T
Tadahiro Hayasaka
Researcher at Tohoku University
Publications - 98
Citations - 3612
Tadahiro Hayasaka is an academic researcher from Tohoku University. The author has contributed to research in topics: Aerosol & Shortwave. The author has an hindex of 21, co-authored 94 publications receiving 3247 citations. Previous affiliations of Tadahiro Hayasaka include University of Tokyo.
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An Asian emission inventory of anthropogenic emission sources for the period 1980-2020
Toshimasa Ohara,Toshimasa Ohara,Hajime Akimoto,Jun Ichi Kurokawa,Nobuhiro Horii,Kazuyo Yamaji,Xiaoyuan Yan,Tadahiro Hayasaka +7 more
TL;DR: In this article, the authors developed a new emission inventory for Asia (Regional Emission inventory in ASia (REAS) Version 1.1) for the period 1980-2020.
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A Gauge-Based Analysis of Daily Precipitation over East Asia
Pingping Xie,Akiyo Yatagai,Mingyue Chen,Tadahiro Hayasaka,Yoshihiro Fukushima,Changming Liu,Song Yang +6 more
TL;DR: In this paper, a new gauge-based analysis of daily precipitation was constructed on a 0.5° latitude-longitude grid over East Asia (5°-60°N, 65°-155°E) for a 26-yr period from 1978 to 2003 using gauge observations at over 2200 stations collected from several individual sources.
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Aerosol trends over China, 1980-2000
TL;DR: In this article, the authors presented annual emission trends of sulfur dioxide, black carbon, and organic carbon for East Asia for the period 1980-2000, using regional results from the GOCART global chemical transport model.
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Tropospheric aerosol optical properties derived from lidar, sun photometer, and optical particle counter measurements
TL;DR: Comparison of Optical thicknesses derived from both instruments clearly shows the effect of Mt. Pinatubo's eruption and the temporal variation of optical thickness in the stratosphere over 12 km.
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Effects of Cloud Horizontal Inhomogeneity on the Optical Thickness Retrieved from Moderate-Resolution Satellite Data
TL;DR: In this article, a Monte Carlo 3D radiative transfer model and a lognormal spectral cloud model are used to simulate monochromatic radiance reflected from overcast boundary layer cloud.