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This is a place in the Atlantic Ocean that contains the Caribbean Sea and Gulf of Mexico, which is very prone and vulnerable to hurricanes during the period time of Atlantic Hurricane.
These are prevailing winds in the midway latitudes between thirty and sixty degrees latitude, gusting from the high pressure area (HPA) in the horse latitudes on the way to the poles.
Also recognize as a gust front, is a storm-scale or mesoscale boundary that can set apart thunderstorm-cooled air from the surrounding air; the same in effect to a cold front, with passage marked by a wind switch and usually a free fall in temperature and a pressure jump.
Also recognize as a gust front, is a storm-scale or mesoscale boundary that can set apart thunderstorm-cooled air from the surrounding air; the same in effect to a cold front, with passage marked by a wind switch and usually a free fall in temperature and a pressure jump.
This is a vortex of wind within a convective storm. That is, it is air that ascends and rotates around a vertical axis, basically in the same location direction as low pressure systems in a certain hemisphere.
Connected with a tropical cyclone is a usual indicator of the strength capacity of the storm. Within a fully developed tropical cyclone, it can be found within the eyewall at a distance described as the radius of maximum wind.
This is the quantitative relation of the partial pressure of water vapor in a water-air mixture to the overflowing vapor pressure of water at a recommended temperature. The relative humidity of air relies on the system of interest of the pressure and temperature.
Some other term for horse latitudes, it is a remarkable belt of high pressure located in the Northern Hemisphere around the latitudes of 30°N and 30°S in the Southern Hemisphere.
