Characteristics of Model Tropical Cyclone Climatology and the Large-Scale Environment

Author:

Camargo Suzana J.1,Giulivi Claudia F.1,Sobel Adam H.2,Wing Allison A.3,Kim Daehyun4,Moon Yumin4,Strong Jeffrey D. O.1,Del Genio Anthony D.5,Kelley Maxwell5,Murakami Hiroyuki6,Reed Kevin A.7,Scoccimarro Enrico8,Vecchi Gabriel A.9,Wehner Michael F.10,Zarzycki Colin11,Zhao Ming6

Affiliation:

1. a Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York

2. b Department of Applied Physics and Applied Mathematics, Department of Earth and Environmental Sciences, Columbia University, New York, New York

3. c Department of Earth, Ocean and Atmospheric Science, Florida State University, Talahassee, Florida

4. d Department of Atmospheric Sciences, University of Washington, Seattle, Washington

5. e NASA Goddard Institute for Space Studies, New York, New York

6. f NOAA/Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey

7. g School of Marine and Atmospheric Sciences, Stony Brook University, Stony Brook, New York

8. h Fondazione Centro Euro-Mediterraneo sui Cambiamenti Climatici, Bologna, Italy

9. i Princeton University, Princeton, New Jersey

10. j Lawrence Berkeley National Laboratory, Berkeley, California

11. k The Pennsylvania State University, University Park, Pennsylvania

Abstract

AbstractHere we explore the relationship between the global climatological characteristics of tropical cyclones (TCs) in climate models and the modeled large-scale environment across a large number of models. We consider the climatology of TCs in 30 climate models with a wide range of horizontal resolutions. We examine if there is a systematic relationship between the climatological diagnostics for the TC activity [number of tropical cyclones (NTC) and accumulated cyclone energy (ACE)] by hemisphere in the models and the environmental fields usually associated with TC activity, when examined across a large number of models. For low-resolution models, there is no association between a conducive environment and TC activity, when integrated over space (tropical hemisphere) and time (all years of the simulation). As the model resolution increases, for a couple of variables, in particular vertical wind shear, there is a statistically significant relationship in between the models’ TC characteristics and the environmental characteristics, but in most cases the relationship is either nonexistent or the opposite of what is expected based on observations. It is important to stress that these results do not imply that there is no relationship between individual models’ environmental fields and their TC activity by basin with respect to intraseasonal or interannual variability or due to climate change. However, it is clear that when examined across many models, the models’ mean state does not have a consistent relationship with the models’ mean TC activity. Therefore, other processes associated with the model physics, dynamical core, and resolution determine the climatological TC activity in climate models.

Funder

National Oceanic and Atmospheric Administration

National Aeronautics and Space Administration

Horizon 2020 Framework Programme

Publisher

American Meteorological Society

Subject

Atmospheric Science

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