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Published by KIuwer Academic Publ., 2003
ISBN 10: 1402013868 ISBN 13: 9781402013867
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Published by Springer Netherlands, 2003
ISBN 10: 1402013868 ISBN 13: 9781402013867
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Add to basketCondition: Good. Your purchase helps support Sri Lankan Children's Charity 'The Rainbow Centre'. Ex-library, so some stamps and wear, but in good overall condition. Our donations to The Rainbow Centre have helped provide an education and a safe haven to hundreds of children who live in appalling conditions.
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ISBN 10: 1507809530 ISBN 13: 9781507809532
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Published by Dordrecht, Boston, London : Kluwer Academic Publishers, 2003
ISBN 10: 1402013868 ISBN 13: 9781402013867
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Condition: Wie neu. 282 S : Ill., graph. Darst., Tab., Kt.; 6740 Sprache: Englisch Gewicht in Gramm: 656 24,5 cm, gebundene Ausgabe, sehr guter Zustand! Reprinted from Climatic Change, Vol. 59, Nos. 1-2, 2003; Sprache: Englisch;.
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Published by Kluwer Academic Publishers, 2003
ISBN 10: 1402013868 ISBN 13: 9781402013867
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Condition: New. Reviews climatic trends in high elevation regions of the world, assessing the reliability of various environmental indicators that can be used for monitoring climatic change, and assessing whether physical impacts of climatic change in high elevation areas are becoming evident. Editor(s): Diaz, Henry F. Series: Advances in Global Change Research. Num Pages: 283 pages, 112 black & white illustrations, 10 colour illustrations, biography. BIC Classification: RBP; RNPG. Category: (P) Professional & Vocational; (UP) Postgraduate, Research & Scholarly; (UU) Undergraduate. Dimension: 235 x 155 x 18. Weight in Grams: 655. . 2003. Hardback. . . . .
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Taschenbuch. Condition: Neu. Climate Variability and Change in High Elevation Regions: Past, Present & Future | Henry F. Diaz | Taschenbuch | Advances in Global Change Research | vi | Englisch | 2010 | Springer | EAN 9789048163229 | Verantwortliche Person für die EU: Springer Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg, juergen[dot]hartmann[at]springer[dot]com | Anbieter: preigu.
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Add to basketHardcover. Condition: Brand New. reprint edition. 282 pages. 9.50x6.50x0.75 inches. In Stock.
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Published by Kluwer Academic Publishers, 2003
ISBN 10: 1402013868 ISBN 13: 9781402013867
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Condition: New. Reviews climatic trends in high elevation regions of the world, assessing the reliability of various environmental indicators that can be used for monitoring climatic change, and assessing whether physical impacts of climatic change in high elevation areas are becoming evident. Editor(s): Diaz, Henry F. Series: Advances in Global Change Research. Num Pages: 283 pages, 112 black & white illustrations, 10 colour illustrations, biography. BIC Classification: RBP; RNPG. Category: (P) Professional & Vocational; (UP) Postgraduate, Research & Scholarly; (UU) Undergraduate. Dimension: 235 x 155 x 18. Weight in Grams: 655. . 2003. Hardback. . . . . Books ship from the US and Ireland.
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Published by Springer Netherlands, Springer, 2010
ISBN 10: 9048163226 ISBN 13: 9789048163229
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Taschenbuch. Condition: Neu. Druck auf Anfrage Neuware - Printed after ordering - Glaciers in the Andes are particularly important natural archives of present and past climatic and environmental changes, in significant part because of the N-S trend of this topographic barrier and its influence on the atmospheric circulation of the southern hemisphere. Strong gradients in the seasonality and amount of precipitation exist between the equator and 30° S. Large differences in amount east and west of the Andean divide also occur, as well as a change from tropical summer precipitation (additionally modified by the seasonal shift of the circulation belts) to winter precipitation in the west wind belt (e. g. , Yuille, 1999; Garraud and Aceituno, 2001). The so-called 'dry axis' lies between the tropical and extra tropical precipitation regimes (Figure 1). The high mountain desert within this axis responds most sensitively to the smallest changes in effective moisture. An important hydro-meteorological feature on a seasonal to inter-annual time-scale is the occurrence of EN SO events, which strongly control the mass balance of glaciers in this area (e. g. , Wagnon et ai. , 2001; Francou et ai. , in press). The precipitation pattern is an important factor for the interpretation of climatic and environmental records extracted from ice cores, because much of this information is related to conditions at the actual time of precipitation, and this is especially so for stable isotope records. Several ice cores have recently been drilled to bedrock in this area. From Huascanin (Thompson et ai. , 1995), Sajama (Thompson et ai.
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Published by Springer Netherlands, 2010
ISBN 10: 9048163226 ISBN 13: 9789048163229
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Published by Springer Netherlands, Springer Netherlands, 2003
ISBN 10: 1402013868 ISBN 13: 9781402013867
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Buch. Condition: Neu. Druck auf Anfrage Neuware - Printed after ordering - Glaciers in the Andes are particularly important natural archives of present and past climatic and environmental changes, in significant part because of the N-S trend of this topographic barrier and its influence on the atmospheric circulation of the southern hemisphere. Strong gradients in the seasonality and amount of precipitation exist between the equator and 30° S. Large differences in amount east and west of the Andean divide also occur, as well as a change from tropical summer precipitation (additionally modified by the seasonal shift of the circulation belts) to winter precipitation in the west wind belt (e. g. , Yuille, 1999; Garraud and Aceituno, 2001). The so-called 'dry axis' lies between the tropical and extra tropical precipitation regimes (Figure 1). The high mountain desert within this axis responds most sensitively to the smallest changes in effective moisture. An important hydro-meteorological feature on a seasonal to inter-annual time-scale is the occurrence of EN SO events, which strongly control the mass balance of glaciers in this area (e. g. , Wagnon et ai. , 2001; Francou et ai. , in press). The precipitation pattern is an important factor for the interpretation of climatic and environmental records extracted from ice cores, because much of this information is related to conditions at the actual time of precipitation, and this is especially so for stable isotope records. Several ice cores have recently been drilled to bedrock in this area. From Huascanin (Thompson et ai. , 1995), Sajama (Thompson et ai.
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Published by H N H International Limited, 2022
ISBN 10: 1032061596 ISBN 13: 9781032061597
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