Pipirr
Graduate Poster
- Joined
- Mar 3, 2006
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Why, if the planet is getting warmer, would some of the glaciers show a rather dramatic advance?
I'm really trying to understand how warmer = more ice ...
Here's some background from the publication in Science:
Extracting a Climate Signal from 169 Glacier Records
Johannes Hans Oerlemans 1
1 Institute for Marine and Atmospheric Research, Utrecht University
A temperature history for different parts of the world has been constructed from 169 glacier length records. Using a first-order theory of glacier dynamics, changes in glacier length were related to changes in temperature. The derived temperature histories are fully independent of proxy and instrumental data used in earlier reconstructions. Moderate global warming started in the middle of the 19th century. The reconstructed warming in the first half of the 20th century is 0.5 K. This warming was remarkably coherent over the globe. The warming signals from glaciers at low and high elevations appear to be very similar.
Some commentary from statured climate scientists:
From the compilations of World Glacier Monitoring Service (and many other groups and individuals), we know that glacier retreat is in fact an essentially global phenomenon, with only a few isolated (and well understood) counter-examples, such as western Norway.
Diogenes, in the study some of the glaciers showed 'a rather dramatic advance' but most of them do not. The ones that do are the exceptions, for "well understood" reasons. For the rest, it was possible to identify "warming signals from glaciers at low and high elevations".
One of the counter examples from that figure is the Franz-Josef glacier in NZ.
The glacier is currently 12 km long and terminates 19 km from the Tasman Sea. It exhibits a cyclic pattern of advance and retreat, driven by differences between the volume of meltwater at the foot of the glacier and volume of snowfall feeding the névé.
Having retreated several kilometres between the 1940s and 1980s, the glacier entered an advancing phase in 1984 and at times has advanced at the phenomenal (by glacial standards) rate of 70 cm a day. The flow rate is about 10 times that of typical glaciers. Over the longer term, the glacier has retreated since the last ice age, and it is believed that it extended into the sea some 10,000 to 15,000 years ago.
From the description, it is an atypical glacier.