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Titlebook: Glacier Fluctuations and Climatic Change; Proceedings of the S Johannes Oerlemans Conference proceedings 1989 Springer Science+Business Med

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Mass Balance History of Blue Glacier, Washington, USA, balance record into the future to a time period adequate for the testing of glacier dynamics models. Initial analysis indicates a good correlation between mass balance and equilibrium line altitude (ELA).
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Hydrometeorological Conditions, Mass Balance and Runoff from Alpine Glaciers,using the catch of totalizing raingauges emptied at roughly half-yearly intervals, for which reasonable levels of correlation exist between valley and mountain gauges..Summer air temperatures averaged over the months May through September and June through August are highly positively correlated with
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The Evolution of the Englacial Temperature Distribution in the Superimposed Ice Zone of a Polar Ice to be considerable. In the second kind of experiments the measured temperature at the interannual surface was used as boundary condition, and to start with the temperature below the interannual surface could only be affected by conduction. The measured and the calculated temperatures match until me
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https://doi.org/10.1007/978-3-322-94099-5s on a marine shelf. Two units consisting of interglacial sediments are interbedded in the massive diamictites..The two macro-scale glaciation periods, following no systematic pattern in southwestern Gondwana, occurred during a cool to cold climatic period lasting for about 270 Ma from the mid-Cambr
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Karl Volger,Erhard Laasch,Erhard Laasch00 yrs BP). Moraines, formerly mapped by other workers as mid-Holocene glacial deposits, are considered to date from recession of valley ice during the late glacial (−12,000 yrs BP). Ice advance during the last glacial (Liki Glaciation) presumably began < 100,000 yrs BP, ending −15,000 yrs BP, and r
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https://doi.org/10.1007/978-3-8348-9900-2or advances also culminated before 3100 BP, and between 1400–1200 BP. In the tenth century AD the glacier was also longer than during the Little Ice Age (1600–1900 AD). In contrast, Klifurárjökull and all the outlets of Eyjafjallajökull reached a maximum Holocene extent during the Little Ice Age. Th
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,Trinkwasserversorgung — Kaltwasseranschluß,moraine bank. The scale of late Holocene-Little Ice Age glacier advances in South Georgia was small by mid-latitude standards, possibly because of the relatively arid environment in the lee side of the island.
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