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  • Lingua: Inglese

    Editore: LAP LAMBERT Academic Publishing, 2010

    3838345789 / 9783838345789

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    Da: Buchpark, Trebbin, GermaniaBuchpark

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    Prezzo corrente: EUR 31,36

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    Condizione: Sehr gut. Zustand: Sehr gut | Sprache: Englisch | Produktart: Bücher | Using an Earth Model of Intermediate Complexity, experiments are performed during the Holocene to study the seasonality of precipitation in Greenland, the effect on the interpretation of ice core signals, and possible mechanisms that can account for the sudden decrease in temperature seen in ice cores from Greenland 8.2 kyr ago. Throughout the Holocene orbital parameters have changed resulting in an increase of the meridional gradient of the annual mean solar forcing. These changes influence the seasonality of Greenland precipitation. The isotope signal in ice cores are precipitation weighted, meaning that a signal is only recorded when it snows, and a change in the seasonality of precipitation will thus cause a bias in the signal. ¿O18 records from Greenland ice cores show a large excursion 8.2 kyr ago. It is believed that the event is caused by freshwater discharges originating from the melting of the Laurentide ice sheet. Orbital and freshwater forcings are built into the circulation model ECBilt-CLIO, and the results will give an indication of the ice core bias and the effects on regional and global climate.…

  • Lingua: Inglese

    Editore: LAP Lambert Academic Publishing, 2010

    3838345789 / 9783838345789

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    Da: Mispah books, Redhill, SURRE, Regno UnitoMispah books

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    Condizione: Usato - Come nuovo

    EUR 148,14

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    paperback. Condizione: Like New. LIKE NEW. SHIPS FROM MULTIPLE LOCATIONS. book.

  • Lingua: Inglese

    Editore: LAP LAMBERT Academic Publishing Feb 2010, 2010

    3838345789 / 9783838345789

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    Da: BuchWeltWeit Ludwig Meier e.K., Bergisch Gladbach, GermaniaBuchWeltWeit Ludwig Meier e.K.

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    EUR 49,00

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    Taschenbuch. Condizione: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -Using an Earth Model of Intermediate Complexity, experiments are performed during the Holocene to study the seasonality of precipitation in Greenland, the effect on the interpretation of ice core signals, and possible mechanisms that can account for the sudden decrease in temperature seen in ice cores from Greenland 8.2 kyr ago. Throughout the Holocene orbital parameters have changed resulting in an increase of the meridional gradient of the annual mean solar forcing. These changes influence the seasonality of Greenland precipitation. The isotope signal in ice cores are precipitation weighted, meaning that a signal is only recorded when it snows, and a change in the seasonality of precipitation will thus cause a bias in the signal. O18 records from Greenland ice cores show a large excursion 8.2 kyr ago. It is believed that the event is caused by freshwater discharges originating from the melting of the Laurentide ice sheet. Orbital and freshwater forcings are built into the circulation model ECBilt-CLIO, and the results will give an indication of the ice core bias and the effects on regional and global climate. 116 pp. Englisch.…

  • Lingua: Inglese

    Editore: LAP LAMBERT Academic Publishing, 2010

    3838345789 / 9783838345789

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    Da: AHA-BUCH GmbH, Einbeck, GermaniaAHA-BUCH GmbH

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    Condizione: Nuovo

    EUR 54,71

    EUR 35,00 spedizione 
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    Taschenbuch. Condizione: Neu. nach der Bestellung gedruckt Neuware - Printed after ordering - Using an Earth Model of Intermediate Complexity, experiments are performed during the Holocene to study the seasonality of precipitation in Greenland, the effect on the interpretation of ice core signals, and possible mechanisms that can account for the sudden decrease in temperature seen in ice cores from Greenland 8.2 kyr ago. Throughout the Holocene orbital parameters have changed resulting in an increase of the meridional gradient of the annual mean solar forcing. These changes influence the seasonality of Greenland precipitation. The isotope signal in ice cores are precipitation weighted, meaning that a signal is only recorded when it snows, and a change in the seasonality of precipitation will thus cause a bias in the signal. O18 records from Greenland ice cores show a large excursion 8.2 kyr ago. It is believed that the event is caused by freshwater discharges originating from the melting of the Laurentide ice sheet. Orbital and freshwater forcings are built into the circulation model ECBilt-CLIO, and the results will give an indication of the ice core bias and the effects on regional and global climate. …

  • Lingua: Inglese

    Editore: LAP LAMBERT Academic Publishing, 2010

    3838345789 / 9783838345789

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    Da: moluna, Greven, Germaniamoluna

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    EUR 41,05

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    Condizione: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Autor/Autorin: Wang Peter RiddersholmPeter Riddersholm Wang: M.Sc. in Geophysics from the Niels Bohr Institute at the University of Copenhagen, Denmark. Main fields of study include complex climate processes and ice core theory.Using an Earth M.…

  • Lingua: Inglese

    Editore: LAP LAMBERT Academic Publishing Feb 2010, 2010

    3838345789 / 9783838345789

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    Da: buchversandmimpf2000, Emtmannsberg, BAYE, Germaniabuchversandmimpf2000

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    Condizione: Nuovo

    EUR 49,00

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    Taschenbuch. Condizione: Neu. This item is printed on demand - Print on Demand Titel. Neuware -Using an Earth Model of Intermediate Complexity, experiments are performed during the Holocene to study the seasonality of precipitation in Greenland, the effect on the interpretation of ice core signals, and possible mechanisms that can account for the sudden decrease in temperature seen in ice cores from Greenland 8.2 kyr ago. Throughout the Holocene orbital parameters have changed resulting in an increase of the meridional gradient of the annual mean solar forcing. These changes influence the seasonality of Greenland precipitation. The isotope signal in ice cores are precipitation weighted, meaning that a signal is only recorded when it snows, and a change in the seasonality of precipitation will thus cause a bias in the signal. ¿O18 records from Greenland ice cores show a large excursion 8.2 kyr ago. It is believed that the event is caused by freshwater discharges originating from the melting of the Laurentide ice sheet. Orbital and freshwater forcings are built into the circulation model ECBilt-CLIO, and the results will give an indication of the ice core bias and the effects on regional and global climate.VDM Verlag, Dudweiler Landstraße 99, 66123 Saarbrücken 116 pp. Englisch. …