The study interval 1984 - 2000 began in a period of
negative glacier mass balance, extending that dominated the 1975 - 1994 interval (Pelto, 1996; Krimmel, 1994).
This years forecast issued May 1 is for
negative glacier mass balance.
If PDO is positive and ENSO is
negative glacier mass balance will be negative on South Cascade Glacier.
Hence the increasingly
negative glacier mass balance record that you are familar with.
Not exact matches
Nearly every
glacier has a
negative mass balance.
Negative mass balances on tributary
glaciers can lead to thinning of the
glaciers and ice shelves.
Overall, I estimate the
mass balance of the Greenland ice sheet to be about -80 + / -10 cubic km of ice per year in 2000 and -110 + / -15 cubic km of ice per year in 2004, i.e. more
negative than based on partial altimetry surveys of the outlet
glaciers.
As for how this could be — and in light of the findings of the references listed above — Rankl et al. reasoned that «considering increasing precipitation in winter and decreasing summer mean and minimum temperatures across the upper Indus Basin since the 1960s,» plus the «short response times of small
glaciers,» it is only logical to conclude that these facts «suggest a shift from
negative to balanced or positive
mass budgets in the 1980s or 1990s or even earlier, induced by changing climatic conditions since the 1960s.»
As predictors of
glacier mass balance positive MEI values, El Nino, and warm phase PDO's favor
negative balances, and cool phase PDO's and
negative MEI values, La Nina, favor positive annual balances.
«The rest of the
glaciers in the Himalayas are mostly melting, in that they have
negative mass balance, here we found that
glaciers aren't,» study researcher Julie Gardelle, of CNRS - Université Grenoble, France, told LiveScience.
The 2003 — 08 specific
mass balance for our entire HKKH study region was − 0.21 ± 0.05 m yr − 1 water equivalent, significantly less
negative than the estimated global average for
glaciers and ice caps4, 10.
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.
The trend in
mass balance is becoming more
negative which is fueling more
glacier retreat and thinning note figure at right.