As of April 1st, most locations from the Great Basin to the West Coast had much below -
average snow pack.
In Alaska, snow pack totals less than 25 percent of average were observed across southern regions of the state, while interior locations had near -
average snow pack.
Not exact matches
I read on our provincial
snow pack data that Vancouver Island is very low, although other parts of the province are above
average.
Antarctica is technically a desert — with an
average 166 mm of precipitation a year — but
snow that falls tends to stay, and becomes
packed ever tighter with the decades.
In March 2017, temperatures in the Sierra Nevada mountain range were 3 to 4 °F above the 1949 - 2005
average (see image below on the left)[4] and contributed to reduced
snow pack levels.
[8] Weather systems passing through California originate globally, and the
average global increase in temperature has been 1 °C, indicating significant risk that storms arriving in California may be warming and converting additional
snow pack to mountain run - off.
In 2015, for the first time in 120 years of record keeping, the winter
average minimum temperature in the Sierra Nevada was above freezing, a key threshold for maintaining
snow pack.
[8] Rain - on -
snow - producing atmospheric river storms are, on
average, only 2 °C warmer than others storm types that preserve
snow pack.
The remaining
snow pack in the area continues to
average a depth of 50 centimetres with an
average water content of 150 millimetres.