Climate Dynamics

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101: Atmospheric General Circulation Dynamics (HW 4, due May 2): Consider a rotating shallow-water layer with a free surface over a flat bottom boundary. 1. Inertia-gravity waves. Assume uniform rotation with a c

: Atmospheric General Circulation Dynamics (HW 4, due May 2): Consider a rotating shallow-water layer with a free surface over a flat bottom boundary. 1. Inertia-gravity waves. Assume uniform rotation with a c

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Source URL: climate-dynamics.org

- Date: 2016-04-18 10:24:03
    102Geophysical Research Letters RESEARCH LETTER2016GL068418 Key Points: • The wet gets wetter, dry gets drier, idea does not apply regionally, because

    Geophysical Research Letters RESEARCH LETTER2016GL068418 Key Points: • The wet gets wetter, dry gets drier, idea does not apply regionally, because

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    Source URL: climate-dynamics.org

    Language: English - Date: 2016-05-16 06:27:20
    103mean_extreme_precip_999_ai

    mean_extreme_precip_999_ai

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    Source URL: climate-dynamics.org

    Language: English
    1041 MAYWALKER ET AL. 3731

    1 MAYWALKER ET AL. 3731

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    Source URL: climate-dynamics.org

    Language: English - Date: 2015-09-11 20:43:18
    1051 MAYCORRIGENDUM Corrigendum TAPIO SCHNEIDER AND TOBIAS BISCHOFF

    1 MAYCORRIGENDUM Corrigendum TAPIO SCHNEIDER AND TOBIAS BISCHOFF

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    Source URL: climate-dynamics.org

    Language: English - Date: 2016-04-26 10:59:41
      106JANUARYLIU AND SCHNEIDER 389

      JANUARYLIU AND SCHNEIDER 389

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      Source URL: climate-dynamics.org

      Language: English - Date: 2015-09-11 20:41:52
      1071  Energetic constraints on the width of the intertropical convergence zone 2

      1 Energetic constraints on the width of the intertropical convergence zone 2

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      Source URL: climate-dynamics.org

      Language: English - Date: 2016-06-16 12:31:24
      108754  JOURNAL OF CLIMATE VOLUME 26

      754 JOURNAL OF CLIMATE VOLUME 26

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      Source URL: climate-dynamics.org

      Language: English - Date: 2015-09-11 20:41:34
      109Boundary layer cloud processes and Global Climate Model (GCM) parameterizations Florent Brient  The Coupled Model Intercomparison Project Phase 5 (CMIP5)

      Boundary layer cloud processes and Global Climate Model (GCM) parameterizations Florent Brient The Coupled Model Intercomparison Project Phase 5 (CMIP5)

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      Source URL: climate-dynamics.org

      Language: English - Date: 2016-05-12 04:00:31
      110Closure of the meridional overturning circulation through Southern Ocean upwelling

      Closure of the meridional overturning circulation through Southern Ocean upwelling

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      Source URL: climate-dynamics.org

      Language: English - Date: 2016-04-17 06:43:22