It wasn't one or two particularly
heavy atmospheric river storms that pulled California out of a drought, increased snowpack and caused flooding.
Not exact matches
That is because
atmospheric rivers (see sidebar) often produce
heavy, cold season precipitation and flooding when they hit the west coast of North America.
Why It Matters: On average,
atmospheric rivers hit the western United States only a few times each winter, but they transport significant amounts of moisture that converges in the mountains producing
heavy precipitation.
A relentless series of storms — driven by persistent troughing and an associated active jet stream along the West Coast — brought numerous
atmospheric rivers and associated
heavy precipitation to much of the state since November.
On January 3 and 4, the first of two back - to - back
atmospheric river storms brought
heavy rain, mountain snow, and localized flooding to central California.
On January 3 and 4, the first of two back - to - back
atmospheric river storms (wide paths of moisture in the atmosphere composed of condensed water vapor), brought
heavy rain and mountain snow to central California, ahead of an even more intense round of
heavy precipitation brought by a powerful, long - duration
atmospheric river storm pulling warm and moist air to California from the subtropical and equatorial region southeast of Hawaii.
The second
atmospheric river storm hit late on January 7, causing a prolonged period of
heavy rainfall.
Called «
atmospheric rivers», such features are relatively common in the North Pacific in the fall and winter, routinely bringing
heavy rains and snow to the Pacific Northwest and California.