Affiliations: Earth Observation Research Center, NASDA, Roppongi
1-9-9, Minato-ku, Tokyo 106-0032, Japan | Center for Atmospheric and Oceanic Studies, Faculty of
Science, Tohoku University, Sendai 980-8578, Japan | Institute of Geoscience, University of Tsukuba,
Tsukuba 305-0006, Japan
Abstract: In the winter, the wind system over the Sea of Japan strongly
affects the weather of the Japan islands. In this paper, wind distributions
over the Sea of Japan during cold-air outbreaks observed by the NASA
scatterometer were analyzed. Strong northwesterly to westerly winds of 15 to 20
m/s were observed off Vladivostok and off the Korea Peninsula, respectively. A
weak wind region, in which the wind speed is less than 9 m/s, is seen downwind
of the mountains and extends more than 200 km. A strong wind convergence zone
was formed in the further lee of the weak wind region. Numerical experiments
using a three-dimensional mesoscale model are performed to compare the wind
distribution observed by NSCAT. The results show that the simulated winds agree
well with those observed by NSCAT except for the intensity of the
convergence.
Keywords: NASA scatterometer, ocean wind, numerical experiment