Projections for global average temperatures relative to 1850 - 79 (upper chart), rates of glacier change (middle) and
total glacier mass (lower chart) for the 21st century.
Not exact matches
As a result, the coastal ice caps and
glaciers lose their melting ice as run off 65 percent faster than they can recapture it — contributing to a loss of ice equivalent to roughly 14 percent of the
total mass of Greenland.
Rising global temperatures have also made
glaciers — ice
masses that currently occupy nearly 10 percent of the world's
total land area — increasingly unstable.
A
total of over 5,000 measurements of
glacier volume and
mass changes since 1850 and more than 42,000 records from observations and reconstructions dating back to the sixteenth century were analyzed.
The estimated 2010 or 2011 surface
mass imbalance (~ 300 Gt / yr) is comparable to the GRACE estimates of the
total mass loss (which includes ice loss via dynamic effects such as the speeding up of outlet
glaciers) of 248 ± 43 Gt / yr for the years 2005 - 2009 Chen et al, 2011.
According to BBC Brasil, between 1993 and 2003 alone, Trento's Presena
glacier lost as much as 39 percent of its
total mass.
Although one can point to particular
glaciers that are growing, glaciologists look for trends in the
total mass of
glaciers worldwide.
Annual net balance on eight North Cascades
glaciers during the 1984 - 1994 period has been determined by measurement, of
total mass loss from firn and ice melt and, of residual snow depth at the end of the summer season.
We had the advantage of already understanding the overall
mass balance pattern of each
glacier in selecting measurement networks that would provide the most representative coverage for the
glacier given the
total number of measurements in each sample (Pelto, 1996; Miller and Pelto, 1999).
The
total global ice
mass lost from Greenland, Antarctica and Earth's
glaciers and ice caps during the study period was about 4.3 trillion tons (1,000 cubic miles), adding about 0.5 inches (12 millimeters) to global sea level.
The limited resolution of GRACE affects the uncertainty of
total mass loss to a smaller degree; we illustrate the «real» sources of
mass changes by including satellite altimetry elevation change results in a joint inversion with GRACE, showing that
mass change occurs primarily associated with major outlet
glaciers, as well as a narrow coastal band.
North Cascade
glaciers annual balance has averaged -0.54 m / a of water equivalent from 1984 - 2006, a cumulative loss of over 12.4 m in
glacier thickness or 20 - 40 % of their
total volume since 1984 due to negative
mass balances.
► Mean specific
mass balance: The
total mass balance per unit area of the
glacier.
Pritchard points out that basal melt is a control on
total mass waste ``... through a reduction in buttressing of the adjacent ice sheet leading to accelerated
glacier flow.»