The development of Tropical Cyclone Diana (1984) is simulated with a mesoscale model using 1.2 km grid spacing over a regional-scale (> 1000 km) domain in the first develops a mesoscale convection system along a remnant frontal zone, which yields a mesoscale vortex. After a period of quiescence, banded convection organizes about the vortex from isolated, grid-resolved cells, with the system becoming warm-core and intensifying into Tropical Storm Diana. (C) Royal Meteorological Society
机构:
Nagoya Univ, Hydrospher Atmospher Res Ctr, Nagoya, Aichi 4648601, Japan
Frontier Res Ctr Global Change, Yokohama, Kanagawa, JapanNagoya Univ, Hydrospher Atmospher Res Ctr, Nagoya, Aichi 4648601, Japan
机构:
Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USAUniv Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA
Suhas, E.
Zhang, Guang J.
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机构:
Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA
Tsinghua Univ, Ctr Earth Syst Sci, Beijing 100084, Peoples R ChinaUniv Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA