what does the first word mean?
It  is the development and strengthening of cyclonic circulations in the atmosphere results in the formation of low pressure area
Introduction
Cyclogenesis is the development or strengthening of cyclonic circulation in the atmosphere (a low-pressure area). Cyclogenesis is an umbrella term for at least three different processes, all of which result in the development of some sort of cyclone, and at any size from the microscale to the synoptic scale.
we would expect what with low pressure in the northern hemisphere 234 significant extratropical cyclones form each winter how does a low pressure area form? Cyclogenesis is the development and strengthening of cyclonic circulations
Cyclonic circulations, or low-pressure areas, Cyclogenesis is an umbrella term for several different processes, all of which result in the development of some sort of cyclone. It is the development or strengthening of cyclonic circulation in the atmosphere (a low-pressure area) It is the development or strengthening of cyclonic circulation in a low-pressure area.
Low-pressure area Cyclogenesis Cyclogenesis
Formation Introduction Introduction
Cyclogenesis is the development and strengthening of cyclonic circulations, or low-pressure areas, within the atmosphere. Cyclogenesis is the opposite of , and has an anticyclonic (high-pressure system) equivalent which deals with the formation of high-pressure areas—anticyclogenesis. Cyclogenesis is an umbrella term for several different processes, all of which result in the development of some sort of cyclone. Meteorologists use the term "cyclone" where circular pressure systems flow in the direction of the Earth's rotation, which normally coincides with areas of low pressure. The largest low-pressure systems are cold-core polar cyclones and extratropical cyclones which lie on the synoptic scale. Warm-core cyclones such as tropical cyclones, mesocyclones, and polar lows lie within the smaller mesoscale. Subtropical cyclones are of intermediate size. Cyclogenesis can occur at various scales, from the microscale to the synoptic scale. Larger-scale troughs, also called Rossby waves, are Cyclogenesis is the development or strengthening of cyclonic circulation in the atmosphere (a low-pressure area).  Cyclogenesis is the development or strengthening of cyclonic circulation in the atmosphere (a low-pressure area). Cyclogenesis is an umbrella term for at least three different processes, all of which result in the development of some sort of cyclone, and at any size from the microscale to the synoptic scale.
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Cyclogenesis [SEP] Introduction
Cyclogenesis is the development or strengthening of cyclonic circulation in the atmosphere (a low-pressure area). Cyclogenesis is an umbrella term for at least three different processes, all of which result in the development of some sort of cyclone, and at any size from the microscale to the synoptic scale. The process in which an extratropical cyclone undergoes a rapid drop in atmospheric pressure (24 millibars or more) in a 24-hour period is referred to as explosive cyclogenesis, and is usually present during the formation of a nor'easter. The anticyclonic equivalent, the process of formation of high pressure areas, is anticyclogenesis.