snowpack


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snow·pack

 (snō′păk′)
n.
An area of naturally formed, packed snow that usually melts during the warmer months.
American Heritage® Dictionary of the English Language, Fifth Edition. Copyright © 2016 by Houghton Mifflin Harcourt Publishing Company. Published by Houghton Mifflin Harcourt Publishing Company. All rights reserved.

snowpack

(ˈsnəʊˌpæk)
n
a quantity of fallen snow that has become massed together
Collins English Dictionary – Complete and Unabridged, 12th Edition 2014 © HarperCollins Publishers 1991, 1994, 1998, 2000, 2003, 2006, 2007, 2009, 2011, 2014

snow•pack

(ˈsnoʊˌpæk)

n.
the accumulation of winter snowfall, esp. in mountain or upland regions.
[1945–50]
Random House Kernerman Webster's College Dictionary, © 2010 K Dictionaries Ltd. Copyright 2005, 1997, 1991 by Random House, Inc. All rights reserved.
References in periodicals archive ?
If the snowpack melts, amount of water that would be released depends on the snow water equivalent (SWE) of the snowpack and the vertical height of the snowpack on the ground is the snow depth.
A growing body of research suggests that warming temperatures and a loss of snowpack linked to climate change may significantly shrink the range where it's possible to make maple syrup.
February and March brought the Colorado River Basin an interesting twist of fate with a very wet winter that produced a deep snowpack in the western slopes of the Rocky Mountains.
Thawing snowpack and heavy rains have brought historically high flooding to several Midwestern states and have led to thousands of evacuations, BBC reports.
With the current high temperatures and increased humidity, the most dangerous time is around noon and early afternoon when the snowpack is wet and overloaded and its stability is most likely to be affected, Kamen Yakimov explained.
City officials expect much of the snowpack to melt over the weekend due to warmer temperatures and rain.
They discovered that the amount of dust on the snowpack controlled the rate at which the rivers rose in the spring, regardless of the air temperature.
This area, which receives little precipitation during summer, relies considerably on the wintertime precipitation phase and snowpack accumulation to sustain a multitude of ecosystem goods and services [2].
A combination of factors - plenty of rain this spring, brimming reservoirs, a copious snowpack and some warm weather - are making the McKenzie and Willamette rivers and their tributaries run cold, full and fast.
In addition to the precipitation, California saw a considerable increase in its snowpack, which will help keep the state out of drought conditions this spring and summer when it begins to melt.
Snow Water Equivalence (SWE) represents the total amount of water available if the snowpack were melted instantaneously.