A glacier's mass is the net result of
seasonal snow accumulation and seasonal ice loss.
Not exact matches
Estimates of surface
snow water equivalent (SWE) in alpine regions with
seasonal melts are particularly difficult in areas of high vegetation density, topographic relief and
snow accumulations.
This snowpack
accumulation near the poles, which gets its water via the Arctic and Antarctic oceans, that in turn rob it from equatorial latitudes of our oceans, also results in a reduction in the earth's spin axis moment of inertia and causes the spin rate to increase as evidenced in the recent history of the rate at which Leap Seconds are added to our calendar (see Wysmuller's Toucan Equation for more on this evidence that during this warm time with much greater polar humidity, earlier
seasonal, later
seasonal and heavier
snows are beginning to move water vapor from the oceans to the poles to re-build the polar ice caps and lead us into a global cooling, while man - made CO2 continues to increase http://www.colderside.com/faq.htm).
Even though the
seasonal ice cover was formed later in the fall of 2007, the mean thickness of the FY ice cover at the end of March seems comparable to that of the previous two seasons because of lower
snow accumulation and thus faster growth i.e., higher ice production.
Other in situ and satellite data suggest that even though the
seasonal ice cover was formed later in the fall of 2007, the mean thickness of first year ice cover is comparable to that of the previous two seasons because of lower
snow accumulation and lower air temperatures and thus, faster growth.