Transactions of the Institute of British Geographers

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Remote Sensing And Image Interpretation

Glacial melting in the Tibetan Plateau affects the water resources of millions of people. This study finds that—partly owing to changes in atmospheric circulations and precipitation patterns—the most intensive glacier shrinkage is in the Himalayan region, whereas glacial retreat in the Pamir Plateau region is less apparent.

Different glacier status with atmospheric circulations in Tibetan Plateau and surroundings

http://ruby.fgcu.edu/courses/twimberley/envirophilo/wanner.pdf

Mid- to Late Holocene climate change: an overview

Data Reduction And Error Analysis For The Physical Sciences

Late Tertiary glaciations and climate dynamics in Antarctica : evidence from the Sirius Group, Mount Fleming, Dry Valleys

Reconstructing the response of present-day ice sheets to past global climate change is important for constraining and refining the numerical models which forecast future contributions of these ice 

https://www.tandfonline.com/doi/pdf/10.1080/17445647.2020.1761464

The glacial geomorphology of western Dronning Maud Land, Antarctica

We use cosmogenic exposure ages to determine the timing of deglaciation of the Scandinavian ice sheet (SIS) at summit elevation in the central Swedish mountains. Mean exposure ages for boulders on ...

/pdf/high-elevation-cosmogenic-nuclide-dating-of-the-last-cehlb6gekq.pdf

High-elevation cosmogenic nuclide dating of the last deglaciation in the central Swedish mountains: implications for the timing of tree establishment

Inceptions, mechanisms, patterns and timing of ice sheet inception

Glacial erosion has created distinctive types of landscapes reflecting the extent, duration, and processes of the parent glaciers. Alpine landscapes are representative of pervasive erosion at the local scale. Landscapes formerly covered by larger scale glaciations display a wide range of appearances, from intensively eroded to preserved. Landscapes of selective linear erosion were formed, where subglacial melting occurred along certain corridors that were flanking regions of subglacial freezing. Landscapes of areal scouring were formed where subglacial melting on low-relief surfaces allowed spatially extensive subglacial stripping to dominate. Landscapes of little or no erosion indicate a dominance of subglacial freezing conditions.

Arjen P. Stroeven

Papers

Late Tertiary glaciations and climate dynamics in Antarctica : evidence from the Sirius Group, Mount Fleming, Dry Valleys

The glacial geomorphology of western Dronning Maud Land, Antarctica

High-elevation cosmogenic nuclide dating of the last deglaciation in the central Swedish mountains: implications for the timing of tree establishment

Inceptions, mechanisms, patterns and timing of ice sheet inception

8.9 Erosional Landscapes