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The ENSO cycle has a huge effect on rainfall and snowfall patterns in California, especially during the winter and spring seasons. During the El Niño phase, the jet stream is located south through California, allowing for warmer temperatures and more heavy rains to occur, particularly in the southern portions of the state.
The Santa Anas are katabatic winds (Greek for "flowing downhill") arising in higher altitudes and blowing down towards sea level. [7] The National Weather Service defines Santa Ana winds as "a weather condition [in southern California] in which strong, hot, dust-bearing winds descend to the Pacific Coast around Los Angeles from inland desert regions".
The primary weather station for Los Angeles is located near downtown at the south side of Dodger Stadium campus, and this article refers primarily to climate data generated by this station as representative of the Los Angeles metropolitan area as a whole.
According to NOAA, a typical weather pattern during a La Niña is cool and wetter than average temperatures in the Pacific Northwest, and warmer and drier than average weather in the Southern U.S ...
The wildfires that ravaged the Los Angeles area were driven by monthslong, climate change-fueled weather patterns, according to scientists. ... For some parts of Southern California, the winter ...
An especially strong Walker circulation causes La Niña, which is considered to be the cold oceanic and positive atmospheric phase of the broader El Niño–Southern Oscillation (ENSO) weather phenomenon, as well as the opposite of El Niño weather pattern, [19] where sea surface temperature across the eastern equatorial part of the central ...
After several consecutive years of severe drought that climate scientists say were made worse because of rising global temperatures, California has been hit with an especially cold and wet winter ...
An El Niño episode is characterised by a breakdown of this water and air cycle, resulting in relatively warm water and moist air in the eastern Pacific. The Walker circulation , also known as the Walker cell , is a conceptual model of the air flow in the tropics in the lower atmosphere ( troposphere ).