There are four factors which
affect ice sheet mass balance: snowfall, sublimation, melting, and glacier calving.
Because Antarctica drains more than 80 percent of its ice sheet through floating ice shelves, accelerated glacier flow has the potential to
affect ice sheet mass balance dramatically and raise sea level (Pritchard et al. 2012).
Not exact matches
Both
ice sheets are significantly losing
mass, and that
affects sea level.
[Response: Rain on the flanks is not that uncommon, but enough rain on the bulk of the
ice sheet to
affect the surface
mass balance as much as you suggest is not on.
The findings reinforce suggestions that strong positive
ice — temperature feedbacks have emerged in the Arctic15, increasing the chances of further rapid warming and sea
ice loss, and will probably
affect polar ecosystems,
ice -
sheet mass balance and human activities in the Arctic...» *** This is the heart of polar amplification and has very little to do with your stated defintion of amplifying the effects of warming going on at lower latitudes.
The principal processes
affecting the
mass balance and dynamics of the
ice sheets are
ice mass input from snowfall with losses from sublimation and drifting.
«This implies that changes at the margin can
affect the
mass balance deep in the centre of the
ice sheet,» said Dr Khan.
«As a result, the loss of glacier
mass worldwide, along with the corresponding release of carbon, will
affect high latitude marine ecosystems, particularly those surrounding the major
ice sheets that now receive fairly limited land - to - ocean fluxes of carbon.»
«Greenland hosts the largest reservoir of freshwater in the northern hemisphere, and any substantial changes in the
mass of its
ice sheet will
affect global sea level, ocean circulation and climate,» said Velicogna.