We are now solidly into mid-winter--a good time to check on the status of precipitation over the region.
Let's start with the total cool-season precipitation since October 1, the beginning of the "water year" (see below).
The majority of the western U.S. has received above-normal precipitation, with the North Cascades and the Los Angeles area being substantially wetter than normal.
There is one major dry area: western Oregon.
The key driver of these patterns of precipitation and temperature has been persistent high pressure aloft over the western U.S, and the persistent trough of low pressure aloft over the eastern U.S. This is illustrated below, which shows the difference from normal at 500 hPa (roughly 18,000 ft). Higher than normal pressure is indicated by the yellow; blue and purple indicate the oppoosite

High pressure is associated with sinking and warming aloft. It also contributed to dry conditions.
The complex distributions of precipitation and temperature have created an even more complex distribution of snowpack over the western U.S.
The southern Sierra Nevada is fine, and eastern Washington and the Rockies are just a little below normal.
But the real problem area is found over Oregon and northern CA, where the combination of a lack of precipitation AND warm temperatures has resulted in snowpack areas below 40%.
Looking forward, the latest European Center forecasts are predicting substantial precipitation along the Washington Coast, over southwest BC, and the north Cascades.
But far less to the south, where the real deficiencies exist.
Oregon folks should not panic yet.
I can remember a number of years that were dry until early February, but made up most of the deficiency in late winter and spring.


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