Snow cover monitoring in the Northern Patagonia Icefield using MODIS satellite images (2000-2006)

被引:47
|
作者
Lopez, Paulina [1 ]
Sirguey, Pascal [2 ]
Arnaud, Yves [3 ]
Pouyaud, Bernard [1 ]
Chevallier, Pierre [1 ]
机构
[1] IRD, F-34095 Montpellier, France
[2] Univ Otago, Sch Surveying, GLIMS New Zealand Off, Dunedin, New Zealand
[3] IRD, Lab Glaciol & Geophys Environm, F-38402 St Martin Dheres, France
关键词
climate change; snow cover; Patagonia; low resolution satellite images;
D O I
10.1016/j.gloplacha.2007.07.005
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The snow cover of the Northern Patagonia Icefield (NPI) was monitored after applying the Normalized Difference Snow Index (NDSI) and the Red/NIR band ratio to 134 Moderate Resolution Imaging Spectroradiometer (MODIS) images captured between 2000 and 2006. The final results show that the snow cover extent of the NPI fluctuates a lot in winter, in addition to its seasonal behaviour. The minimum snow cover extent of the period (3600 km(2)) was observed in March 2000 and the maximum (11,623 km(2)) in August 2001. We found that temperature accounts for approximately 76% of the variation of the snow cover extent over the entire icefield. We also show two different regimes of winter snow cover fluctuations corresponding to the eastern and the western sides of the icefield. The seasonality of the snow cover on the western side was determined by temperature rather than precipitation, while on the east side the seasonality of the snow cover was influenced by the seasonal behaviour of both temperature and precipitation. This difference can be explained by the two distinct climates: coastal and continental. The fluctuations in the winter snow cover extent were more pronounced and less controlled by temperature on the western side than on the eastern side of the icefield. Snow cover extent was correlated with temperature R-2 = 0.75 and R-2 = 0.74 for the western and eastern sides, respectively. Since limited meteorological data are available in this region, our investigation confirmed that the change in snow cover is an interesting climatic indicator over the NPI providing important insights in mass balance comprehension. Since snow and ice were distinguished snow cover fluctuations can be associated to fluctuations in the snow accumulation area of the NPI. In addition, days with minimum snow covers of summer season can be associated to the period in which Equilibrium Line Altitude (ELA) is the highest. (c) 2007 Elsevier B.V All rights reserved.
引用
收藏
页码:103 / 116
页数:14
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