The Finnish Meteorological Institute has participated in a study that tested an inversion - type method for
calculating glacier mass balance for the first time.
Not exact matches
This allowed them to
calculate the redistribution of
mass on Earth's surface due to the melting of the Greenland and Antarctic ice sheets and mountain
glaciers, and model the shift in Earth's axis.
The data allowed them to
calculate the redistribution of
mass on Earth's surface due to the melting of the Greenland and Antarctic ice sheets and mountain
glaciers, and the resulting rise in sea level.
The
mass balance for the entire
glacier is
calculated by summation of the product of
glacier area within each 0.10 m
mass balance contour, and the net balance of that interval.
Van de Wal and Wild (2001) find that the effect of precipitation changes on
calculated global - average
glacier mass changes in the 21st century is only 5 % of the temperature effect.
We have found that we can reasonably
calculate mass balance from climate records for the mean of all the
glaciers, but not for individual
glaciers., with input from Snotel sites and Diablo Dam weather station.
The data allowed them to
calculate the redistribution of
mass on Earth's surface due to the melting of the Greenland and Antarctic ice sheets and mountain
glaciers, and the resulting rise in sea level.