By the way Kenneth, you were commented on the line «when it warms,
glaciers retreat until either a new equilibrium between ablation and accumulation is found or until they disappear.»
Dear Kenneth, when it warms,
glaciers retreat until either a new equilibrium between ablation and accumulation is found or until they disappear.
Not exact matches
The height of these cliffs made them unstable, triggering the release of thousands of icebergs into Pine Island Bay, and causing the
glacier to
retreat rapidly
until its grounding line reached a restabilising point in shallower water.
The
glaciers expanded in bursts, advancing quickly,
retreating briefly, and then expanding farther —
until about 100 years ago, according to the study.
NOAA has a nice visual of the recession of the Jakobshavn
glacier which RC posted here: http://www.realclimate.org/images/jakobshavn.jpg There was a rather large
retreat from 1851
until 1913, then slowing
until 2001, with a recent acceleration.
Re # 40: -LSB-... As for the 1940s, I'm not familiar with the details of GNP, but in Washington State where I live,
glaciers did
retreat substantially
until about the 1940s, before advancing again
until the late 1970s.
When pulses of warm water are strong enough to rise over the shelf's outer ridge, that warm dense water then flows downward to the grounding point of the
glacier and remains there
until a new equilibrium is established via basal melting and a
retreating grounding point.
The
glaciers expanded in bursts, advancing quickly,
retreating briefly, and then expanding farther —
until about 100 years ago, according to the study.
«Shift to the warm - phase PDO in 1977 initiated global warming and recession of
glaciers that persisted
until 1998» The World Glacier Monitoring Service has noted that the peak percentage of
glaciers retreating is not in 1998 but in 2005 or 2006 at more than 95 % that is persisted alright.
When it is warm, ice melts faster and the
glacier will
retreat until it reaches a new equilibrium between accumulation and ablation.
Until recently, the contribution of ice sheets to sea - level rise remained unknown and is still debated, but the current acceleration of sea - level rise is attributed to heating of the oceans and melting of land
glaciers which is supported by measurements of ocean temperatures and the behavior of mountain
glaciers, the vast majority of which are
retreating or exhibit signs of instability.
In general,
glaciers retreat due to a combination of rising temperatures and declining precipitation, but the temperature and precipitation records from the Alps indicated that
glaciers should have continued advancing
until around 1910.
(By the way go to an Iceland website and you'll find that the
glaciers there were
retreating from the late 1800's
until 1980 and have since become stationary.