Projection of Future Climate Change over Japan in Ensemble Simulations with a High-Resolution Regional Climate Model
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- Murata Akihiko
- Meteorological Research Institute
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- Sasaki Hidetaka
- Meteorological Research Institute
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- Kato Teruyuki
- Meteorological Research Institute
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- Shido Fumitake
- Meteorological Research Institute
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- Kanada Sachie
- Nagoya University
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- Suzuki-Parker Asuka
- University of Tsukuba
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- Nagatomo Toshiharu
- University of Tsukuba
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- Hibino Kenshi
- University of Tsukuba
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- Aoyagi Toshinori
- Meteorological Research Institute
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- Nosaka Masaya
- Meteorological Research Institute
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- Kawase Hiroaki
- Meteorological Research Institute
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- Oh'izumi Mitsuo
- Meteorological College
書誌事項
- 公開日
- 2015
- 資源種別
- journal article
- DOI
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- 10.2151/sola.2015-022
- 公開者
- 公益社団法人 日本気象学会
説明
Future changes in surface air temperature and precipitation over Japan by the end of the 21st century are projected by a well-developed non-hydrostatic regional climate model with a grid spacing of 5 km under the RCP8.5 scenario. Uncertainties in the projected temperature and precipitation are also evaluated with the results obtained from ensemble simulations using this high-resolution model. The projected future climate indicates robust increases in the annual-mean surface air temperature for all regions in Japan. In contrast, many regions do not exhibit statistically significant changes in annual precipitation. In some regions and months, however, monthly precipitation in a couple of members of the ensemble simulations has a statistically significant decrease or increase. Monthly precipitation over the eastern Japan Sea side (EJ) region in December has relatively robust decreases. These decreases are attributed to decreases or weakening of convection over the Japan Sea polar air-mass convergence zone, which is accounted for by the weakening of large-scale low-level northwesterly winds associated with the winter monsoon. The relationship between precipitation and convergence in the EJ region is consistent with the results above: Convective clouds are shallower in the future climate compared with those in the present climate.
収録刊行物
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- SOLA
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SOLA 11 (0), 90-94, 2015
公益社団法人 日本気象学会
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詳細情報 詳細情報について
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- CRID
- 1390001205222297600
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- NII論文ID
- 130005078532
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- ISSN
- 13496476
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- 本文言語コード
- en
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- 資料種別
- journal article
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- データソース種別
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- JaLC
- Crossref
- CiNii Articles
- KAKEN
- OpenAIRE
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- 抄録ライセンスフラグ
- 使用不可
