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Volume 9, issue 2 | Copyright
Geosci. Model Dev., 9, 779-788, 2016
https://doi.org/10.5194/gmd-9-779-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Development and technical paper 25 Feb 2016

Development and technical paper | 25 Feb 2016

Impact of surface coupling grids on tropical cyclone extremes in high-resolution atmospheric simulations

Colin M. Zarzycki1, Kevin A. Reed2, Julio T. Bacmeister1, Anthony P. Craig1, Susan C. Bates1, and Nan A. Rosenbloom1 Colin M. Zarzycki et al.
  • 1National Center for Atmospheric Research, Boulder, Colorado, USA
  • 2School of Marine and Atmospheric Sciences, State University of New York at Stony Brook, Stony Brook, New York, USA

Abstract. This paper discusses the sensitivity of tropical cyclone climatology to surface coupling strategy in high-resolution configurations of the Community Earth System Model. Using two supported model setups, we demonstrate that the choice of grid on which the lowest model level wind stress and surface fluxes are computed may lead to differences in cyclone strength in multi-decadal climate simulations, particularly for the most intense cyclones. Using a deterministic framework, we show that when these surface quantities are calculated on an ocean grid that is coarser than the atmosphere, the computed frictional stress is misaligned with wind vectors in individual atmospheric grid cells. This reduces the effective surface drag, and results in more intense cyclones when compared to a model configuration where the ocean and atmosphere are of equivalent resolution. Our results demonstrate that the choice of computation grid for atmosphere–ocean interactions is non-negligible when considering climate extremes at high horizontal resolution, especially when model components are on highly disparate grids.

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This paper highlights the sensitivity of simulated tropical cyclone climatology to the choice of ocean coupling grid in high-resolution climate simulations. When computations of atmosphere–ocean interactions are carried out on the coarser grid in the system, key quantities such as surface wind drag and heat fluxes are incorrectly calculated. In the case of a coarser ocean grid, significantly stronger cyclone winds result, due to misaligned frictional vectors in the atmospheric dynamical core.
This paper highlights the sensitivity of simulated tropical cyclone climatology to the choice of...
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