rich water from deep water towards the ocean surface, replacing the warmer, usually nutrient-depleted surface water. The nutrient-rich upwelled water stimulates the growth and reproduction of primary producers such as phytoplankton.
Vertical movement of cold deep water rich in nutrients and oxygen to the surface. Associated with high productivity. Can occur in high latitude areas, as the lack of a pynocline allows significant vertical mixing.
Dec 26, 2016 · And there are nearly 1,3 billion cubic kilometres of water in the ocean. But, with a surface area of 362 million km2 the top layer of the oceans (the upper 200 meters) 'only' has a content of 72.4 million km 3. Most ocean water (95%) is cold 'deep water'. There is a considerable mixing of water masses in the top layer of the ocean.
the surrounding warm water and so it sinks to the bottom. The sinking icy water moves the warm water ahead of it and causes a current that moves the pepper grains on the bottom of the tank. B. Relation to Ocean Motion The ocean waters near the equator are heated directly by the sun's rays. Waters at the poles
Jun 24, 2020 · The current water depth has been fairly stable the last couple of days and is at 578.93 feet msl as of this report. The surface water temperature is in the upper 70s to low 80s. The water is clear with a slight stain, which Lou says, "is typical this time of year with the warmer water. Happy fishing and see you on the lake."
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Jul 15, 2000 · According to his own ocean models, he says, cold water could sink because its own weight in the North Atlantic and settle comfortably in the deep sea. Then, it would drift into the Drake Passage, 1,000-km-wide waterway connecting the Atlantic and Pacific Oceans between South America and the Antarctic Peninsula.
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Apr 24, 2018 · These are two of Antarctica's fastest-melting regions, and no wonder: When cold surface water no longer sinks into the depths, a deeper layer of warm ocean water can travel across the continental shelf and reach the bases of glaciers, retaining its heat as the cold waters remain above.
Dense-cold-salty water sinks to the ocean bottom. Surface water flows in to replace the sinking water, which in turn becomes cold and salty enough to sink. This "starts" the global conveyer belt, a connected system of deep and surface currents that circulate around the globe on a 1000 year time span. This global set of ocean currents is a critical part of Earth's climate system as well as the ocean nutrient and carbon dioxide cycles.
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Apr 08, 2019 · Flowing northward near the surface, it transports warm, salty water from near the equator into the latitudes near Greenland and northern Europe. Here, it hits colder water from the Arctic, becomes...
A current can also change somewhat in depth and speed over time. Surface ocean currents can be very large. The Gulf Stream, a surface current in the North Atlantic, carries 4500 times more water than the Mississippi River. Each second, ninety million cubic meters of water is carried past Chesapeake Bay (US) in the Gulf Stream. Surface ocean ...
Where would you expect surface water to sink and initiate a deep water current in the atlantic ocean
The Atlantic Ocean is the second-largest of the world's oceans, with an area of about 106,460,000 km 2 (41,100,000 sq mi). It covers approximately 20 percent of Earth's surface and about 29 percent of its water surface area. It separates the "Old World" from the "New World".
Mar 18, 2019 · Warm water is heated by the Gulf Stream, a warm air current that originates in the Gulf of Mexico. The warm water then moves north, where it forces cooler water to sink and move south. As the...
The North Atlantic deep water trapped between the Antarctic bottom and intermediate waters rises to the surface in the area of the 60 degrees South divergence, As it reaches the surface it splits and parts Northward Identification of deep currents
This evaporating water leaves all its salts in the remaining water. This is why you feel a lot lighter when you swim in the Mediterranean than when you swim in the ocean: the water of the Mediterranean contains more salt than the water of the Atlantic (36 to 38 grams per litre in the Mediterranean against 34.9 in the Atlantic).
It then spreads slowly into the rest of the ocean. Other water must replace the surface water that sinks. This sets up the thermohaline circulation. The basic thermohaline circulation is one of sinking of cold water in the polar regions, chiefly in the northern North Atlantic and near Antarctica.
18.4 Ocean Water As everyone knows, seawater is salty. It is that way because the river water that flows into the oceans contains small amounts of dissolved ions, and for the most part, the water that comes out of the oceans is the pure water that evaporates from the surface.
Apr 26, 2001 · The Pacific Ocean on the West Coast has a greater expanse than the Atlantic Ocean on the East Coast. This means that the fetch (the distance over which the wind blows) is greater on the West Coast than on the East Coast. In this case, you can think of wave as a snowball: The farther you roll your snowball along in the snow, the bigger it gets.
As one goes deeper and deeper in the ocean, the pressure increases by 1.0*10^4 Pa for every meter below the surface. If a . asked by Erin on April 13, 2008; Physics. If you lay a steel needle horizontally on water, it will float. If you place the needle vertically into the water, it will sink. Explain why. It is because of surface tension.
The surface water in the North Atlantic region sinks to a depth of around 2000 metres due to convection. There it settles on an even denser deep-water layer from the Antarctic that extends down to the sea floor. As the cold and salty surface water sinks by convection, salty water flows in from nearby warmer regions, from the direction of the ...
The water, or hydrologic, cycle describes the pilgrimage of water as water molecules make their way from the Earth's surface to the atmosphere and back again, in some cases to below the surface. This gigantic system, powered by energy from the Sun, is a continuous exchange of moisture between the oceans, the atmosphere, and the land.
Given your understanding of the relationship between ocean water temperature, salinity, and density, where would you expect surface water to sink and initiate a deep-water current in the Atlantic Ocean? Explain your choice. floor TFc. Deep-ocean trenches are located mostly in the middle of ocean basins TF d. High evaporation rates in the subtropics (about 30 latitude) cause the surface-ocean water to have a lower-than-average salinity 10.
Apr 29, 2008 · At the earth's poles, when water freezes, the salt doesn't necessarily freeze with it, so a large volume of dense cold, salt water is left behind. When this dense water sinks to the ocean floor, more water moves in to replace it, creating a current. The new water also gets cold and sinks, continuing the cycle.
18.4 Ocean Water As everyone knows, seawater is salty. It is that way because the river water that flows into the oceans contains small amounts of dissolved ions, and for the most part, the water that comes out of the oceans is the pure water that evaporates from the surface. Mar 20, 2019 · Deep-water circulation changes lead North Atlantic climate during deglaciation. Nature Communications , 2019; 10 (1) DOI: 10.1038/s41467-019-09237-3 Cite This Page : The idea is that large flows of ice into the ocean in the North Atlantic cause freshening at the surface. This could then weaken Atlantic ocean circulation, lessen northward heat transport, and ... Deep-ocean currents are initiated by downwelling of cold, dense water near Antarctica and in the North Atlantic Ocean. c. Deep-ocean currents often travel faster than ocean surface currents. A primer on water. When you open the faucet you expect water to flow. And you expect it to flow night or day, summer or winter, whether you want to fill a glass or water the lawn. It should be clean and pure, without any odor.You have seen or read about places where the water doesn't have these qualities. May 14, 2019 · Throughout most of the time period, the Atlantic sector is the most intense carbon sink per unit area within the Southern Ocean and from 2012 onward, the CO 2 uptake per unit area in the Atlantic ... May 14, 2019 · Throughout most of the time period, the Atlantic sector is the most intense carbon sink per unit area within the Southern Ocean and from 2012 onward, the CO 2 uptake per unit area in the Atlantic ... Aug 21, 2014 · The cycle starts when saltier, denser water at the surface northern part of the Atlantic, near Iceland, causes the water to sink. This changes the speed of the huge current in the Atlantic Ocean... Jul 15, 2000 · According to his own ocean models, he says, cold water could sink because its own weight in the North Atlantic and settle comfortably in the deep sea. Then, it would drift into the Drake Passage, 1,000-km-wide waterway connecting the Atlantic and Pacific Oceans between South America and the Antarctic Peninsula. Upwelling is an oceanographic phenomenon that involves wind-driven motion of dense, cooler, and usually nutrient-rich water from deep water towards the ocean surface, replacing the warmer, usually nutrient-depleted surface water. The nutrient-rich upwelled water stimulates the growth and reproduction of primary producers such as phytoplankton. A current can also change somewhat in depth and speed over time. Surface ocean currents can be very large. The Gulf Stream, a surface current in the North Atlantic, carries 4500 times more water than the Mississippi River. Each second, ninety million cubic meters of water is carried past Chesapeake Bay (US) in the Gulf Stream. Surface ocean ... Apr 23, 2018 · And this, in turn, is blocking a process in which cold and salty ocean water sinks below the sea surface in winter, forming "the densest water on the Earth," in the words of study lead author ... Gulf Stream, warm ocean current flowing in the North Atlantic northeastward off the North American coast between Cape Hatteras, N.C., U.S., and the Grand Banks of Newfoundland, Can. In popular conception the Gulf Stream also includes the Florida Current (between the Straits of Florida and Cape Dec 26, 2016 · And there are nearly 1,3 billion cubic kilometres of water in the ocean. But, with a surface area of 362 million km2 the top layer of the oceans (the upper 200 meters) 'only' has a content of 72.4 million km 3. Most ocean water (95%) is cold 'deep water'. There is a considerable mixing of water masses in the top layer of the ocean. Ocean Stratification. The ocean composes 70.8% of the earth's surface. Sea water fills the basins separating the continents with an average depth of 3795 meters.The transition from the continental to the deep ocean or continental margins extend from the sea shore to around 2500 meters depth, it covers 40.7% of the ocean (29% of Earth surface). Aug 21, 2014 · The cycle starts when saltier, denser water at the surface northern part of the Atlantic, near Iceland, causes the water to sink. This changes the speed of the huge current in the Atlantic Ocean that circulates heat throughout the planet. "When it's heavy water on top of light water, it just plunges very fast and takes heat with it," Tung ... Jan 21, 2011 · The cold, salty water becomes dense and sinks to the ocean floor. This water is known as the North Atlantic Deep Water, and it is one of the primary driving forces of the conveyor belt. The force of the sinking, cold water pushes the existing North Atlantic Deep Water south, toward Antarctica, in a slow-moving underwater current. The idea is that large flows of ice into the ocean in the North Atlantic cause freshening at the surface. This could then weaken Atlantic ocean circulation, lessen northward heat transport, and ... Aug 21, 2014 · The cycle starts when saltier, denser water at the surface northern part of the Atlantic, near Iceland, causes the water to sink. This changes the speed of the huge current in the Atlantic Ocean that circulates heat throughout the planet. "When it's heavy water on top of light water, it just plunges very fast and takes heat with it," Tung ... Dec 26, 2016 · And there are nearly 1,3 billion cubic kilometres of water in the ocean. But, with a surface area of 362 million km2 the top layer of the oceans (the upper 200 meters) 'only' has a content of 72.4 million km 3. Most ocean water (95%) is cold 'deep water'. There is a considerable mixing of water masses in the top layer of the ocean. Upwelling is an oceanographic phenomenon that involves wind-driven motion of dense, cooler, and usually nutrient-rich water from deep water towards the ocean surface, replacing the warmer, usually nutrient-depleted surface water. The nutrient-rich upwelled water stimulates the growth and reproduction of primary producers such as phytoplankton. Apr 29, 2008 · At the earth's poles, when water freezes, the salt doesn't necessarily freeze with it, so a large volume of dense cold, salt water is left behind. When this dense water sinks to the ocean floor, more water moves in to replace it, creating a current. The new water also gets cold and sinks, continuing the cycle. 7. Given your understanding of the relationship between ocean water temperature, salinity, and density, where would you expect surface water to sink and initiate a deep-water current in the Atlantic Ocean? Explain your choice. 10. Pro fres ice, sali 8. Refer to the salinity-density experiment you con- of s ducted in Activity 10.4A. The reverse process, called downwelling, also occurs when wind causes surface water to build up along a coastline. The surface water eventually sinks toward the bottom. Subsurface water that rises to the surface as a result of upwelling is typically colder, rich in nutrients, and biologically productive. Apr 26, 2001 · The Pacific Ocean on the West Coast has a greater expanse than the Atlantic Ocean on the East Coast. This means that the fetch (the distance over which the wind blows) is greater on the West Coast than on the East Coast. In this case, you can think of wave as a snowball: The farther you roll your snowball along in the snow, the bigger it gets. Upwelling is an oceanographic phenomenon that involves wind-driven motion of dense, cooler, and usually nutrient-rich water from deep water towards the ocean surface, replacing the warmer, usually nutrient-depleted surface water. The nutrient-rich upwelled water stimulates the growth and reproduction of primary producers such as phytoplankton. Apr 26, 2001 · The Pacific Ocean on the West Coast has a greater expanse than the Atlantic Ocean on the East Coast. This means that the fetch (the distance over which the wind blows) is greater on the West Coast than on the East Coast. In this case, you can think of wave as a snowball: The farther you roll your snowball along in the snow, the bigger it gets.
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The cold water is now denser, due to the added salts, thus it sinks toward the ocean bottom. Surface water then moves in to replace the sinking water, thus creating a current. This movement within a fluid created by hotter (and therefore less dense) materials rising, and colder (and therefore denser) materials sinking, is called convection .
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Mar 23, 2015 · The Atlantic overturning is driven by differences in the density of the ocean water. From the south, the warm and hence lighter water flows northwards, where the cold and thus heavier water sinks ...
Firstly, let me give you a little basic knowledge about a property of liquids, then i'll proceed to the answer. As the temperature of a liquid/solid increases, its volume increases.
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Jul 15, 2000 · According to his own ocean models, he says, cold water could sink because its own weight in the North Atlantic and settle comfortably in the deep sea. Then, it would drift into the Drake Passage, 1,000-km-wide waterway connecting the Atlantic and Pacific Oceans between South America and the Antarctic Peninsula. - Rey's new yellow lightsaber toy
Deep-ocean currents are initiated by downwelling of cold, dense water near Antarctica and in the North Atlantic Ocean. c. Deep-ocean currents often travel faster than ocean surface currents.
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Feb 12, 2011 · Where in the Atlantic Ocean would you expect surface water to sink and initiate a subsurface flow? What are some reasons? Answer Save. 1 Answer. Relevance. Anonymous.
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The route of current is through the Atlantic Basin around South Africa and into the Indian Ocean and on past Australia into the Pacific Ocean Basin. If the water is sinking in the North Atlantic Ocean then it must rise somewhere else. This upwelling is relatively widespread.
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The reverse process, called downwelling, also occurs when wind causes surface water to build up along a coastline. The surface water eventually sinks toward the bottom. Subsurface water that rises to the surface as a result of upwelling is typically colder, rich in nutrients, and biologically productive.
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Oct 09, 2010 · Where in the Atlantic Ocean would you expect surface water to sink and initiate a subsurface flow? I'm stumped with this question. I do know that in order for the surface water to sink it needs to have a high density from either salinity or temp. But I don't know where and why it will initiate a subsurface flow. Can anyone help? Thanks - Ls1 timing curve
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As you might expect, surface water temperature varies considerably between the Equator and the poles. As the ocean water is distributed across the Earth's surface by drifts and currents (see the infrared satellite photo of the warm Gulf Stream moving north along the east coast of Florida), warm water from the lower latitudes is moved into the ... The global oceans are connected by deep currents (blue lines) and surface currents (red). Carbon from the atmosphere enters the ocean depths in areas of deep water formation in the North Atlantic and offshore of the Antarctic Peninsula. Where deep currents rise towards the surface, they can release "fossil" carbon dioxide stored centuries ago.
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Dec 02, 2019 · Here warm, salty Atlantic water ferried north from the tropics on the Gulf Stream meets the colder, fresher Arctic water. The mixture cools, and begins to sink and head back south. Apr 29, 2008 · At the earth's poles, when water freezes, the salt doesn't necessarily freeze with it, so a large volume of dense cold, salt water is left behind. When this dense water sinks to the ocean floor, more water moves in to replace it, creating a current. The new water also gets cold and sinks, continuing the cycle.
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Aug 21, 2014 · The cycle starts when saltier, denser water at the surface northern part of the Atlantic, near Iceland, causes the water to sink. This changes the speed of the huge current in the Atlantic Ocean that circulates heat throughout the planet. "When it's heavy water on top of light water, it just plunges very fast and takes heat with it," Tung ... As one goes deeper and deeper in the ocean, the pressure increases by 1.0*10^4 Pa for every meter below the surface. If a . asked by Erin on April 13, 2008; Physics. If you lay a steel needle horizontally on water, it will float. If you place the needle vertically into the water, it will sink. Explain why. It is because of surface tension.
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Gulf Stream, warm ocean current flowing in the North Atlantic northeastward off the North American coast between Cape Hatteras, N.C., U.S., and the Grand Banks of Newfoundland, Can. In popular conception the Gulf Stream also includes the Florida Current (between the Straits of Florida and Cape Given your understanding of the relationship between ocean water temperature, salinity, and density, where would you expect surface water to sink and initiate a deep-water current in the Atlantic Ocean? Explain your choice.
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Gulf Stream, warm ocean current flowing in the North Atlantic northeastward off the North American coast between Cape Hatteras, N.C., U.S., and the Grand Banks of Newfoundland, Can. In popular conception the Gulf Stream also includes the Florida Current (between the Straits of Florida and Cape Mar 18, 2019 · Warm water is heated by the Gulf Stream, a warm air current that originates in the Gulf of Mexico. The warm water then moves north, where it forces cooler water to sink and move south. As the...
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A current can also change somewhat in depth and speed over time. Surface ocean currents can be very large. The Gulf Stream, a surface current in the North Atlantic, carries 4500 times more water than the Mississippi River. Each second, ninety million cubic meters of water is carried past Chesapeake Bay (US) in the Gulf Stream. Surface ocean ... Nov 18, 2014 · Unlike the fast, isolated surface gyres, this deep ocean current travels all over the planet into every ocean basin. Eventually this cold water warms and is pushed to the surface where it starts the cycle again. Following this deep ocean current would be like riding a roller coaster that takes a thousand years from start to finish. Apr 29, 2008 · At the earth's poles, when water freezes, the salt doesn't necessarily freeze with it, so a large volume of dense cold, salt water is left behind. When this dense water sinks to the ocean floor, more water moves in to replace it, creating a current. The new water also gets cold and sinks, continuing the cycle.
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Apr 11, 2018 · The AMOC brings warm water from the equator up toward the Atlantic's northern reaches and cold water back down through the deep ocean. The current is partly why Western Europe enjoys temperate ... Water also sinks into the deep ocean off of Antarctica. Cold water (blue lines) sinks in the North Atlantic, flows along the bottom of the ocean and upwells in the Pacific or Indian. The water then travels in surface currents (red lines) back to the North Atlantic.
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Dec 26, 2016 · And there are nearly 1,3 billion cubic kilometres of water in the ocean. But, with a surface area of 362 million km2 the top layer of the oceans (the upper 200 meters) 'only' has a content of 72.4 million km 3. Most ocean water (95%) is cold 'deep water'. There is a considerable mixing of water masses in the top layer of the ocean. Deep-ocean currents are initiated by downwelling of cold, dense water near Antarctica and in the North Atlantic Ocean. c. Deep-ocean currents often travel faster than ocean surface currents. Winds drive ocean currents in the upper 100 meters of the ocean's surface. However, ocean currents also flow thousands of meters below the surface. These deep-ocean currents are driven by differences in the water's density, which is controlled by temperature (thermo) and salinity (haline). This process is known as thermohaline circulation.
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Deep-,Sea i~L.~eareh, 1961, Vo[. 7, pp. 265 to 275. Pergt~mon Press Ltd., London. Printed in Great lh'itain On the temperature, salinity, and density differences between the Atlantic and Pacific oceans in the upper kilometre* JOSEPH L. REID, Jr. Scripps Institution of Oceanography (Received 26 May 1960) Abstract--The surface of the Pacific Ocean stands about 40 cm higher than the Atlantic ... Pacific Ocean - Pacific Ocean - Temperature and salinity: The oceans tend to be stratified, the principal factor being temperature; the bottom waters of the deep parts are intensely cold, with temperatures only slightly above freezing. The surface zone, where temperature variations are perceptible, is between 330 and 1,000 feet (100 and 300 metres) thick. It is more compressed in the temperate ...
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Sep 30, 2020 · As the warm water comes in, colder, denser water sinks and begins moving south—eventually flowing along the bottom of the ocean all the way to Antarctica. This animation shows the Gulf Stream sending warm water to the North Atlantic Ocean, forcing colder water to sink and travel southward. Dense-cold-salty water sinks to the ocean bottom. Surface water flows in to replace the sinking water, which in turn becomes cold and salty enough to sink. This "starts" the global conveyer belt, a connected system of deep and surface currents that circulate around the globe on a 1000 year time span. This global set of ocean currents is a critical part of Earth's climate system as well as the ocean nutrient and carbon dioxide cycles.
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Jan 21, 2011 · The cold, salty water becomes dense and sinks to the ocean floor. This water is known as the North Atlantic Deep Water, and it is one of the primary driving forces of the conveyor belt. The force of the sinking, cold water pushes the existing North Atlantic Deep Water south, toward Antarctica, in a slow-moving underwater current. The North Atlantic deep water trapped between the Antarctic bottom and intermediate waters rises to the surface in the area of the 60 degrees South divergence, As it reaches the surface it splits and parts Northward Identification of deep currents Mar 20, 2020 · The salt you smell has to do with the salinity, or amount of dissolved salt, in the water. The Chesapeake Bay is an estuary—a partially enclosed body of water where fresh water from rivers and streams mixes with salt water from the ocean. About half of the water in the Bay comes from salt water from the Atlantic Ocean. But, in winter some lake surfaces can get very cold. When this happens, the surface water becomes more dense than the deeper water with a more constant year-round temperature (which is now warmer than the surface), and the lake "turns", when the colder surface water sinks to the lake bottom.
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Given your understanding of the relationship between ocean water temperature, salinity, and density, where would you expect surface water to sink and initiate a deep-water current in the Atlantic Ocean? Explain your choice.
Apr 08, 2019 · The deep water then circles back south, where much of it re-merges in the Southern Ocean, to release carbon back to the air. The journey takes place over decades to centuries.
Initiated in the North Atlantic Ocean, where warm water cools and sinks below the surface. This water moves southward as a subsurface flow and joins water near Antarctica. This deep water spreads into the Indian and Pacific Oceans, where it slowly rises and completes the conveyer as it travels along the surface into the NOrth Atlantic Ocean.


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Teach in a place where you'll never stop learning. Together, our students, schools, families and communities share an ambitious mission to create a future without limits. The only way to realize it is with talented educators like you. Shape the future by joining KIPP NYC today.
What Sets KIPP NYC Apart
Investment in People
Sustainable Work Hours
Voice & Professional Development
At KIPP NYC, we invest in your career as much as we invest in you as a person. Work-life balance is extremely important to us. We offer Wellness Wednesdays throughout the year, where teachers and students have a half day of school and get to enjoy activities that bring them joy. We also acknowledge our staff members with rewards for their time with us, including:
Longevity Compensation. After three years with KIPP NYC, teachers earn additional compensation in their annual salary.
All of Us Will Learn Award. Staff members have the opportunity to take a class or gain greater knowledge in an area of interest and get reimbursed up to $300, after completing three years at KIPP NYC.
We Remember, We Appreciate Sabbatical. After completing 10 continuous years at KIPP NYC, staff are eligible for an eight-week paid sabbatical.
As an organization, we are committed to striking a balance between the needs of our students, families, and staff. The feedback we received in focus groups with our school communities compelled us to re-evaluate how to make a school day more sustainable for students and teachers. Thus, we adjusted our schedule so that the school day starts between 7:45-8:00am and ends between 3:15-3:30pm. We will continue to have a longer school year than traditional public schools; however, the shorter day will give students more opportunities to engage in afterschool activities. It will also give staff more time at the end of the day for personal or work time.
KIPP NYC offers pay and benefits that reflect our appreciation for the invaluable role our educators play in lighting paths to opportunity for our students:
Competitive Salary. Our staff are compensated on an equitable salary scale that values experience in the classroom and New York State certification. Additionally, our compensation includes a longevity component that recognizes a commitment to KIPP NYC as an organization.
Generous Paid Time Off. Our staff enjoy 7-9 weeks of PTO depending on the role each calendar year! This includes a full week for the Thanksgiving holiday, winter holidays, and typical school breaks throughout the year.
Full Benefits. KIPP NYC provides full-time staff members with generous benefits along with multiple "Team and Family Rewards" based on longevity in the organization, including medical, dental coverage & vision benefits; mental health coverage; 403(b) employee match for eligible employees; gym reimbursement (inclusive of home workouts); and graduate school reimbursement
We honor the innate talent and hard-earned skill our teachers bring to KIPP NYC. Our leadership both listens to and advocates for teacher perspectives. We support educators with curriculum by content area and grade level; however, teachers have the freedom to design and tailor lesson plans for their students. Additionally, our school leaders are committed to being responsive to their teachers' perspectives on individual student needs.
KIPP NYC prides itself on providing growth opportunities for every staff member. We have established programs like Teacher in Residence (TIR) where we offer two career options that lead to full-time teaching roles and New York State certification. As a TIR, you'll work with KIPP's highest performing mentor teachers who consistently observe and provide actionable feedback to develop your teaching practice and nurture a growth mindset.
We also offer Emerging Leaders, Leaders Fellows, and Principals In Residence Leadership Development Programs to assist staff members in reaching their career aspirations. In these programs, participants develop leadership skills and competencies to continue in a leadership position or progress to the next step in their journey, including preparing to become a school principal.
At KIPP NYC, we are committed to building strategically diverse teams to serve our students, families, and staff. We recognize that we are better together and having both teachers and leaders that reflect our school communities results in better outcomes for students. Our Talent team ensures that there are equitable promotion processes in place for all leadership positions. Additionally, we've built out pipelines such as Emerging Leaders, Leader Fellows, and Principal In Residence to ensure that a diverse set of staff have opportunities to grow and succeed.
On each of our campuses, as well as within our central office staff, we prioritize diversity, equity, and inclusion training. This comes to life through targeted book studies and affinity group discussions. Our schools actively coach and train on culturally responsive teaching and restorative practices.
At KIPP NYC, we know that social-emotional learning is an important component of every child's education. To better help us meet the unique needs of each of our students, we employ a tiered approach to Social Work services. This includes weekly Advisory Group and daily grade-level community meetings, targeted affinity groups to help address shared needs, parent support groups, and individually tailored counseling for students.
Every single day I'm learning something different. Supporting all students is something that I hold near and dear to my heart. It's a lot of fun; it's really nice to be back.
KIPP NYC Alumna and Teacher
I was born and raised in the Bronx just like our students! KIPP staff are connected to our families and community on a personal level. We are committed to maintaining an equitable, predictable, and joyous environment for our community.
Ayiesha
KIPP NYC Dean
I work at KIPP because I have experienced a feeling of an extended family from everyone. The support I receive is nothing like I have experienced before. I am truly appreciative of the opportunity I have here at KIPP.
We have a very robust after school program at our middle schools. I coach and organize the KIPP Cup, a girls and boys basketball tournament against other east coast KIPP regions. I love it because after school and athletics present more opportunities to work with students.
I operate from a place of love. Children are with us K-16 and beyond so the partnership between families, teachers, and students are aligned around a mission for students to achieve maximum success.
Hericka
KIPP NYC Social Worker
At KIPP, we believe that a quality education expands the mind, leans on the heart, and moves the body. Our students will be critical thinkers and the empathetic leaders of tomorrow.
We are committed to ensuring not only student success, but also to helping students create their own vision of success. At KIPP, we are shaping future thinkers, advocates, and trailblazers.
Syon
We don't think of SEL as a need only for students. It is a collective experience for students, families, teachers and staff, especially during a time where it has been challenging to be a helper emotionally
Wilza
Who doesn't love math? As a founding teacher, I wanted to continue to impact a community that looks like me, teach a subject, math, that I love, and do this work alongside a team that has shared beliefs and values as I do.
Yanet
KIPP NYC Principal in Residence
KIPP NYC's Core Values
We seek educators who possess the personal and professional characteristics that align with our Core Values.
We Believe.
We believe in the infinite potential of all people. Our hope, faith, and optimism fuel our daily work and drive us toward achieving a more equitable and just world, starting with our KIPPsters.
All of Us Will Learn.
We know excellent instruction means teaching the whole child and the whole class. We believe student achievement is the product of adult learning and development. Together all KIPP students – big and small – intellectually prepare, practice, teach, and assess in order to maximize our individual and collective potential.
Commitment to Excellence.
We believe excellence is a sustained pursuit, not an endpoint. We own the results we achieve. We assert that excellence is often the 1/12th between good and great. We strive for excellence in all things.
Teach Like Harriett.
KIPP was founded on the inspiration of Harriett Ball, and the understanding that great teaching is fundamental to great schools. Like Harriett, we cultivate joy and love of learning with high expectations for academic work. We believe Math is Life, Reading is Freedom, and Knowledge is Power. We measure our success by student mastery and alumni outcomes.
Team & Family.
We work in schools and communities, not classrooms. We believe team always beats individual. We contribute to and are responsible for group success. Like a family, we act with empathy and support one another to build strong relationships. We never give up on our Team & Family.
Find a Way or Make One.
We persist in the face of challenges and creatively seek solutions. We cultivate critical and divergent thinking in ourselves and others to achieve our goals. We work to achieve transformational outcomes through enduring alliances and a humble commitment to find, learn, and share what is best for students and alumni.
Revolutionary Love.
We believe extraordinary school communities are built from love. The love we have for ourselves, our teammates, and our communities drives the courageous change we need to leave the world better than we found it.
Build a Better Tomorrow.
We know our KIPPsters, past, present, and future, are the leaders of a better tomorrow, so we work to empower, prepare, and embolden them to lead choice-filled lives. We take action to dismantle systems of oppression and construct a society that is defined by equity and restorative justice.
We Remember. We Appreciate.
We remember and appreciate where we have come from in order to know where we are going. We look honestly at our past and present to plan our future. We believe our staff, our families, and our students are our greatest strength.
Hear directly from the voices that make up the KIPP NYC community and read about the incredible ways KIPP NYC is making a difference in the future of our students.
Get Career Updates from KIPP NYC
About once a month, you'll get KIPP news and opportunities in your inbox.
Let's Get Started. Apply to Work With Us.


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SolarCity's Insider-Heavy Bond Offering Provides Fodder for Bulls and Bears Alike
Musk and two SolarCity execs will purchase $100M of a $124M debt sale, raising concern that the market is unwilling to provide the solar company with further funding.
Lou Whiteman
Aug 24, 2016 11:18 AM EDT
Elon Musk and other key figures at SolarCity Corp. (SCTY) have committed to buy $100 million of the solar panel installation company's debt ahead of its planned $2.6 billion acquisition by Musk's Tesla Motors (TSLA - Get Report) .
SolarCity in a regulatory filing late Tuesday said that Musk has committed to buy $65 million of a previously-announced $124 million "solar bond" offering, while SolarCity CEO Lyndon Rive and chief technology officer Peter Rive are to buy $17.5 million apiece. Musk in addition to serving as CEO of Tesla is chairman of SolarCity, and the Rives are Musk's cousins.
San Mateo, Calif.-based SolarCity provides commercial and residential solar panel installation at little to no upfront cost, recovering its costs via monthly payments and sales of unused electricity back to the grid. The business is debt-intensive, with SolarCity listing $3.25 billion in borrowings on its balance sheet as of June 30.
The company has struggled to break even in recent quarters, and prior to Tesla's acquisition announcement some had questioned whether SolarCity would be able to continue to fund its obligations. The deal, involving two companies that count Musk as the largest shareholder, was met with criticism by some but the companies attempted to mitigate concerns by recusing directors with ties to both sides from deliberations and requiring approval by non-affiliated shareholders.
The latest bond sale, which was disclosed concurrent to Tesla's high-profile announcement of a new vehicle battery that should provide better performance, is sure to raise additional eyebrows. Company bulls are likely to see the insider purchase as a vote of confidence, while bears will read it as a sign of the market's tepid interest in buying additional SolarCity borrowings.
The bond deal is believed to be the first time Musk has invested in SolarCity bonds directly, though a third Musk-affiliated company, privately-held Space Exploration Technologies Corp., bought about $90 million of a $105 million debt issuance last year and an additional amount of SolarCity debt earlier this year.
Oppenheimer managing director Colin Rusch, appearing on CNBC Wednesday morning, said he is concerned by the apparent lack of demand for the SolarCity bonds and by "the relationship between SolarCity and Tesla and the return on equity for the Tesla investors here."
Rusch said the hope for Tesla post-deal is that the company is "robust enough" to manage SolarCity's cash needs, noting that there is potential for "significant cash flow off the auto platform." But Tesla also has significant cash needs of its own as it attempts to bring its more affordable Model 3 to market and build out its global retail and charger networks, leading some to predict the company is likely to issue more shares in the quarters to come.
Tesla already tapped public markets once this year, raising more than $1 billion to fund operations in a May secondary.
Ahead of the merger SolarCity is taking steps to cut expenses. The company Wednesday told California officials it intends to lay off more than 100 workers beginning in mid-October, with most of the cuts focused on back-office, legal and accounting functions that presumably can eventually be taken over by Tesla employees.
InvestingStocksTransportationAutomobile ComponentsUtilitiesBondsTechnologyIndustrial GoodsEnergyMergers and Acquisitions


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Mastering predictive modeling to improve patient care
By: Elizabeth Wood
The Best in OR Business Award is presented annually at the OR Business Management Conference to recognize an outstanding leader who has saved on costs, increased OR utilization, improved patient safety, or otherwise streamlined the surgical services department.
Vikram Tiwari, PhD
The 2020 award will be presented to Vikram Tiwari, PhD, associate professor of anesthesiology, biomedical informatics, and management at Vanderbilt University School of Medicine and Vanderbilt University, as well as director, surgical analytics, at Vanderbilt University Hospital. Since joining Vanderbilt in 2012, he has demonstrated skills in leadership and innovation that meet the criteria for the award.
"My interest in healthcare developed during my doctoral studies and led to my thesis on coordination and capacity management in hospitals," Tiwari says. With a doctorate in operations management and decisions sciences from Indiana University Bloomington, as well as engineering and MBA degrees, Tiwari has helped OR leaders at Vanderbilt better understand how to use data to inform decision making and increase efficiency.
Power of predictive analytics
"Thanks in large part to his expertise in predictive analytics and passion for serving patients, we can much more efficiently tailor our operating room staffing levels to our case volume," notes C. Wright Pinson, MD, deputy chief executive officer (CEO) at Vanderbilt University Medical Center (VUMC) and CEO of Vanderbilt Health System. "This has made a significant difference in our organization and serves as a best practice for hospitals throughout the country."
Cindy Kildgore, MSHA, RN, CNOR, perioperative services director at VUMC, echoes that praise. She told OR Manager that Tiwari built and maintains data sets within Tableau, such as first case on-time starts, turnover times (by hour of the day, as well as the components of turnover time), and financial cost per case/per surgeon. "He has significantly impacted our ability to increase our volume with sufficient knowledge of future needs," she says.
"At VUMC, we thrive on innovation, and leaders encourage and support new ideas," Tiwari says. Having that culture helped ease the way for adoption of advanced analytical methods.
"The predictive modeling we have done to predict our daily surgical volume has helped many different departments in our hospital," he says. The model, constructed in 2013, has recently been updated to reflect the surgical volume that is now higher than when the model was first used. "We are also now able to predict case volume very accurately up to 30 days out," he adds. "We have separate models for each day of the week, as well as for each of the 30 days into the future."
Tiwari's predictive analytics, Kildgore says, have been used to help shift outpatient volume off site. Tiwari used simulation modeling to determine how many ORs could be accommodated in this new ambulatory surgery center without compromising the holding room (HR) and postanesthesia care unit (PACU). "That work proved that we can have one additional OR in lieu of fewer HR/PACU beds," he says.
Tiwari notes that implementing any process change requires demonstrating that the new process will create less, not more, manual work, and that it won't inadvertently overload some other part of the system. "Seeing through the lens of systems thinking when crafting changes helps get better buy-in from the affected stakeholders," he explains. "We also rely on validated data metrics and measurements for effective monitoring of improvements in performance."
In addition to his data analytics work, Tiwari is a researcher who has published extensively, and he teaches courses in healthcare operations management and healthcare analytics to MBA students. "The inspiration for my research and teaching comes from real issues of capacity management planning and process efficiencies faced by our hospital that I work on intricately," he notes.
He sees analytics as a way to achieve better care for patients. "The most rewarding accomplishments are those where some aspect of my analysis helps these people," he says.
"We have just started to scratch the surface of the analytics toolkit," Tiwari adds. "Most of what we still do will be described as 'descriptive analytics,' that is, reporting data retrospectively. I want to develop tools for predicting future states to help decision makers proactively improve resource usage. I also want to leverage organizations like OR Manager to help spread the word on the potential of using scientific techniques to better manage an organization's capacities and capabilities."
He believes that continuously learning and staying curious are important for success. His advice for aspiring leaders? "Those who show a positive attitude, are team players, take the initiative, and are ready to challenge themselves tend to stand out," he says.
These characteristics are reflected in Tiwari's many accomplishments and have earned him the admiration and respect of colleagues and leaders at Vanderbilt. True to form, Tiwari not only is a past presenter at both the annual OR Manager Conference and the OR Business Management Conference, he also is presenting "The Power and Perils of Data Analytics" on January 29—the same day he will receive the Best in OR Business Award.
To learn more, visit www.ormanager.com/managementconference. ✥
Making Enhanced Recovery the Norm, Not the Exception
After this session you'll be able to: Understand how a value-based LEAN process can positively impact the introduction of an enhanced recovery program. Develop strategies to implement use of enhanced…
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SpaceX hopes to resume launches in November
Falcon 9 launch. Photo: SpaceX
SpaceX does not plan to stop launches for 9-12 months, as the United Launch Alliance estimated . A week ago, the head of a rival company, Tori Bruno, suggested that the explosion of the Falcon 9 launch vehicle would disrupt the SpaceX flight schedule for the next 9-12 months due to a lengthy investigation into the causes of the incident. This could cause a strong SpaceX reputational damage. Some customers could go to competitors.
But the company Ilona Mask, perhaps, will recover from the strike much earlier. SpaceX may resume flights in November 2016, said company president Gwynne Shotwell.
"We expect ... a stop for about three months with the resumption of flights around November," said Gwynn Shotwell during a video call on September 13 at the World Satellite Business Week conference in Paris. A video of her performance was posted on Youtube , and she was shot by a reporter for the German business magazine WirtschaftsWoche .
Shotwell said nothing about whether any missile repairs are required [probably meant refining the design] in order to return to the launches in November. She did not report on the extent of damage to the launch platform and ground support equipment, but the launch platform at the explosion site is unlikely to be repaired before November. Therefore, the November launch, if it takes place, will occur from another launch pad - either from the Vandenberg Air Force Base (LC-4E), or from the territory of the A. Kennedy Florida (LC-39A).
The explosion on September 1 destroyed the communications satellite of the Israeli company Space Communication worth $ 200 million. Shotwell saidthat experts still could not establish the cause of the explosion. It is not clear even the cause of a rocket or ground equipment. After the explosion, Ilon Musk said that "this is the most difficult failure in 14 years of the company's operation."
Earlier, SpaceX reported that it had almost prepared a second launch pad for the LC-39A in Florida, in the territory of the Yevgeny Space Center. Kennedy. It should be finished in November. This launch pad was last used five years ago to launch NASA shuttles. True, the deputy. Director of the Center for Planning and Development of the Space Center. Kennedy Tom Engler (Tom Engler) said that SpaceX did not receive pre-orders for launch from this launch pad.
Launch pad 39A in Florida. Photo: SpaceX
Tom Engler also added that the September 1 incident from the NASA point of view does not change anything in the planning and preparation of launches.
At the same time, sources in SpaceX told Reuters that the first from the site of the Space Center. Kennedy will fly a non-heavy Falcon Heavy rocket, as previously planned, but a regular Falcon 9. It is not yet known whose cargo it will lift. Before the explosion on September 1, the next SpaceX client from the launch pad in Florida was to become the Luxembourg company SES SA with its satellite. And from a site in California in September they planned to raise the satellite Iridium Communications.
Falcon Heavy is a heavy-class booster with 27 engines that can deliver up to 54.4 tons to a low reference orbit, up to 22.2 tons to a geo-transfer orbit, and up to 13.6 tons to Mars. According to new information, the first test launch of Falcon Heavy was moved to the I quarter. 2017
In the list of outstanding orders SpaceX more than 70 missions, it must put into orbit equipment worth more than $ 10 billion. Before September 1, the Falcon 9 rocket made 27 successful launches and 1 failed.
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Home / Blog / Story Type / Blog / Special Education and the Covid-19 Pandemic
Special Education and the Covid-19 Pandemic
The uncertainty and evolving nature of the Covid-19 pandemic will require kindness, wisdom and cooperation as we move forward to safely educating our children now that everything has changed.
By Howard Mendelson
I've been practicing education law, on behalf of school districts and on behalf of parents throughout the great State of New Jersey, since I was admitted to practice law back in December of 1986 – over 33 years ago! The public's knowledge of and utilization of education lawyers, including special education lawyers, has grown exponentially over the past 33 years. Parents, students, administrators, and teachers have come to recognize the need for attorneys when addressing issues of and concerning education and, particularly, special education. Those entrusted with educating our youngsters have become increasingly reliant upon lawyers to help them reach consensus and, when necessary, litigate issues of and concerning their children. The good education lawyer is, however, always cognizant of the goal of any education law matter; whatever the respective positions might be, the good education lawyer remains "child-centered" when addressing an education law matter. The good education lawyer seeks to resolve issues and solve problems in a cost-effective "child-centered" manner. As one of the best-ever now retired school superintendents used to say, no matter what side you may be on, it should "always be about the youngsters!"
Everything Has Changed
With that in mind, I must here again proclaim what I taught to those lawyers, judges, teachers, administrators and/or parents "virtually" attending the first-ever presentation by the newly-formed Education Rights Section of the New Jersey Association of Justice at this year's Boardwalk Seminar from August 5 to August 7, regarding the undeniable realities of special education and the pandemic of 2020. Education and, especially special education, will never be the same! The post-virus world that we now live in has impacted not only general education, but has even more severely impacted special education. Physical presence, touch, redirection, physical therapy, behavioral skills, speech therapy, and parent-teacher interaction are even more vital in the context of special education. While the pandemic of 2020 has literally impacted everything; each one of us individually, each of our families, our communities, and perhaps, most importantly, our children and local school districts, perhaps no segment of our society has been more impacted than our children with special needs.
Every student with special needs is supposed to have an Individualized Education Program (hereinafter "IEP") developed by their local school district during the Spring of each school year and implemented by the local school district during the Summer and/or by the start of the next school year. Each students IEP is supposed to be completed by June 30 of each calendar year! Accordingly, from March to May, is generally "IEP season"; the time of year that administrators, teachers, parents, lawyers and advocates hopefully come together to develop IEP's for the upcoming school year; IEP's that the Individuals with Disabilities Education Act (IDEA) require provide each classified student with a "meaningful educational benefit" based upon goals and objectives developed by the Child Study Team and hopefully implemented during the prior school year. Needless to say, and while the Department of Education and each New Jersey school district have done their best to keep all concerned moving forward and revising/relaxing requirements in these strangest of times, many IEP's for next year have not in fact been addressed, modified and/or revisited as they would have been in a more typical school year; let alone implemented as and when contemplated when the parents met with their school districts and develop IEP's back in the Spring of 2019. As good as we education lawyers are, I have yet to see any provisions in any IEP addressing pandemics, school closures, virtual instruction, physical therapy during a lockdown, etc.
Special education concepts of "compensatory education", "extended school year" and "stay-put" protections (requiring that an existing IEP remain in place pending a dispute between a school district and parents) will accordingly become increasingly important as we move forward.
Special education concepts of "compensatory education", "extended school year" and "stay-put" protections (requiring that an existing IEP remain in place pending a dispute between a school district and parents) will accordingly become increasingly important as we move forward. Compensatory education; education designed to address any deficiencies in the program and placement previously provided to the concerned youngster, will perhaps become more of the norm, rather than the exception.
In the words of Aladdin and Jasmine, it truly is "a whole new world." While the Department of Education and local school districts have been issuing and modifying checklists and requirements for reopening of schools for the upcoming school year, the uncertainty and evolving nature of same will require kindness, wisdom and cooperation as we move forward to safely educating our children now that "everything has changed." Now, more than ever, school districts, teachers and parents, should review these checklists and requirements with their legal counsel and, hopefully, try to reach consensus rather than litigate issues of and concerning their children; as the IDEA requires, all concerned should be creative, flexible, and kind in trying to reach consensus toward a "child-centered" cost-effective recognition of the very unique circumstances we now find ourselves. We are way better together than we are a part and, in the context of special education matters, these very emotional matters are much easier to resolve when all concerned remember that it's "always about the youngsters."
Meanwhile, in both my professional and personal life, I shall do as the old Buddhist teaching suggests: I shall "remain opened to everything and attached to nothing." Indeed, from an education lawyer's perspective, true "wisdom" in these days may very well mean telling your client; parent and/or district, that you really do not know what will happen if and when schools open up this coming September. We will, however, within the confines of our existing law, do everything we possibly can to provide our children with the health, education and welfare they dearly deserve, we all wish to provide for them, and which our laws clearly require.
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Home > Our campaigns
Explore our major campaigns, investigations and analysis on important topics related to the work we do at Bolt Burdon Kemp. Many of our campaigns gain substantial news coverage and show how we're influencing the national conversations on topics such as child abuse, spinal injury and medical negligence.
Access To SEN Education UK
If you have a child with special educational needs and disabilities (SEN or SEND) or are simply interested in SEN education, you've probably realised there's a lot of information out there. But, while official facts and figures are available, wading through different guidelines, statistics and reports can be time consuming and confusing. So, we've mapped out a few key pieces of information.
Womens Health Hub
Women's reproductive health is a key component of a robust, productive society. So why is it so grossly neglected? With the help of consultant gynaecologist Dr Anne Henderson and a survey of British residents, we explore the financial, emotional and social realities of women's reproductive health.
Over 99% of all businesses in the UK are SMEs (small-to-medium enterprises). Yet, we found that 95% of SME owners don't know about the protections granted to disabled workers, which might explain why only half of people with disabilities are employed in the UK. Click through for the results of our proprietary study on SME owners' knowledge and uptake of the Equality Act 2010.
We tested London's public transport network to find out how well it caters for people in wheelchairs. Unfortunately, our results suggest wheelchair users often need to go the extra mile when commuting in London. Click through to learn more.
Cerebral Palsy Advice for Parents
Learning your child has cerebral palsy can be overwhelming. We created the Cerebral Palsy Advice Hub to try to answer some of the questions you might have. Read our informative articles helmed by experts in the field, covering the facts of the condition itself, life with cerebral palsy, and where to get help and support.
Crisis Point: A Day in A&E
Every year, the NHS winter crisis makes the headlines. But the truth is, A&E departments are immensely busy all year round. To showcase the difficulties of keeping one of the busiest NHS departments running smoothly, we've created an interactive challenge that puts you in the heart of A&E.
"Revenge porn" ruins lives Call it what it is: sexual abuse
In this expert Q&A video series, we answer your questions about "revenge porn", the nuances in the law, and the impact on victims.
Lost Heroines – when sexual harassment hits the military
In 2018, all British Armed Forces roles will finally be open to women. But as recent events have made clear, women still face inequality at work. The military is no different. In this feature we explore the heroic achievements of armed forces women and the workplace threats they've had to overcome.
Map reveals the extent of Scout leaders' child sex offences
Discover the true extent of the Scouts abuse scandal with our interactive map. Explore Scout leader convictions by name, area or associated Scout group, and discover information on each case.
Top 10 most significant advances in spinal injury repair
We take an in-depth look into the most significant advances in spinal injury repair, to find out what the future holds for those with these life-changing injuries.
Trust me I'm a doctor? The rise in misdiagnosis claims
In 2016/2017, the NHS paid out £1.024 billion for wrong, delayed and missed diagnoses. We explore the facts and figures behind the alarming rise in misdiagnosis claims.
Has Britain learned its lessons from the Falklands War?
More than 20 years on from the Falklands War, the MoD still isn't doing enough to protect servicemen from cold injuries. We explore the devastating effects of cold injuries, both then and now.
How to Keep your Brain Healthy
Looking for ways to keep your brain fighting fit? Discover the latest scientific research, and try these expert tips from a nutritional therapist, music therapist and yoga teacher.
Accessible Travel and Spinal Injury
Travelling abroad for the first time after you have suffered a spinal injury can be a daunting prospect. Here, Raquel Siganporia, who became paralysed herself, gives advice on planning an accessible holiday.
Brain Injury in the Workplace
Explore our expert guide for managers, employers and HR professionals, on how to support an employee returning to work after a brain injury.
Copyright 2018 Bolt Burdon Kemp.All Rights Reserved


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110819 Brevard County Sheriff's Department Crime Report
Brevard County Sheriff's Office
Jazmine Cannon, 18, of Mims, was arrested Oct. 24 and charged with possession of a controlled substance.
Brian McHale, 29, of Melbourne, was arrested Oct. 24 and charged with grand theft of a motor vehicle, possession of methamphetamine, and possession of drug paraphernalia.
Darryl Postier, 36, of Cocoa, was arrested Oct. 24 and charged with driving while license suspended with knowledge (habitual offender).
Nicholas Ramos, 22, of Palm Bay, was arrested Oct. 24 and charged with possessing/viewing material depicting child sex conduct.
Jeremy Rutledge, 34, of Tampa, was arrested Oct. 24 and charged with dealing in stolen property, and false verification of ownership to secondhand dealer under $300.
Bradley Swertfager, 22, of Palm Bay, was arrested Oct. 24 and charged with possession of a controlled substance, never obtaining a driver's license, and possession of drug paraphernalia.
Ronald Vandiver, 29, of Merritt Island, was arrested Oct. 24 and charged with possession of cocaine.
Petrice Williams, 52, of Mims, was arrested Oct. 24 and charged with false ID given to law enforcement officer, grand theft of a motor vehicle, and grand theft larceny over $300 and less than $5,000.
Nicole Brooks, 35, (homeless/address not listed), was arrested Oct. 24 and charged with possession of a controlled substance, possession of drug paraphernalia, possession of drug paraphernalia with residue, possession of drug paraphernalia/equipment.
Shawn Furie, 43, of Merritt Island, was arrested Oct. 24 and charged with petty theft larceny (3rd or subsequent offense).
Melissa Scott, 32, of Cocoa, was arrested Oct. 24 and charged with two counts of burglary of an occupied dwelling unarmed, loitering and prowling, two counts of petty theft larceny from building over $100 and less than $750 (1st degree), and resisting officer without violence.
Daquiri White, 38, of Titusville, was arrested Oct. 25 and charged with possession of cocaine, sale of cocaine, and use of two-way communication device to facilitate felony.
Bryan Acosta, 40, of Palm Bay, was arrested Oct. 26 and charged with false imprisonment as kidnapping, and battery.
Noah Carpenter, 28, of Merritt Island, was arrested Oct. 26 and charged with dealing in stolen property, and petty theft larceny (3rd or subsequent offense).
Stephanie Poff, 27, of Cape Canaveral, was arrested Oct. 26 and charged with possession of methamphetamine.
Pierce Chapman, 33, of Melbourne, was arrested Oct. 27 and charged with possession/viewing of material depicting child sex conduct.
Jacob Cook, 44, of Titusville, was arrested Oct. 27 and charged with driving under the influence (3rd violation within 10 years), and driving while license suspended with knowledge (3rd or subsequent offense).
Wanda Flonnery, 32, of Titusville, was arrested Oct. 27 and charged with battery on a law enforcement officer/firefighter/EMT.
Carrie Goodman, 40, of Cocoa, was arrested Oct. 27 and charged with possession of a controlled substance, driving while license suspended with knowledge, and possession of drug paraphernalia with residue.
Joseph Kelly, 34, of Cocoa, was arrested Oct. 27 and charged with possession of a controlled substance.
Adam Maman, 34, of Merritt Island, was arrested Oct. 27 and charged with sexual battery to victim over 12 years of age with weapon or force, and battery.
Jeremiah Merced, 40, of Merritt Island, was arrested Oct. 27 and charged with petty theft 2nd degree shoplifting (3rd or subsequent offense).
Kayla Osteen, 31, of Titusville, was arrested Oct. 27 and charged with grand theft shoplifting over $750 and less than $5,000, and resisting officer without violence.
Paul Ranslow, 54, of Cocoa, was arrested Oct. 27 and charged with burglary of an unoccupied conveyance unarmed, and petty theft 2nd degree from a motor vehicle (1st offense).
Randy Jones, 36, of Melbourne, was arrested Oct. 28 and charged with felony battery by strangulation as domestic violence.
Ernis Perez Valdez, 49, of Hialeah, was arrested Oct. 28 and charged with unlawful conveyance of fuel, and driving while license suspended with knowledge (1st offense).
Antonio Petty, 35, of Rockledge, was arrested Oct. 28 and charged with possession of a controlled substance, possession of drug paraphernalia, and resisting officer without violence.
Kevin Ward, 67, of Palm Bay, was arrested Oct. 28 and charged with battery on a person 65 years of age or older.
Lamonica Alexander, 42, of Palm Bay, was arrested Oct. 29 and charged with driving while license suspended with knowledge (3rd or subsequent offense).
Michael Augustine, 51, of Edgewater, was arrested Oct. 29 and charged with possession of a controlled substance, and possession of drug paraphernalia.
Antuwn Clark, 19, of Palm Bay, was arrested Oct. 29 and charged with cash deposit with intent to defraud, defrauding a financial institution, grand theft larceny over $300 and less than $5,000, and utterance of forged bill/check/draft or note.
Roshaunda Davis, 30, of Merritt Island, was arrested Oct. 29 and charged with aggravated assault as domestic violence.
Trevor Desrosiers, 35, of Titusville, was arrested Oct. 29 and charged with failure to register as a career criminal.
Timothy Helms, 48, of Merritt Island, was arrested Oct. 29 and charged with dealing in stolen property, false verification of ownership to pawnbroker, and petty theft shoplifting over $100 and less than $300 (1st degree).
Erin Kovell, 29, (address not listed), was arrested Oct. 29 and charged with possession of a controlled substance, possession of heroin, possession of drug paraphernalia, and violation of condition for felony pretrial release.
John Miranda, 27, of Titusville, was arrested Oct. 29 and charged with habitual traffic offender.
Jacqueice Witcher, 33, of Mims, was arrested Oct. 29 and charged with leaving the scene of a crash involving death.
Anita Crosby, 77, of Mims, was arrested Oct. 30 and charged with battery on a law enforcement officer/firefighter/EMT, driving under the influence, and resisting officer without violence.
Ellie Diaz, 46, of Orlando, was arrested Oct. 30 and charged with aggravated battery, and battery.
Andre Johnson, 34, of Mims, was arrested Oct. 30 and charged with failure to register changes in employment as sex offender, failure to report name or residence change as sex offender, and resisting officer without violence.
Jason Martin, 32, of Mims, was arrested Oct. 30 and charged with driving while license suspended with knowledge (3rd or subsequent offense), and possession of drug paraphernalia.
Ashlyn Primeaux, 19, of Merritt Island, was arrested Oct. 30 and charged with grand theft larceny over $300 and less than $5,000.
Brandon Roach, 20, of Satellite Beach, was arrested Oct. 30 and charged with felony battery by strangulation as domestic violence, battery as domestic violence, and false imprisonment as kidnapping.
Bianca Washington, 29, of Alachua, was arrested Oct. 30 and charged with fraudulent use of a credit card over $100 or more than twice in 6 months, and grand theft larceny over $750 and less than $5,000.
Richard Nevins, 34, of Merritt Island, was arrested Oct. 25 and charged with possession of methamphetamine, and possession of drug paraphernalia.
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Facebook Kills Daily Deals, But Keeps Check-In Deals
MG Siegler	@mgsiegler / 8 years
After quietly announcing they were killing off their nascent Deals product this afternoon, Facebook caused some confusion. You see, with the decision to kill off Facebook Places earlier in the week, everyone wondered what it meant for the location-based deals they launched alongside it? Those would remain alive, Facebook said at the time. But does today's execution change anything?
No, says Facebook. Daily Deals are separate from Check-in Deals. The Check-in Deals will work a bit different with the end of Places, but the company will continue to support and enhance that product. Daily Deals are dead — and my email account thanks them for that.
Facebook's statement on the matter:
After testing Deals for four months, we've decided to end our Deals product in the coming weeks. We think there is a lot of power in a social approach to driving people into local businesses. We remain committed to building products to help local businesses connect with people, like Ads, Pages, Sponsored Stories, and Check-in Deals. We've learned a lot from our test and we'll continue to evaluate how to best serve local businesses.
In more violent terms that may be easier to understand: they're killing off their Groupon-killer, but keeping half of their Foursquare-killer while killing off the other half of their Foursquare-killer.
Below, a reminder of what the still-alive Check-in Deals will look like on the Facebook iPhone app:


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Adventurer takes on New Zealand's original adventure race
Multisport (295)
Never one to shy away from a challenge, world-renowned mountaineer, adventurer and conservationist Holly Budge has her sights set firmly on the Kathmandu Coast to Coast.
Budge was the first woman to skydive off Mt Everest, to raise awareness of the African elephant crisis and raise charitable funds for her charity, How Many Elephants. She founded the charity six years ago while she was studying for a Masters in Sustainable Design.
The charity's mission is to stop the poaching of African elephants for ivory.
Budge is based in Franz Josef, a place she credits with providing the best possible training environment for the Coast to Coast.
"I've totally thrown myself into this and I'm very fortunate living in Franz, being able to get out on the kayak three to four times a week has been great."
Budge says the training for the Coast to Coast has been a different type of endurance than she's used to despite having scaled the highest and most technical mountains in the world and having a long career as a skydiver and filmer.
"Everest, for example, is a 60-day expedition, and when I did that, I'd had a few mountains under my belt so I knew what to expect. It's a long slog, but you're able to ease into it.
"The Coast to Coast is tough from the very beginning, where mountaineering is slow and methodical the Coast to Coast is going to be a full on two days and it's going to hurt."
However, Budge is confident her mental toughness will kick in when her body starts to tire.
"I'm always advocating in my talks, when you think you're done you're actually only at 75 percent.
"It's being able to rationalize, when your body is screaming you need to listen to that part of your brain that says keep going."
It's this perseverance and desire to push out of her comfort zone which is helping to drive Budge, even in her most difficult of the three disciplines.
A past scare in a whitewater rafting incident some years back has left Budge with an apprehension of fast-moving water.
"It was about 20 years ago, we got flipped out of the raft and I became trapped underneath it. The instructor had told me if this happens to find the air pocket. When I found the air pocket it was so tiny and I just couldn't breathe, suffering from asthma as well I really panicked."
Despite this, Budge says she has been enjoying learning how to kayak and gaining new skills and confidence. She's gained her grade 2 and has spent some time on the Waimakariri River already.
"This is definitely another adventure for me, I'm coming into it from ground zero. I'd never been on a road bike and the furthest I had ever run was 15km – I'm not a natural runner.
"I feel confident I can transfer the skills I've learnt in other extreme challenges to give me the persistence and sheer dogged determination I will need to pull this off. My motto is – think big, dream bigger."
Budge hasn't ruled out doing the Coast to Coast again – all going well she wouldn't mind having a crack at the longest day.
"People have said to me once you have done the Coast to Coast you're hooked."


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Wolff reveals Man Utd study in attempt to prevent Mercedes slump
Ewan Gale
Thursday 18 August 2022 04:00 - Updated: 13:01
Mercedes team principal Toto Wolff has revealed he has studied English football team Manchester United in an attempt to stave off a major slump.
Since Sir Alex Ferguson stepped down as manager of Man Utd in 2013, the once-dominant force of English football in the 1990s and 2000s has suffered testing times, winning one trophy since and zero Premier League titles.
The Silver Arrows similarly monopolised F1 in a stellar run between 2014 and last term, with 15 of 16 potential championships won - only Max Verstappen breaking the streak with the drivers' title last year.
Wolff hinted at walking away from the sport in the past two seasons before committing to his team - both in his team principal role and as a shareholder - and now faces the task of hunting down Red Bull and Ferrari after slipping to third-fastest in F1's new era.
Referring to the 13-time Premier League champions, Wolff told the Financial Times: "I studied why great teams were not able to repeat great title [runs],"
"No sports team in any sport has ever won eight consecutive World Championship titles and there are many reasons for that, and what is at the core is the human.
"The human gets complacent. You are not energised in the same way you were before. You are maybe not as ambitious.
"I often get the question: 'How hard is that?'
"I had so many periods, so many episodes in my life that I would judge as difficult, that this is not on the same scale.
"I don't think it's challenging in a way because I've had much harder times in all of my life, not particularly in Formula 1, but this is actually within my comfort zone."
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Over the last 50 years, the role of an archivist has adapted massively to include the collecting and processing of digital records. This page talks about what's involved in working with digital records and why we do it.
There are two type of digital record – Born Digital and Digitised. Born digital records are records which are created in a digital format- for example a word document, a spreadsheet, an audio file or a video file. These files are accessed via digital hardware such as laptops or desktop computers and unless they are created in a format that can be printed, they cannot be accessed outside of this environment.
Digitised records begin life in a physical format, like a book, a leaflet, VHS tape or cassette tape. A series of processes is applied to these items to create a digital version which can then be stored, preserved and accessed via digital hardware. We digitise these records for many reasons. One main reason is access. People all over the world can view a digital file online, whereas the same number will be unlikely to travel to an archive to view the original. The originals may be very fragile or damaged and digitising them will create a digital copy which can then be accessed to protect the original. In rare cases records are digitised for storage reasons where the physical items take up too much space but there is a desire to keep the information they contain.
Just like with physical collections, the most important thing when you start working on a collection is to know what you have. The UK National Archive have created DROID, a, free, easy to use tool which runs checks on a specified batch of files and produces a list of all the file formats contained in the file batch. If you can carry out this process, you have completed not only the first, but one of the most important steps in any digital preservation workflow. Droid and a user guide can be accessed and downloaded below.
DROID and User Guide Download
DROID uses a tool called PRONOM, which is a file format registry to identify your files. PRONOM can also be accessed and searched if you come a file format you are haven't seen before.
PRONOM is a file format registry or database in which we store information about different file formats, such as word documents, pdf or mp3. In PRONOM we try to describe some key information about each file format, the typical extensions used and, most importantly, we look inside the files and find patterns and information that can be used to identify file formats. In the same way that a signature can be used to identify an individual we call the information that identifies file formats signatures.
Why is this work important? For the same reason it is essential for a conservator to know if a physical record is vellum or paper, or if the materials used for writing are watercolour or iron gall ink. Digital preservation experts have to know what file formats are in their collection and what software can open them in order to effectively preserve them for future generations. PRONOM is used all over the world mostly in the fields of digital preservation, information management and digital forensics.
The information the PRONOM team and its contributors record is used by file format identification tools you may have used such as DROID, Freud or Siegfried. It can even come built into your preservation system.
There are now over 2000 file formats recorded in PRONOM but there is still a long way to go. We have a lot of help from contributors all around the world and have collaborated with around 100 institutions, ranging from archives and libraries, through to museums and educational institutions, and even private companies who are interested in the long-term preservation of digital records.
Learn more about PRONOM here.
If you would like to test your file format knowledge, our game, 'File Format or Fake' can be accessed below. .
FILE FORMAT OR FAKE GAME
For further help and support, the resources provided by the Digital Preservation Coalition, particularly the free to access Digital Preservation Handbook will provide a step by step guide for those new to working with digital records, or anyone keen to manage their own personal collections better.
DPC Resources


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Straughter Beats Buzzer Give Walsh 62-61 Win Over Hillsdale
Hillsdale (17-5, 11-4) 39 22 61
Walsh (15-5, 10-4) 30 32 62
Pts: Nick Czarnowski - 12
Reb: Nick Czarnowski - 9
Ast: Nate Neveau - 7
Pts: Darryl Straughter - 19
Reb: Chandler Vaudrin - 13
Ast: Chandler Vaudrin - 4
(NORTH CANTON, Ohio) – The last 15 seconds of Thursday evening's 62-61 victory over Hillsdale are some that won't be forgotten in a long time by the Walsh faithful. After a buzzer-beater broke the hearts of the Cavaliers (15-5, 10-4) on Tuesday, they rebounded with a buzzer-beater of their own to down the Chargers (17-5, 11-4) to make Alumni Arena erupt.
After Hillsdale inbounded the ball with 30 seconds left, the Chargers' Nate Neveau eventually drove the lane and dished off to Gordon Behr who was wide-open on the left block. At the last second, however, Bo Furcron was able to leave his man and meet Behr in the air and blocked what would have been a game-icing layup.
Darryl Straughter was able to pull in the rebound and drive up the court with under 10 seconds remaining. After a quick dish off to Chandler Vaudrin to reset, Straughter launced a 3-pointer from the left wing and found nothing but net and a 1-point win.
It was a spectacular ending to one of his best games of the season. He finished the night with a game-high 19 points on 7-of-9 from the field. He was 4-of-5 behind the arc.
He was joined in double figures by Furcron with 14 points and Vaudrin who added yet another double-double with 13 points and rebounds.
Naturally in games like this, nothing came easy for the Cavaliers who were down by as many as 14 in the game. That occurred after Neveau scored on a layup to make the score 36-22 with 4:07 left in the first half and forced Walsh to call a timeout.
Coach Jeff Young's call to attempt to get his crew refocused worked out as Walsh came out and started a 19-3 run that stretched into the second half and gave the Maroon and Gold a 41-39 lead after a Furcron layup.
Hillsdale eventually regained the lead and held it for the majority of the second, half, but momentum was now on the side of the Cavaliers.
The win avenged an early season loss to the Chargers back in December. Walsh will have an opportunity to do the same on Saturday when it hosts No. 11 Findlay. Tip-off with the Oilers is set for 1 p.m.


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You are at:Home»All News»Transport»Melbourne plan to remove cars from the city
Melbourne plan to remove cars from the city
August 6, 2018 Transport
An ambitious plan to make Melbourne more liveable by reducing the number of vehicles could serve as a blueprint to solve New Zealand's growing traffic woes
The Victorian city's transport officials are considering the impact of congestion and vehicles, with the number of people using the CBD grid expected to climb from 900,000 to 1.4 million by 2036.
Discussion papers released by the City of Melbourne have highlighted concerns relating to space, safety, congestion, pollution and cost when people choose to drive in the city, according to The Urban Developer.
Central Melbourne currently dedicates 460 hectares of space to parking, with 57% of street space in the municipality taken up by roads and 4% on-street parking.
Council Transport Portfolio Chairman Nicolas Frances Gilley argued that staggering population growth coupled with increased congestion meant major changes were needed.
"Our ambition is for a beautiful, liveable city where people can continue to enjoy all that Melbourne is famous for, our tree-lined streets, pedestrian thoroughfares and outdoor dining," Gilley said.
While driving creates congestion the issues continue once a vehicle is stopped, with major cities requiring a rethink on efficiency and optimisation.
"We need to optimise our city streets for people walking, cycling and taking public transport because that is how the majority of people move around and it's the most efficient way to move large numbers of people as our population grows," Gilley said.
The papers argue that spaces should be used for wider footpaths and bigger tram stops to more comfortably accommodate passenger increases.
"We need to change the way we think about car parking and ask ourselves if private vehicle storage is the best use of our most important public spaces."
Another issue identified is the inequality of car usage.
People on incomes over A$156,000 are more likely to drive to work but are also more likely to live in areas well-serviced by public transport.
Around the world, large-scale infrastructure changes are taking place.
In San Francisco a dynamic new pricing system has been implemented for on-street parking – resulting in a 50% reduction in drivers.
New York and London have also decreased dependence on cars after converting major road space to pedestrian zones and bicycle lanes to improve safety and decongest the cities major arteries.
"Discouraging through traffic, providing high-quality alternatives to driving and supporting vehicle sharing and car-pooling could be other solutions to reducing car dependence and congestion."
It also suggested that streets in the CBD grid be reduced to one lane each way, with the spare lanes being converted into space for cyclists, pedestrians and public transport users.
A draft Transport Strategy will be released later this year.
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