Going forwards, IMBIE provides a framework for
assessing ice sheet mass balance, and has an explicit aim to widen participation to enable the entire scientific community to become involved.
Not exact matches
To
assess these implications, we translate global into local SLR projections using a model of spatial variation in sea - level contributions caused by isostatic deformation and changes in gravity as the Greenland and Antarctic
ice sheets lose
mass (36 ⇓ — 38), represented as two global 0.5 ° matrices of scalar adjustment factors to the
ice sheets» respective median global contributions to SLR and (squared) to their variances.
For example, Martín - Español et al. (2017) find that the total
mass trend for the East Antarctic
Ice Sheet was a gain of +57 Gt per year during 2003 - 2013, which is 4 times the rate of gain
assessed for 1992 - 2011.
Great progress has been made recently in
assessing the current rate of
mass loss from the
ice sheets (Shepherd et al., 2012), as well as monitoring the changing snowfall, surface melting, and temperature contributing to the changes.
In 2007, Denmark launched the Programme for Monitoring of the Greenland
Ice Sheet (PROMICE) to assess changes in the mass balance of the ice she
Ice Sheet (PROMICE) to assess changes in the mass balance of the ice s
Sheet (PROMICE) to
assess changes in the
mass balance of the
ice she
ice sheetsheet.
We need to quantify and understand these feedbacks so that we can
assess the energy budget at the
ice sheet surface and predict future changes in
ice mass.