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Summer monsoon rain over eastern New Mexico. The North American monsoon, variously known as the Southwest monsoon, the Mexican monsoon, the New Mexican monsoon, or the Arizona monsoon [1] is a term for a pattern of pronounced increase in thunderstorms and rainfall over large areas of the southwestern United States and northwestern Mexico.
If the shift is delayed, so is the southwest monsoon. An early shift results in an early monsoon. Strength: The strength of the southwest monsoon is determined by the strength of the easterly tropical jet over central India. A strong easterly tropical jet results in a strong southwest monsoon over central India, and a weak jet results in a weak ...
The major monsoon systems of the world consist of the West African, Asian–Australian, the North American, and South American monsoons. The term was first used in English in British India and neighboring countries to refer to the big seasonal winds blowing from the Bay of Bengal and Arabian Sea in the southwest bringing heavy rainfall to the area.
Powerful monsoon storms moved through Arizona, Utah and Colorado on Aug. 21-23, 2024, with intense downpours, hail, heavy winds, flooding and lightning. In comparison, most of the summertime in ...
The North American monsoon, which has brought localized but dangerous flash flooding to parts of the southwestern United States over the past week, will finally ease back into the upcoming weekend.
An annual event, known as the North America monsoon, will continue to bring the risks of flash flooding, dust storms and lightning strikes over the southwestern United States in the weeks to come.
Upwelling current at the Somali coast during Southwest Monsoon. The offshore Somali coastal area is one of the most productive marine ecosystems in the world. Especially during the southwest Indian monsoon, strong upwelling pumps cold (17-22 °C) and highly nutrient rich (about 5 to 20 μm of nitrate [21]) subsurface water to the coastal region.
The Winter Monsoon Current extends from the Bay of Bengal, around India and Sri Lanka, and across the Arabian Sea at a latitude of approximately 8 degrees North. Currents flow to the southwest along the coast of Somalia to the equator. Measurements of the strengths of these currents have been obtained from ship drift records.