And at the recent Fall Meeting of the American Geophysical Union, Bill Lau of NASA drew attention to another way in which soot can
affect glacier mass balance.
Not exact matches
Notably, the quote «Mölg and Hardy (2004) show that
mass loss on the summit horizontal
glacier surfaces is mainly due to sublimation (i.e. turbulent latent heat flux) and is little
affected by air temperature through the turbulent sensible heat flux.»
The situation regarding
glaciers on Mt. Kenya is probably more complicated than just a question about temperature — changes in precipitation pattern will also
affect their
mass balance.
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).
There are four factors which
affect ice sheet
mass balance: snowfall, sublimation, melting, and
glacier calving.
«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.»
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.