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Luke Copland
University of Ottawa
GlacierOceanographyGeomorphologyGeologySea ice
106Publications
28H-index
2,239Citations
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Publications 106
Newest
#1Scott N. Williamson (U of O: University of Ottawa)H-Index: 9
#2Luke Copland (U of O: University of Ottawa)H-Index: 28
Last. David Burgess (NRCan: Natural Resources Canada)H-Index: 20
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Abstract Mass balance measurements in the Canadian Arctic are limited, particularly for smaller glaciers, which introduces significant uncertainties in regional mass balance assessment. Here we report on the correlations between Moderate Resolution Imaging Spectroradiometer (MODIS) Terra albedo measurements (Version 6) and net annual mass balance for five glaciers in the Canadian Arctic over the period 2002–2016. Three glacier albedo aggregation methods are tested for the melt season (June, July...
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#1Nicole Schaffer (University of La Serena)H-Index: 5
#2Luke Copland (U of O: University of Ottawa)H-Index: 28
Last. Johan Nilsson (California Institute of Technology)H-Index: 5
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#1William Kochtitzky (UMaine: University of Maine)H-Index: 2
#2D. Winski (UMaine: University of Maine)H-Index: 6
Last. Hester Jiskoot (U of L: University of Lethbridge)H-Index: 17
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Links between climate and glacier surges are poorly understood but are required to enable prediction of surges and mitigation of associated hazards. Here, we investigate the role of snow accumulati...
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#1Naomi E. Ochwat (U of C: University of Calgary)
#2Shawn J. Marshall (U of C: University of Calgary)H-Index: 32
Last. Luke Copland (U of O: University of Ottawa)H-Index: 28
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Abstract. In recent years, the analysis of firn in Greenland, Svalbard, and other high Arctic regions has contributed to the understanding of meltwater retention in firn and its importance to measurements of glacier mass balance. This has provided insight into firn densification processes and meltwater retention. Changes in these attributes can also provide insight into meteorological variability and climate trends. In spring 2018, two firn cores (21 m and 36 m in length) were extracted from the...
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#1William Kochtitzky (U of O: University of Ottawa)H-Index: 1
#2Luke Copland (U of O: University of Ottawa)H-Index: 28
Last. Christine F. Dow (UW: University of Waterloo)H-Index: 11
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Recent surges of Dan Zhur (Donjek) Glacier have formed lakes at the glacier terminus which have drained catastrophically, resulting in hazards to people and infrastructure downstream. Here we use a...
1 CitationsSource
#1Scott N. Williamson (U of O: University of Ottawa)
#1Scott N. Williamson (U of O: University of Ottawa)H-Index: 9
Last. David S. Hik (SFU: Simon Fraser University)H-Index: 38
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AbstractThe climate of high, mid-latitude mountains appears to be warming faster than the global average, but evidence for such elevation-dependent warming (EDW) at higher latitudes is presently sc...
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#1Wesley Van Wychen (UW: University of Waterloo)H-Index: 6
#1Wesley Van WychenH-Index: 2
Last. David Burgess (NRCan: Natural Resources Canada)H-Index: 20
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The islands of the Canadian Arctic, known as the Canadian Arctic Archipelago (CAA), contain the largest area of glacierized terrain outside of the ice sheets of Greenland and Antarctica. The ice masses are focused in the eastern part of the CAA, and stretch from the ice shelves of northernmost Ellesmere Island to glaciers in the southernmost parts of Baffin Island, together with a few mountain glaciers in northern Labrador. The majority of glacier ice (roughly 70%) is contained within the large ...
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#2Luke CoplandH-Index: 28
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#1Abigail Dalton (U of O: University of Ottawa)H-Index: 1
#2Luke Copland (U of O: University of Ottawa)H-Index: 28
Last. Alison Cook (U of O: University of Ottawa)H-Index: 1
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ABSTRACTSince the 1960s, warming air and sea surface temperatures have led to decreasing sea ice extent and longer periods of open water in the Canadian Arctic Archipelago (CAA), together with chan...
1 CitationsSource
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