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The curve shown in graphs of these reconstructions is widely known as the hockey stick graph because of the sharp increase in temperatures during the last century. As of 2010 [update] this broad pattern was supported by more than two dozen reconstructions , using various statistical methods and combinations of proxy records, with variations in ...
A driving force behind many California wildfires, including the current ones, is the Santa Ana winds. These dry, gusty winds are a weather phenomenon that have shaped Southern California’s ...
A standard weather phenomenon along the northern and central California coast from late spring to early fall. May Gray / June Gloom : A characteristic weather pattern of late spring (May and June) in which a combination of inland heat, off-shore cool water, and prevailing wind patterns bring foggy and overcast weather to coastal regions.
Minimum temperature map of the United States from 1871–1888 Maximum temperature map of the United States from 1871–1888. The following table lists the highest and lowest temperatures recorded in the 50 U.S. states, the District of Columbia, and the 5 inhabited U.S. territories during the past two centuries, in both Fahrenheit and Celsius. [1]
This graph's main version resides at Template:Graph:Weather monthly history. Please make or suggest all the changes there, and copy it everywhere else (until the copying is automated) Please make or suggest all the changes there, and copy it everywhere else (until the copying is automated)
Last year, California was in the midst of the driest three-year run in recorded history when NOAA, the National Oceanic and Atmospheric Administration, published a seasonal forecast for a drier ...
Records from the National Weather Show that the Sacramento area received rainfall totals ranging from more than half an inch of rain to nearly an inch and a half in the past 24 hours.
Boreal (B-S), rising sea levels, forest replaces tundra in northern Europe 7500–3900: Neolithic Subpluvial/African humid period in North Africa, wet 7000–3000: Holocene climatic optimum, or Atlantic in northern Europe (B-S) 6200: 8.2-kiloyear event cold 5000–4100