Air Pressure & Altitude | Overview & Examples
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The center of the highest or lowest air pressure in your region is marked on the analysis or forecast chart with an “H” for high or “L” for low. A broad area of high pressure, or a high-pressure ridge, is often associated with fair weather due to the downward vertical motion, which causes warming and drying of the airmass. In contrast, a low-pressure trough features a general rising air motion, promoting the growth of clouds and unsettled weather. We can determine the wind direction from these p
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The center of the highest or lowest air pressure in your region is mark…
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ℹ The Tehuantepecer is a regional gap wind that develops when a strong pressure gradient forms between cold, dense air over the Gulf of Mexico and lower pressure over the eastern tropical Pacific. The air is funnelled through the low-elevation Isthmus of Tehuantepec, where topographic channelling leads to a marked increase in wind speed. The flow is predominantly northerly to northeasterly, forming a narrow low-level jet over the Gulf of Tehuantepec. Downstream over the Pacific Ocean, the jet sp
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