where do low pressure areas form?
It forms where the air pressure is lower than that of surrounding locations
Introduction
A low-pressure area, low area or low is a region where the air pressure is lower than that of surrounding locations. Low-pressure systems form under areas of wind divergence that occur in the upper levels of the atmosphere.
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 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 how is this associated with the weather? UNANSWERABLE what are some of its related terms? It is the opposite of cyclolysis which scaled are used to measure it? The macroscale, the synoptic scale, the mesoscale, and the microscale what does the first one do? It deals with systems with global size, such as the Madden–Julian oscillation who invented the second one? UNANSWERABLE what is the function of the third one? It deals with  the study of weather systems smaller than synoptic scale systems but larger than microscale and storm-scale cumulus systems is the fourth one the opposite of the first one? Yes, it is smallest of the meteorological scales what results does the second one give? It  covers a portion of a continent, such as extratropical cyclones, with dimensions of across
A low-pressure area, low area or low is a region where the air pressure is lower than that of surrounding locations. Low-pressure systems form under areas of wind divergence that occur in the upper levels of the atmosphere. The first area is on the east side of upper troughs and a second area occurs ahead of embedded shortwave troughs They form under areas of wind divergence that occur in the upper levels of the atmosphere.
Low-pressure area Low-pressure area Low-pressure area
Introduction Introduction Introduction
A low-pressure area, low area or low is a region where the air pressure is lower than that of surrounding locations. Low-pressure systems form under areas of wind divergence that occur in the upper levels of the atmosphere. The formation process of a low-pressure area is known as cyclogenesis. Within the field of meteorology, atmospheric divergence aloft occurs in two areas. The first area is on the east side of upper troughs, which form half of a Rossby wave within the Westerlies (a trough with large wavelength that extends through the troposphere). A second area of wind divergence aloft occurs ahead of embedded shortwave troughs, which are of smaller wavelength. Diverging winds aloft ahead of these troughs cause atmospheric lift within the troposphere below, which lowers surface pressures as upward motion partially counteracts the force of gravity. Low-pressure systems form under areas of wind divergence that occur in the upper levels of the atmosphere. The formation process of a low-pressure area is known as cyclogenesis. Within the field of meteorology, atmospheric divergence aloft occurs in two areas. The first area is on the east side of upper troughs, which form half of a Rossby wave within the Westerlies (a trough with large wavelength that extends through the troposphere). A second area of wind divergence aloft occurs ahead of embedded shortwave troughs, which are of smaller wavelength. Low-pressure systems form under areas of wind divergence that occur in the upper levels of the atmosphere.
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Low-pressure area [SEP] Introduction
A low-pressure area, low area or low is a region where the air pressure is lower than that of surrounding locations. Low-pressure systems form under areas of wind divergence that occur in the upper levels of the atmosphere. The formation process of a low-pressure area is known as cyclogenesis. Within the field of meteorology, atmospheric divergence aloft occurs in two areas. The first area is on the east side of upper troughs, which form half of a Rossby wave within the Westerlies (a trough with large wavelength that extends through the troposphere). A second area of wind divergence aloft occurs ahead of embedded shortwave troughs, which are of smaller wavelength.