That is because atmospheric rivers (see sidebar) often produce heavy,
cold season precipitation and flooding when they hit the west coast of North America.
Not exact matches
For their study, Beck and Sieber selected 19 climate and soil variables that could influence how humans use the land, including soil type and
precipitation in the
coldest and warmest
seasons.
The winter of 2010/2011 proved to be a dark,
cold and windy
season with no shortage of
precipitation.
Precipitation freezes during the
coldest months and then melts during the agricultural
season.
For the entire Northern Hemisphere, there is evidence of an increase in both storm frequency and intensity during the
cold season since 1950,1 with storm tracks having shifted slightly towards the poles.2, 3 Extremely heavy snowstorms increased in number during the last century in northern and eastern parts of the United States, but have been less frequent since 2000.11,15 Total seasonal snowfall has generally decreased in southern and some western areas, 16 increased in the northern Great Plains and Great Lakes region, 16,17 and not changed in other areas, such as the Sierra Nevada, although snow is melting earlier in the year and more
precipitation is falling as rain versus snow.18 Very snowy winters have generally been decreasing in frequency in most regions over the last 10 to 20 years, although the Northeast has been seeing a normal number of such winters.19 Heavier - than - normal snowfalls recently observed in the Midwest and Northeast U.S. in some years, with little snow in other years, are consistent with indications of increased blocking (a large scale pressure pattern with little or no movement) of the wintertime circulation of the Northern Hemisphere.5 However, conclusions about trends in blocking have been found to depend on the method of analysis, 6 so the assessment and attribution of trends in blocking remains an active research area.
It now rains considerably more in winter almost everywhere in Germany; in some cases,
precipitation volumes have increased by as much as 30 percent in the
cold season.
A 2013 study modeled climate and water system (hydroclimate) changes in the Western US over the next three decades and found that increased temperature is the dominant factor, likely leading to several hydroclimate changes, including: decreases in spring snow pack, increases in
cold -
season days above freezing, and decreases in the
cold -
season snow - to -
precipitation ratio.
Hoell A., M. Barlow, F. Cannon and T. Xu (April 2017): Oceanic Origins of Historical Southwest Asia
Precipitation During the Boreal
Cold Season.
Hoell A. (March 2018):
Cold Season Southwest Asia
Precipitation Sensitivity to El Niño - Southern Oscillation Events.