Mountain glaciers of southeast Siberia: current state and changes since the Little Ice Age

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منابع مشابه

Ice Cores , High - Mountain Glaciers , and Climate

The near-global retreat of high-mountain glaciers and the shrinkage of ice fields and ice caps and retreat of their associated outlet glaciers are perhaps the most visible evidence for 20th-century climate change and the recent increase in the globally averaged near-surface temperatures of the Earth’s surface. The loss of high-mountain glaciers—including ice fields, ice caps, and other glaciers...

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Little Ice Age

Volume 1, The Earth system: physical and chemical dimensions of global environmental change, pp 504–509

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Nutrient utilisation and weathering inputs in the Peruvian upwelling region since the Little Ice Age

For this study two sediment cores from the Peruvian shelf covering the time period between the Little Ice Age (LIA) and present were examined for changes in productivity (biogenic opal concentrations (bSi)), nutrient utilisation (stable isotope compositions of silicon (δSiopal) and nitrogen (δNsed)), as well as in ocean circulation and material transport (authigenic and detrital radiogenic neod...

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Evidence for external forcing of the Atlantic Multidecadal Oscillation since termination of the Little Ice Age

The Atlantic Multidecadal Oscillation (AMO) represents a significant driver of Northern Hemisphere climate, but the forcing mechanisms pacing the AMO remain poorly understood. Here we use the available proxy records to investigate the influence of solar and volcanic forcing on the AMO over the last ~450 years. The evidence suggests that external forcing played a dominant role in pacing the AMO ...

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Ice-volume changes of selected glaciers in the Swiss Alps since the end of the 19th century

The evolution of surface topography of glaciers in the Swiss Alps is well documented with high-resolution aerial photographs repeatedly recorded since the 1960s and further back in time with topographic maps including elevation contour lines first surveyed in the mid-19th century. In order to quantify and interpret glacier changes in the Swiss Alps, time series of volume changes over the last 1...

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ژورنال

عنوان ژورنال: Annals of Glaciology

سال: 2014

ISSN: 0260-3055,1727-5644

DOI: 10.3189/2014aog66a135