Recession of the southern part of Barnes Ice Cap, Baffin Island, Canada, between 1961 and 1993, determined from digital mapping of Landsat TM

Changes along the margin of the southern half of the 5900 km 2 Barnes Ice Cap have been assessed using 1993 Landsat TM imagery in comparison with digitized 1: 50 000 NTS maps based on 1961 photogrammetry. The average recession over the 183 km long southern perimeter was found to be at least 4 m a -1 , with no significant difference between the southeast and southwest sectors. Viewed in conjunction with the sustained retreat previously reported for the northwest margin, these results indicate that a general reduction in the size of Barnes Ice Cap is occurring. The present retreat phase began under a regional climate warming in the late 19th to early 20th century period and continues, while the record of the ablation-season temperature since the midcentury has not shown any significant trend.

[1]  G. Holdsworth Evidence of a Surge on Barnes Ice Cap, Baffin Island , 1973 .

[2]  B. Hanson,et al.  Changes in mass balance, velocity, and surface profile along a flow line on Barnes Ice Cap, 1970–1984 , 1987 .

[3]  Joan E. Luther,et al.  Recent Changes at the Northwest Margin of the Barnes Ice Cap, Baffin Island, N.W.T., Canada , 1993, Arctic and Alpine Research.

[4]  P. Jones,et al.  Variations in Surface Air Temperatures: Part 2. Arctic Regions, 1881–1980 , 1982 .

[5]  John E. Walsh,et al.  Recent Variations of Sea Ice and Air Temperature in High Latitudes , 1993 .

[6]  P. D. Baird Part I: Method of Nourishment of the Barnes Ice Cap , 1952, Journal of Glaciology.

[7]  M. Mahaffy A three‐dimensional numerical model of ice sheets: Tests on the Barnes Ice Cap, Northwest Territories , 1976 .

[8]  P. Chavez An improved dark-object subtraction technique for atmospheric scattering correction of multispectral data , 1988 .

[9]  J. Jacobs Spatial Representativeness of Climatic Data from Baffin Island, N.W.T., with Implications for Muskoxen and Caribou Distribution , 1989 .

[10]  J. Ives Indications of Recent Extensive Glacierization in North–Central Baffin Island, N.W.T. , 1962, Journal of Glaciology.

[11]  Dorothy K. Hall,et al.  Analysis of glacier facies using satellite techniques , 1991, Journal of Glaciology.

[12]  R. Hooke Pleistocene Ice at the Base of The Barnes Ice Cap, Baffin Island, N.W.T., Canada , 1976 .

[13]  W. H. Ward The glaciological studies of the Baffin Island Expedition, 1950. Part II: The physics of deglaciation in central Baffin Island , 1952 .

[14]  Tómas Jóhannesson,et al.  Time–Scale for Adjustment of Glaciers to Changes in Mass Balance , 1989, Journal of Glaciology.

[15]  John F Nye,et al.  The response of glaciers and ice-sheets to seasonal and climatic changes , 1960, Proceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences.

[16]  R. Gustafson,et al.  Temperature profiles in the Barnes Ice Cap, Baffin Island, Canada, and heat flux from the subglacial terrane , 1980 .

[17]  R. Hooke Flow near the Margin of the Barnes Ice Cap, and the Development of Ice-Cored Moraines , 1973 .

[18]  J. Foster,et al.  Comparison of in situ and Landsat derived reflectance of Alaskan glaciers , 1989 .

[19]  The glaciological studies of the Baffin Island Expedition, 1950. Part IV: The heat exchange at the surface of the Barnes Ice Cap during the ablation period , 1953 .

[20]  W. H. Ward,et al.  The Glaciological Studies of the Baffin Island Expedition, 1950 , 1952 .