Impact of the dynamical core on the direct simulation of tropical cyclones in a high-resolution global model

被引:63
|
作者
Reed, K. A. [1 ,2 ]
Bacmeister, J. T. [2 ]
Rosenbloom, N. A. [2 ]
Wehner, M. F. [3 ]
Bates, S. C. [2 ]
Lauritzen, P. H. [2 ]
Truesdale, J. E. [2 ]
Hannay, C. [2 ]
机构
[1] SUNY Stony Brook, Sch Marine & Atmospher Sci, Stony Brook, NY 11794 USA
[2] Natl Ctr Atmospher Res, Climate & Global Dynam Lab, Boulder, CO 80307 USA
[3] Univ Calif Berkeley, Lawrence Berkeley Natl Lab, Berkeley, CA 94720 USA
基金
美国国家科学基金会;
关键词
dynamical core; global model; tropical cyclone; COMMUNITY ATMOSPHERE MODEL; GENERAL-CIRCULATION MODEL; CLIMATE SIMULATIONS; INTERCOMPARISON PROJECT; SENSITIVITY; PARAMETERIZATION; CONVECTION; SCHEMES; AMIP; GCM;
D O I
10.1002/2015GL063974
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
This paper examines the impact of the dynamical core on the simulation of tropical cyclone (TC) frequency, distribution, and intensity. The dynamical core, the central fluid flow component of any general circulation model (GCM), is often overlooked in the analysis of a model's ability to simulate TCs compared to the impact of more commonly documented components (e.g., physical parameterizations). The Community Atmosphere Model version 5 is configured with multiple dynamics packages. This analysis demonstrates that the dynamical core has a significant impact on storm intensity and frequency, even in the presence of similar large-scale environments. In particular, the spectral element core produces stronger TCs and more hurricanes than the finite-volume core using very similar parameterization packages despite the latter having a slightly more favorable TC environment. The results suggest that more detailed investigations into the impact of the GCM dynamical core on TC climatology are needed to fully understand these uncertainties.
引用
收藏
页码:3603 / 3608
页数:6
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