Glaciers and Global Warming
Ice core and mass balance studies from glaciers, ice caps and ice sheets constitute an ideal medium for monitoring and studying present and past environmental change and, as such, make a valuable contribution to the present debate over anthropogenic forcing of climate. Data derived from 32 years of...
| Published in: | Géographie physique et Quaternaire |
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| Main Authors: | , |
| Format: | Text |
| Language: | English |
| Published: |
Les Presses de l'Université de Montréal
1995
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| Subjects: | |
| Online Access: | http://id.erudit.org/iderudit/033064ar https://doi.org/10.7202/033064ar |
| Summary: | Ice core and mass balance studies from glaciers, ice caps and ice sheets constitute an ideal medium for monitoring and studying present and past environmental change and, as such, make a valuable contribution to the present debate over anthropogenic forcing of climate. Data derived from 32 years of measurements in the Canadian Arctic show no significant trends in glacier mass balance, ice melt, or snow accumulation, although the mass balance continues to be slightly negative. Models suggest that industrial aerosol loading of the atmosphere should add to the warming effect of greenhouse gases. However, we have found a sharp increase in the concentration of industrial pollutants in snow deposited since the early 1950's which makes the trendless nature of our various time series surprising. Spatial differences in the nature of climatic change may account for the lack of trend in the Queen Elizabeth Islands but encourages similar investigations to this study elsewhere in the circumpolar region. A global warming trend over the past 150 years has been demonstrated from instrumental data and is evident in our ice cores. However, the ice core data and glacier geometry changes in the Canadian Arctic suggest the Arctic warming is more pronounced in summer than winter. The same warming trend is not unique when viewed in the context of changes over the past 10,000 or 100,000 years. This suggests the 150-year trend is part of the natural climate variability. L'analyse des carottes de glace et les mesures du bilan de masse des glaciers, des calottes glaciaires et des indlandsis permettent de déceler des changements environnementaux survenus dans le passé tout en permettant de surveiller les changements actuels. Ces études peuvent contribuer au débat portant sur les conséquences physiques de l'activité humaine sur le climat. Trente-deux ans de données accumulées sur les bilans de masse, la fonte et l'accumulation de neige sur les glaciers de l'Arctique canadien ne montrent aucune tendance significative, bien que les bilans ... |
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