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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.
The North American monsoon is marked by a broad area of high pressure, usually parked in the Four Corners region, but the exact position of that high can influence exactly where (and how much ...
The North American Monsoon (NAM) occurs from late June or early July into September, originating over Mexico and spreading into the southwest United States by mid-July. This allows the wet season to start in the Southwest during the summer rather than early fall as seen across the remainder of the West. [10]
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.
For the Southwest, the North American monsoon can be both a blessing and a curse. It brings much-needed rain to the region, but that precipitation typically falls in torrential downpours that the ...
[78] [c] [19] [d] The red side-up orientation of the flag was used by the First Philippine Republic during the Philippine–American War from 1899 to 1901, [79] by the Philippine Commonwealth during World War II from 1941 to 1945, by the Japanese-sponsored Philippine Republic when it declared war against the United Kingdom and the United States ...
The American flag remained unchanged since 1919. For the Philippine flag, the design conceived by Emilio Aguinaldo remained but the shades of blue and red were adopted from the American flag. The sun's face was removed, but its stylized rays were retained. There existed many versions of the flag as no official design had been codified. 1936–1946
August position of the ITCZ and monsoon trough in the Pacific Ocean, depicted by area of convergent streamlines in the northern Pacific. The monsoon trough is a portion of the Intertropical Convergence Zone in the Western Pacific, [1] [2] as depicted by a line on a weather map showing the locations of minimum sea level pressure, [1] and as such, is a convergence zone between the wind patterns ...