Comparison of Snow Cover Observations along the Tateyama-Kurobe Alpine Route with Snow Cover Simulations Using the Non-hydrostatic Regional Climate Model (NHRCM) with Different Horizontal Resolutions

Author:

KAWASE Hiroaki1,IIDA Hajime2,AOKI Kazuma3,SHIMADA Wataru3,NOSAKA Masaya1,MURATA Akihiko1,SASAKI Hidetaka1

Affiliation:

1. Meteorological Research Institute, Japan Meteorological Agency

2. Tateyama Caldera Sabo Museum

3. Graduate School of Science and Engineering, University of Toyama

Publisher

Tokyo Geographical Society

Subject

Earth-Surface Processes,Geology,Geophysics,Geography, Planning and Development,Global and Planetary Change

Reference32 articles.

1. Aoki, K., and K. Watanabe (2009): Measurements of atmospheric aerosol at Mt. Tateyama, Japan. Earozoru Kenkyu, 24, 112-116.

2. Aoki, T., Hachikubo, A. and Hori, M. (2003): Effects of snow physical parameters on shortwave broadband albedos. Journal of Geophysical Research, 108(D19), 4616.

3. Fukui, K. and Iida, H. (2012): Identifying active glaciers in Mt. Tateyama and Mt. Tsurugi in the northern Japanese Alps, central Japan. Seppyo, 74, 213-222.

4. Fukui, K., Iida, H. and Kosaka T. (2018): Newly identifying active glaciers in the Northern Japanese Alps and their characteristics. Geographical Review of Japan Series A, 191, 43-61.

5. Hara, M., Yoshikane, T., Kawase, H. and Kimura, F. (2008): Estimation of the impact of global warming on snow depth in Japan by the pseudo-global-warming method. Hydrological Research Letters, 2, 61-64.

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