A 2015 study using regional ice core data reveals no unusual temperature changes but an exceptional 30 % increase in
snow accumulation during the twentieth century, again supporting Zwally's analysis of mass gain in interior west Antarctica.
Some commentators, notably the formidable DeWitt Payne, suggest Drake gets it wrong because a simpler explanation is that
snow accumulation during the deepest part of the ice age is slower than it is during interglacial periods.
Not exact matches
Meteorological data, which only date back 35 years, show the low pressure system has strengthened
during that time, leading to more storms swirling around the Amundsen Sea and potentially greater
snow accumulation, according to the paper.
«West Antarctic coastal
snow accumulation rose 30 percent
during 20th century.»
Annual
snow accumulation on West Antarctica's coastal ice sheet increased dramatically
during the 20th century, according to a new study published in the American Geophysical Union journal Geophysical Research Letters.
This 2013 GMC Acadia Denali with AWD saved me
during a commute in a late - winter storm that included white - out conditions and 2 inches or more of
snow accumulation.
Even though the
accumulation of
snow is fairly uncommon
during this month, the chances of
snow lying on the ground are at their highest around February 23rd.
Meanwhile
during this period of ice melt, Mt. Blanc in Europe and Mt. Logan in North America have both recently had their elevations increased due to the significan
accumulation of
snow in recent years - hardly what I would say is an indicator of serious global warming.
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).
Although Zwally calculated the net «mass gains from
snow accumulation exceeded losses from ice discharge by about 112 and 82 Gt / year respectively
during the 1992 - 2001 and 2003 - 08 measurement periods», he also reported that the rate of ice loss along the west Antarctic coast and the peninsula had increased from 64 GT / year to 135 GT / year
during those same periods.
Mass Gains of the Antarctic Ice Sheet Exceed Losses http://ntrs.nasa.gov/search.jsp?R=20120013495 SCAR ISMASS Workshop, July 14, 2012 «
During 2003 to 2008, the mass gain of the Antarctic ice sheet from
snow accumulation exceeded the mass loss from ice discharge by 49 Gt / yr (2.5 % of input), as derived from ICESat laser measurements of elevation change
Annual mass balance is the difference between winter
snow and ice
accumulation on a glacier, and summer
snow and ice loss from a glacier
during a given year.
http://ntrs.nasa.gov/archive/nasa/casi.ntrs.nasa.gov/20120013495.pdf
During 2003 to 2008, the mass gain of the Antarctic ice sheet from
snow accumulation exceeded the mass loss from ice discharge by 49 Gt / yr (2.5 % of input), as derived from ICESat laser measurements of elevation change.
The beginning of the
snow accumulation season (the end of the snowmelt season) is projected to be later (earlier), and the fractional
snow coverage is projected to decrease
during the
snow season (Hosaka et al., 2005).
Here in Minnesota, a large portion of these claims occur
during the winter due to heavy
accumulation of ice and
snow.
Solar installation may also affect the roof warranty due to damage of the membrane
during installation, additional wear and tear resulting from unforeseen traffic on the roof, or from excessive loads on the roof structure due to system weight, wind load or
snow accumulation.