As we near the final month of summer in the Northern Hemisphere, NASA scientists are watching
the annual seasonal melting of the Arctic sea ice cover.
Not exact matches
Glaciers follow an
annual cycle,
melting in summer and growing in winter owing to
seasonal changes in temperature and precipitation.
Despite the key role meltwater plays in people's livelihoods and on the region's ecosystem services, such factors as
annual amounts of ice and snow
melt, its
seasonal and spatial variability, as well as the contributions of precipitation to these basins, have not been clearly enumerated (24).
This is twice the 2001 heat flux, comparable to the
annual shortwave radiative flux into the Chukchi Sea, and enough to
melt 1 / 3rd of the 2007
seasonal Arctic sea - ice loss.
For example, the
melting of the Greenland ice sheet broke previous records in 2002, 2005, and 2007, and
seasonal melting from 1996 to 2007 was above average compared with the 1973 - 2007 period.10, 11 The
melting of the Greenland ice sheet contributed around 0.02 inch (0.6 millimeter) to global sea - level rise in 2005 — more than double the 1996 contribution.4 From 1993 to 2003 the average rate of sea - level rise increased to about 0.12 inches (3.1 millimeters) per year.12 That means that in 2005 Greenland could have contributed 19 percent of the average
annual global sea level rise rate.