Hasil Pencarian - M. Claussen

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  1. 1
    Late Quaternary vegetation-climate feedbacks

    Late Quaternary vegetation-climate feedbacks oleh M. Claussen*

    Diterbitkan 2009-06-01
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  2. 2
    Simulated range of mid-Holocene precipitation changes from extended lakes and wetlands over North Africa

    Simulated range of mid-Holocene precipitation changes from extended lakes and wetlands over North Africa oleh N. F. Specht, M. Claussen, M. Claussen, T. Kleinen

    Diterbitkan 2022-05-01
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  3. 3
    Influence of the representation of convection on the mid-Holocene West African Monsoon

    Influence of the representation of convection on the mid-Holocene West African Monsoon oleh L. Jungandreas, C. Hohenegger, M. Claussen, M. Claussen

    Diterbitkan 2021-08-01
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  4. 4
    Dynamic interaction between lakes, climate, and vegetation across northern Africa during the mid-Holocene

    Dynamic interaction between lakes, climate, and vegetation across northern Africa during the mid-Holocene oleh N. F. Specht, M. Claussen, M. Claussen, T. Kleinen

    Diterbitkan 2024-07-01
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  5. 5
    Rapid increase in simulated North Atlantic dust deposition due to fast change of northwest African landscape during the Holocene

    Rapid increase in simulated North Atlantic dust deposition due to fast change of northwest African landscape during the Holocene oleh S. Egerer, S. Egerer, M. Claussen, M. Claussen, C. Reick

    Diterbitkan 2018-07-01
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  6. 6
    Harmonising plant functional type distributions for evaluating Earth system models

    Harmonising plant functional type distributions for evaluating Earth system models oleh A. Dallmeyer, M. Claussen, M. Claussen, V. Brovkin

    Diterbitkan 2019-02-01
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  7. 7
    The end of the African humid period as seen by a transient comprehensive Earth system model simulation of the last 8000 years

    The end of the African humid period as seen by a transient comprehensive Earth system model simulation of the last 8000 years oleh A. Dallmeyer, M. Claussen, M. Claussen, S. J. Lorenz, T. Shanahan

    Diterbitkan 2020-01-01
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  8. 8
    Two drastically different climate states on an Earth-like terra-planet

    Two drastically different climate states on an Earth-like terra-planet oleh S. Kalidindi, S. Kalidindi, C. H. Reick, T. Raddatz, M. Claussen, M. Claussen

    Diterbitkan 2018-06-01
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  9. 9
    How does the explicit treatment of convection alter the precipitation–soil hydrology interaction in the mid-Holocene African humid period?

    How does the explicit treatment of convection alter the precipitation–soil hydrology interaction in the mid-Holocene African humid period? oleh L. Jungandreas, L. Jungandreas, C. Hohenegger, M. Claussen, M. Claussen

    Diterbitkan 2023-03-01
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  10. 10
    Transitivity of the climate–vegetation system in a warm climate

    Transitivity of the climate–vegetation system in a warm climate oleh U. Port, M. Claussen

    Diterbitkan 2015-11-01
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  11. 11
    Simulated climate variability in the region of Rapa Nui during the last millennium

    Simulated climate variability in the region of Rapa Nui during the last millennium oleh C. Junk, M. Claussen

    Diterbitkan 2011-06-01
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  12. 12
    Implications of land use change in tropical northern Africa under global warming

    Implications of land use change in tropical northern Africa under global warming oleh T. Brücher, M. Claussen, T. Raddatz

    Diterbitkan 2015-12-01
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  13. 13
    The influence of land cover change in the Asian monsoon region on present-day and mid-Holocene climate

    The influence of land cover change in the Asian monsoon region on present-day and mid-Holocene climate oleh A. Dallmeyer, M. Claussen

    Diterbitkan 2011-06-01
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  14. 14
    Quantifying the effect of vegetation dynamics on the climate of the Last Glacial Maximum

    Quantifying the effect of vegetation dynamics on the climate of the Last Glacial Maximum oleh A. Jahn, A. Jahn, M. Claussen, M. Claussen, A. Ganopolski, V. Brovkin

    Diterbitkan 2005-01-01
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  15. 15
    Earth system model simulations show different feedback strengths of the terrestrial carbon cycle under glacial and interglacial conditions

    Earth system model simulations show different feedback strengths of the terrestrial carbon cycle under glacial and interglacial conditions oleh M. Adloff, M. Adloff, M. Adloff, C. H. Reick, M. Claussen, M. Claussen

    Diterbitkan 2018-04-01
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  16. 16
    Effects of orbital forcing, greenhouse gases and ice sheets on Saharan greening in past and future multi-millennia

    Effects of orbital forcing, greenhouse gases and ice sheets on Saharan greening in past and future multi-millennia oleh M. Duque-Villegas, M. Duque-Villegas, M. Claussen, M. Claussen, V. Brovkin, T. Kleinen

    Diterbitkan 2022-08-01
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  17. 17
    What was the source of the atmospheric CO<sub>2</sub> increase during the Holocene?

    What was the source of the atmospheric CO<sub>2</sub> increase during the Holocene? oleh V. Brovkin, S. Lorenz, T. Raddatz, T. Ilyina, I. Stemmler, M. Toohey, M. Claussen, M. Claussen

    Diterbitkan 2019-07-01
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  18. 18
    Detecting hotspots of atmosphere–vegetation interaction via slowing down &ndash; Part 2: Application to a global climate model

    Detecting hotspots of atmosphere–vegetation interaction via slowing down &ndash; Part 2: Application to a global climate model oleh S. Bathiany, M. Claussen, K. Fraedrich

    Diterbitkan 2013-02-01
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  19. 19
    Strength of forest-albedo feedback in mid-Holocene climate simulations

    Strength of forest-albedo feedback in mid-Holocene climate simulations oleh J. Otto, T. Raddatz, M. Claussen

    Diterbitkan 2011-09-01
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  20. 20
    Detecting hotspots of atmosphere–vegetation interaction via slowing down &ndash; Part 1: A stochastic approach

    Detecting hotspots of atmosphere–vegetation interaction via slowing down &ndash; Part 1: A stochastic approach oleh S. Bathiany, M. Claussen, K. Fraedrich

    Diterbitkan 2013-02-01
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