Forward modelling of the completeness and preservation of palaeoclimate signals recorded by ice-marginal moraines.
Earth Surf Process Landf
; 47(9): 2198-2208, 2022 Jul.
Article
in En
| MEDLINE
| ID: mdl-36249916
ABSTRACT
Glaciers fluctuate in response to climate change and record these changes by building sedimentary landforms, including moraines. Therefore, glacial landscapes are a potentially valuable archive of terrestrial palaeoclimate change. Typically, a cooling climate causes glaciers to expand and a warming climate causes glaciers to shrink. However, the glacier response time and the influence of mountainous topography on glacier dynamics complicates this behaviour, such that moraines are not always a straightforward indicator of glacier change in response to climate change. We used a glacial landscape evolution model to simulate the response of a hypothetical mountain glacier to simple changes in climate and the resulting formation and preservation of moraines. These results show that the rate of climate change relative to the glacier response time determines the geometry, number, and position of moraines. Glaciers can build distinct moraines in the absence of climate change. The distance from the maximum ice extent may not represent the chronological order of moraine formation. Moraines can be preserved after being overrun and eroded by subsequent glaciations, but moraine sequences may also contain gaps that are unidentifiable in the field.
Full text:
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Collection:
01-internacional
Database:
MEDLINE
Language:
En
Journal:
Earth Surf Process Landf
Year:
2022
Document type:
Article