Dynamical downscaling of simulations of the Last Glacial Maximum (LGM) and late twentieth century (20C) were conducted using the Weather Research and Forecasting (WRF) model with the aim of (1) understanding how the downscaled kinematic and thermodynamic variables influence simulated tropical cyclone (TC) activity over the western North Pacific during the LGM and the 20C periods and (2) to test the relevance of TC genesis factors for the colder LGM climate. The results show that, despite the lower temperatures during the LGM, the downscaled TC climatology over the western North Pacific in the LGM simulation does not differ significantly from that in the 20C simulation. Among the TC environmental factors, the TC potential intensity, mid-tropospheric entropy deficit, and vertical wind shear during the LGM were consistent with previous analyses of TC genesis factors in LGM global climate model simulations. Changes in TC genesis density between the LGM and the 20C simulations seem to be well represented by the ventilation index, a nondimensional measure of the combined effects of vertical wind shear, and thermodynamic properties, suggesting the potential applicability of those factors for TC activity evaluation during the LGM and possibly other climates. � 2016. The Authors.
Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM, United States; Lamont-Doherty Earth Observatory, Columbia University, New York, NY, United States; Department of Atmospheric Sciences, Texas A&M University, College Station, TX, United States
Recommended Citation:
Yoo J,, Galewsky J,, Camargo S,et al. Dynamical downscaling of tropical cyclones from CCSM4 simulations of the Last Glacial Maximum[J]. Journal of Advances in Modeling Earth Systems,2016-01-01,8(3)