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11 produkter
Earth's Cryosphere and Sea Level Change
Av Lennart Bengtsson, Simeon Koumoutsaris m. fl.
Inbunden, 2011
1096 kr
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This book gives a comprehensive overview of our present understanding of the Earth's cryosphere, its changes and their consequences for mean sea level changes. Since the middle of the 19th century there has been an increase of sea level height by 20-25 cm. Some 8-10 cm of this is due to net losses …
Glacier Fluctuations and Climatic Change
Proceedings of the Symposium on Glacier Fluctuations and Climatic Change, held at Amsterdam, 1–5 June 1987
Inbunden, 1989
2403 kr
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Proceedings of the Symposium on Glacier Fluctuations and Climatic Change, held in Amsterdam, June 1-5, 1987
Ice Sheets and Climate
Av Johannes Oerlemans, C.J. van der Veen
Inbunden, 1984
1096 kr
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Climate modelling is a field in rapid development, and the fltudy of cryospheric processes has become an important part of it. On smaller time scales, the effect of snow cover and sea ice on the atmospheric circulation is of concern for long-range weather forecasting. Thinking in decades or …
Dynamics of the West Antarctic Ice Sheet
Proceedings of a Workshop held in Utrecht, May 6–8, 1985
Av C.J. van der Veen, Johannes Oerlemans
Inbunden, 1986
2185 kr
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Few scientists doubt the prediction that the antropogenic release of carbon dioxide in the atmosphere will lead to some warming of the earth's climate. So there is good reason to investigate the possible effects of such a warming, in dependence of geographical and social economic setting. Many …
Glacier Fluctuations and Climatic Change
Proceedings of the Symposium on Glacier Fluctuations and Climatic Change, held at Amsterdam, 1–5 June 1987
Häftad, 2010
2403 kr
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Proceedings of the Symposium on Glacier Fluctuations and Climatic Change, held in Amsterdam, June 1-5, 1987
Dynamics of the West Antarctic Ice Sheet
Proceedings of a Workshop held in Utrecht, May 6–8, 1985
Av Johannes Oerlemans, C.J. van der Veen
E-bok, 2012
2925 kr
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Few scientists doubt the prediction that the antropogenic release of carbon dioxide in the atmosphere will lead to some warming of the earth''s climate. So there is good reason to investigate the possible effects of such a warming, in dependence of geographical and social economic setting. Many …
Ice Sheets and Climate
Av C.J. van der Veen, Johannes Oerlemans
E-bok, 2012
1459 kr
Lägg i varukorg
Climate modelling is a field in rapid development, and the fltudy of cryospheric processes has become an important part of it. On smaller time scales, the effect of snow cover and sea ice on the atmospheric circulation is of concern for long-range weather forecasting. Thinking in decades or …
Ice Sheets and Climate
Av Johannes Oerlemans, C.J. van der Veen m. fl.
Häftad, 2011
1096 kr
Lägg i varukorg
Climate modelling is a field in rapid development, and the fltudy of cryospheric processes has become an important part of it. On smaller time scales, the effect of snow cover and sea ice on the atmospheric circulation is of concern for long-range weather forecasting. Thinking in decades or …
Dynamics of the West Antarctic Ice Sheet
Proceedings of a Workshop held in Utrecht, May 6–8, 1985
Av C.J. van der Veen, Johannes Oerlemans
Häftad, 2012
2185 kr
Lägg i varukorg
Few scientists doubt the prediction that the antropogenic release of carbon dioxide in the atmosphere will lead to some warming of the earth's climate. So there is good reason to investigate the possible effects of such a warming, in dependence of geographical and social economic setting. Many …
Glacier Fluctuations and Climatic Change
Proceedings of the Symposium on Glacier Fluctuations and Climatic Change, held at Amsterdam, 1–5 June 1987
E-bok, 2013
3251 kr
Lägg i varukorg
Earth's Cryosphere and Sea Level Change
Av Lennart Bengtsson, Simeon Koumoutsaris m. fl.
Häftad, 2014
1096 kr
Lägg i varukorg
This book gives a comprehensive overview of our present understanding of the Earth's cryosphere, its changes and their consequences for mean sea level changes. Since the middle of the 19th century there has been an increase of sea level height by 20-25 cm. Some 8-10 cm of this is due to net losses …
