EVOLUTION OF THE ELBRUS GLACIATION SINCE THE MID XIX CENTURY UNDER CHANGING CLIMATE. KEY FINDINGS OF THE GLACIO-CARTOGRAPHICAL MONITORING
https://doi.org/10.24057/2071-9388-2010-3-2-13-31
Abstract
Quantitative data on changes in the area and volume of the Elbrus glaciation indicated that the greatest rates of its retreat coincided with the 1850–1887 period. Beginning in 1887, the area reduction was occurring practically evenly through time while the decrease in its volume has even slowed down. These facts suggest that global climate warming, which alternated with short-term cooling periods, began in the middle of the XIX century after the end of the Little Ice Age. The warming was most likely due to natural rather than anthropogenic causes.
About the Authors
Yevgeniy ZolotarevRussian Federation
Senior scientist of the Laboratory for Remote Sensing Methods, Department of Cartography, Faculty of Geography, M.V. Lomonosov Moscow State University
Yevgeniy Kharkovets
Russian Federation
Research Associate of the Laboratory for Remote Sensing Methods Department of Cartography, Faculty of Geography, M.V. Lomonosov Moscow State University
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Review
For citations:
Zolotarev Ye., Kharkovets Ye. EVOLUTION OF THE ELBRUS GLACIATION SINCE THE MID XIX CENTURY UNDER CHANGING CLIMATE. KEY FINDINGS OF THE GLACIO-CARTOGRAPHICAL MONITORING. GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY. 2010;3(2):13-31. https://doi.org/10.24057/2071-9388-2010-3-2-13-31