The Ridiculously Resilient Ridge Returns; typical winter conditions still nowhere to be found in California
Filed in Uncategorized by Daniel Swain on February 16, 2015 • 30 Comments
Summary of recent conditions
Well, it has certainly been warm out there. Record warmth, in fact, has occurred on most days so far this calendar year somewhere in the state of California.
A veritable February heatwave occurred over the recent holiday weekend, bringing record highs from the Mexican border all the way up to Oregon. And the calendar year to date, in some spots (including San Francisco), is currently the warmest on record. 2015 thus far is certainly among the warmest calendar years to date on a statewide basis, and will likely surpass (by the end of February) the previous record…set just last year (in 2014). This extraordinary warmth has been especially pronounced over the past 10 days as clear skies and shirtsleeve weather allowed many Californians to get outdoors and enjoy the strangely balmy February conditions. But those spending time outdoors over the past weekend have likely noticed signs that the present situation is far from typical for mid-winter in California. Vegetation–native and otherwise–has already begun to show signs of growth and flowering that typically aren’t experienced until well into the spring. Despite the green hillsides, streamflow in most of California’s creeks, streams, and rivers remains well below average for this time of year. Sierra Nevada snowpack–already at near-record low levels before the mid-February heatwave which brought temperatures above 60 degrees to the Tahoe Basin–has declined even further in recent days.
Early in the month, a very brief sequence of strong and moist storm systems brought widespread significant precipitation to the northern 2/3 of the state, with a focus on northern coastal areas. This intense rainfall did result in rapid rises on certain rivers in NorCal, and resulted in temporarily strong inflows into many of NorCal’s major reservoirs. Remarkably, however, this storm sequence ultimately resulted in little or no lasting snow accumulation below 8000 feet in the Sierra Nevada. Extremely warm temperatures dominated the event–not surprising, given the subtropical origin of the moisture. Interestingly, this event was quite similar to the brief but intense warm and wet storm sequence experienced in NorCal back in December 2014...