Comparison of Spatial Pattern and Mechanism between Convexity and Gap Winds

Author:

Nishi Akifumi1,Kusaka Hiroyuki2

Affiliation:

1. Graduate School of Life and Environmental Sciences, University of Tsukuba

2. Center for Computational Sciences, University of Tsukuba

Publisher

Meteorological Society of Japan

Subject

Atmospheric Science

Reference24 articles.

1. Arakawa, S., 1969: Climatological and dynamical studies on the local strong winds, mainly in Hokkaido. Japan. Geophys. Mag., 34, 349-425.

2. Clark, T. L., and W. R. Peltier, 1984: Critical level reflection and the resonant growth of nonlinear mountain waves. J. Atmos. Sci., 41, 3122-3134.

3. Elvidge, A. D., and I. A. Renfrew, 2016: The causes of foehn warming in the lee of mountains. Bull. Amer. Meteor. Soc., 97, 455-466, doi:10.1175/BAMS-D-14-00194.1.

4. Gaberšek, S., and D. Durran, 2004: Gap flows through idealized topography. Part I: Forcing by large-scale winds in the nonrotating limit. J. Atmos. Sci., 61, 2846-2862, doi:10.1175/ JAS-3340.1.

5. Gohm, A., G. J. Mayr, A. Fix, and A. Giez, 2008: On the onset of bora and the formation of rotors and jumps near a mountain gap. Quart. J. Roy. Meteor. Soc., 134, 21-46, doi:10.1002/qj.206.

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