Outputs (8)

Extensive MIS 3 glaciation in southernmost Patagonia revealed by cosmogenic nuclide dating of outwash sediments (2015)
Journal Article
Darvill, C., Bentley, M., Stokes, C., Hein, A., & Rodés, A. (2015). Extensive MIS 3 glaciation in southernmost Patagonia revealed by cosmogenic nuclide dating of outwash sediments. Earth and Planetary Science Letters, 429, 157-169. https://doi.org/10.1016/j.epsl.2015.07.030

The timing and extent of former glacial advances can demonstrate leads and lags during 2 periods of climatic change and their forcing, but this requires robust glacial chronologies. In 3 parts of southernmost Patagonia, dating pre-global Last Glacial... Read More about Extensive MIS 3 glaciation in southernmost Patagonia revealed by cosmogenic nuclide dating of outwash sediments.

The surficial and subglacial geomorphology of western Dronning Maud Land, Antarctica (2015)
Journal Article
Chang, M., Jamieson, S., Bentley, M., & Stokes, C. (2016). The surficial and subglacial geomorphology of western Dronning Maud Land, Antarctica. Journal of Maps, 12(5), 892-903. https://doi.org/10.1080/17445647.2015.1097289

The surficial and subglacial geomorphology of ∼220,000 km2 of western Dronning Maud Land (WDML), Antarctica, is presented at a scale of 1:750,000. The mapped area includes the Stancomb-Wills Glacier north of 75°25′S and follows the grounded ice margi... Read More about The surficial and subglacial geomorphology of western Dronning Maud Land, Antarctica.

An ice-sheet scale comparison of eskers with modelled subglacial drainage routes (2015)
Journal Article
Livingstone, S., Storrar, R., Hillier, J., Stokes, C., Clark, C., & Tarasov, L. (2015). An ice-sheet scale comparison of eskers with modelled subglacial drainage routes. Geomorphology, 246, 104-112. https://doi.org/10.1016/j.geomorph.2015.06.016

Eskers record the signature of channelisedmeltwater drainage during deglaciation providing vital information on the nature and evolution of subglacial drainage. In this paper, we compare the spatial pattern of eskers beneath the former Laurentide Ice... Read More about An ice-sheet scale comparison of eskers with modelled subglacial drainage routes.

On the Reconstruction of Palaeo-Ice Sheets: Recent Advances and Future Challenges (2015)
Journal Article
Stokes, C., Tarasov, L., Blomdin, R., Cronin, T., Fisher, T., Gyllencreutz, R., …Teller, J. (2015). On the Reconstruction of Palaeo-Ice Sheets: Recent Advances and Future Challenges. Quaternary Science Reviews, 125, 15-49. https://doi.org/10.1016/j.quascirev.2015.07.016

Reconstructing the growth and decay of palaeo-ice sheets is critical to understanding mechanisms of global climate change and associated sea-level fluctuations in the past, present and future. The significance of palaeo-ice sheets is further underlin... Read More about On the Reconstruction of Palaeo-Ice Sheets: Recent Advances and Future Challenges.

Controls on the location, morphology and evolution of complex esker systems at decadal timescales, Breiðamerkurjökull, southeast Iceland (2015)
Journal Article
Storrar, R., Evans, D., Stokes, C., & Ewertowski, M. (2015). Controls on the location, morphology and evolution of complex esker systems at decadal timescales, Breiðamerkurjökull, southeast Iceland. Earth Surface Processes and Landforms, 40(11), 1421-1438. https://doi.org/10.1002/esp.3725

This paper uses detailed mapping of eskers to address three questions which are important for reconstructing meltwater behaviour beneath contemporary and ancient ice masses: ‘What controls the morphology of simple and complex esker systems?’, ‘How do... Read More about Controls on the location, morphology and evolution of complex esker systems at decadal timescales, Breiðamerkurjökull, southeast Iceland.

Ice streams in the Laurentide Ice Sheet: identification, characteristics and comparison to modern ice sheets (2015)
Journal Article
Margold, M., Stokes, C., & Clark, C. (2015). Ice streams in the Laurentide Ice Sheet: identification, characteristics and comparison to modern ice sheets. Earth-Science Reviews, 143, 117-146. https://doi.org/10.1016/j.earscirev.2015.01.011

This paper presents a comprehensive review and synthesis of ice streams in the Laurentide Ice Sheet (LIS) based on a new mapping inventory that includes previously hypothesised ice streams and includes a concerted effort to search for others from acr... Read More about Ice streams in the Laurentide Ice Sheet: identification, characteristics and comparison to modern ice sheets.

Basal topographic controls on rapid retreat of Humboldt Glacier, northern Greenland (2015)
Journal Article
Carr, J., Vieli, A., Stokes, C., Jamieson, S., Palmer, S., Christoffersen, P., …Young, D. (2015). Basal topographic controls on rapid retreat of Humboldt Glacier, northern Greenland. Journal of Glaciology, 61(225), 137-150. https://doi.org/10.3189/2015jog14j128

Discharge from marine-terminating outlet glaciers accounts for up to half the recent mass loss from the Greenland ice sheet, yet the causal factors are not fully understood. Here we assess the factors controlling the behaviour of Humboldt Glacier (HG... Read More about Basal topographic controls on rapid retreat of Humboldt Glacier, northern Greenland.

Geomorphology and weathering characteristics of erratic boulder trains on Tierra del Fuego, southernmost South America: implications for dating of glacial deposits (2015)
Journal Article
Darvill, C. M., Bentley, M. J., & Stokes, C. R. (2015). Geomorphology and weathering characteristics of erratic boulder trains on Tierra del Fuego, southernmost South America: implications for dating of glacial deposits. Geomorphology, 228, 382-397. https://doi.org/10.1016/j.geomorph.2014.09.017

Erratic boulder trains (EBTs) are a useful glacial geomorphological feature because they reveal former ice flow trajectories and can be targeted for cosmogenic nuclide exposure dating. However, understanding how they are transported and deposited is... Read More about Geomorphology and weathering characteristics of erratic boulder trains on Tierra del Fuego, southernmost South America: implications for dating of glacial deposits.