Showing 41 - 60 results of 541 for search '"Max Planck Institute for Meteorology"', query time: 0.14s Refine Results
  1. 41
    Radiative forcing and feedback by forests in warm climates – a sensitivity study

    Radiative forcing and feedback by forests in warm climates – a sensitivity study by U. Port, M. Claussen, V. Brovkin

    Published 2016-07-01
    “…We evaluate the radiative forcing of forests and the feedbacks triggered by forests in a warm, basically ice-free climate and in a cool climate with permanent high-latitude ice cover using the Max Planck Institute for Meteorology Earth System Model. As a paradigm for a warm climate, we choose the early Eocene, some 54 to 52  million years ago, and for the cool climate, the pre-industrial climate, respectively. …”
    Get full text
    Article
  2. 42
    Input-driven versus turnover-driven controls of simulated changes in soil carbon due to land-use change

    Input-driven versus turnover-driven controls of simulated changes in soil carbon due to land-use change by S S Nyawira, J E M S Nabel, V Brovkin, J Pongratz

    Published 2017-01-01
    Get full text
    Article
  3. 43
    Heinrich events show two-stage climate response in transient glacial simulations

    Heinrich events show two-stage climate response in transient glacial simulations by F. A. Ziemen, M.-L. Kapsch, M. Klockmann, U. Mikolajewicz

    Published 2019-01-01
    Get full text
    Article
  4. 44
    Representation of soil hydrology in permafrost regions may explain large part of inter-model spread in simulated Arctic and subarctic climate

    Representation of soil hydrology in permafrost regions may explain large part of inter-model spread in simulated Arctic and subarctic climate by P. de Vrese, G. Georgievski, J. F. Gonzalez Rouco, D. Notz, T. Stacke, N. J. Steinert, S. Wilkenskjeld, V. Brovkin, V. Brovkin

    Published 2023-05-01
    Get full text
    Article
  5. 45
    Timescales of the permafrost carbon cycle and legacy effects of temperature overshoot scenarios

    Timescales of the permafrost carbon cycle and legacy effects of temperature overshoot scenarios by Philipp de Vrese, Victor Brovkin

    Published 2021-05-01
    Get full text
    Article
  6. 46
    Extreme heat and drought typical of an end-of-century climate could occur over Europe soon and repeatedly

    Extreme heat and drought typical of an end-of-century climate could occur over Europe soon and repeatedly by Laura Suarez-Gutierrez, Wolfgang A. Müller, Jochem Marotzke

    Published 2023-11-01
    Get full text
    Article
  7. 47
    How Useful Is a Linear Ozone Parameterization for Global Climate Modeling?

    How Useful Is a Linear Ozone Parameterization for Global Climate Modeling? by Katharina Meraner, Sebastian Rast, Hauke Schmidt

    Published 2020-04-01
    Get full text
    Article
  8. 48
    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? by V. Brovkin, S. Lorenz, T. Raddatz, T. Ilyina, I. Stemmler, M. Toohey, M. Claussen, M. Claussen

    Published 2019-07-01
    Get full text
    Article
  9. 49
    Dynamic hydrological discharge modelling for coupled climate model simulations of the last glacial cycle: the MPI-DynamicHD model version 3.0

    Dynamic hydrological discharge modelling for coupled climate model simulations of the last glacial cycle: the MPI-DynamicHD model version 3.0 by T. Riddick, V. Brovkin, S. Hagemann, S. Hagemann, U. Mikolajewicz

    Published 2018-10-01
    Get full text
    Article
  10. 50
    Controls on fire activity over the Holocene

    Controls on fire activity over the Holocene by S. Kloster, T. Brücher, V. Brovkin, S. Wilkenskjeld

    Published 2015-05-01
    Get full text
    Article
  11. 51
    More accurate quantification of model-to-model agreement in externally forced climatic responses over the coming century

    More accurate quantification of model-to-model agreement in externally forced climatic responses over the coming century by Nicola Maher, Scott B. Power, Jochem Marotzke

    Published 2021-02-01
    Get full text
    Article
  12. 52
    Transitivity of the climate–vegetation system in a warm climate

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

    Published 2015-11-01
    “…We use the Earth system model of the Max Planck Institute for Meteorology to analyse the stability of the climate system under early Eocene and pre-industrial conditions. …”
    Get full text
    Article
  13. 53
    Seasonal aspects of the quasi‐biennial oscillation in the Max Planck Institute Earth System Model and ERA‐40

    Seasonal aspects of the quasi‐biennial oscillation in the Max Planck Institute Earth System Model and ERA‐40 by Thomas R. Krismer, Marco A. Giorgetta, Monika Esch

    Published 2013-06-01
    Get full text
    Article
  14. 54
    Background albedo dynamics improve simulated precipitation variability in the Sahel region

    Background albedo dynamics improve simulated precipitation variability in the Sahel region by F. S. E. Vamborg, V. Brovkin, M. Claussen

    Published 2014-02-01
    Get full text
    Article
  15. 55
    Impact of resolution on large-eddy simulation of midlatitude summertime convection

    Impact of resolution on large-eddy simulation of midlatitude summertime convection by C. Moseley, C. Moseley, I. Pscheidt, G. Cioni, R. Heinze

    Published 2020-03-01
    Get full text
    Article
  16. 56
    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 by M. Duque-Villegas, M. Duque-Villegas, M. Claussen, M. Claussen, V. Brovkin, T. Kleinen

    Published 2022-08-01
    Get full text
    Article
  17. 57
    Analysis of the surface mass balance for deglacial climate simulations

    Analysis of the surface mass balance for deglacial climate simulations by M.-L. Kapsch, U. Mikolajewicz, F. A. Ziemen, F. A. Ziemen, C. B. Rodehacke, C. B. Rodehacke, C. Schannwell

    Published 2021-03-01
    Get full text
    Article
  18. 58
    Coupled ice sheet–climate modeling under glacial and pre-industrial boundary conditions

    Coupled ice sheet–climate modeling under glacial and pre-industrial boundary conditions by F. A. Ziemen, C. B. Rodehacke, U. Mikolajewicz

    Published 2014-10-01
    Get full text
    Article
  19. 59
    The upper-atmosphere extension of the ICON general circulation model (version: ua-icon-1.0)

    The upper-atmosphere extension of the ICON general circulation model (version: ua-icon-1.0) by S. Borchert, G. Zhou, G. Zhou, M. Baldauf, H. Schmidt, G. Zängl, D. Reinert

    Published 2019-08-01
    “…We use the ICOsahedral Non-hydrostatic (ICON) general circulation model, which is a joint development of the Max Planck Institute for Meteorology (MPI-M) and the German Weather Service (DWD), and provides, e.g., local mass conservation, a flexible grid nesting option, and a non-hydrostatic dynamical core formulated on an icosahedral–triangular grid. …”
    Get full text
    Article
  20. 60
    Arctic Clouds and Surface Radiation – a critical comparison of satellite retrievals and the ERA-Interim reanalysis

    Arctic Clouds and Surface Radiation – a critical comparison of satellite retrievals and the ERA-Interim reanalysis by M. Zygmuntowska, T. Mauritsen, J. Quaas, L. Kaleschke

    Published 2012-07-01
    Get full text
    Article

Search Tools: