Summertime Temperature Extremes over Japan in the Late 21st Century Projected by a High-Resolution Regional Climate Model
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- MURATA Akihiko
- Meteorological Research Institute
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- NAKANO Masuo
- Japan Agency for Marine-Earth Science and Technology
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- KANADA Sachie
- Japan Agency for Marine-Earth Science and Technology
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- KURIHARA Kazuo
- Meteorological Research Institute
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- SASAKI Hidetaka
- Meteorological Research Institute
書誌事項
- 公開日
- 2012
- DOI
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- 10.2151/jmsj.2012-a05
- 公開者
- 公益社団法人 日本気象学会
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説明
Future changes in summertime temperature extremes over Japan are projected by a well-developed regional climate model (RCM) with a spatial resolution of 5 km. The performance of the RCM with respect to temperature in the present climate is evaluated first based on observations. Although the differences in the biases (from observations) of daily temperatures between the RCM and the driving atmospheric general circulation model (AGCM) simulations are not statistically significant, root-mean-square errors (from observations) in daily mean and minimum temperatures reproduced by the RCM are smaller than those by the AGCM with a coarser spatial resolution. These results indicate that RCM with a higher spatial resolution has better performance than the driving AGCM in simulating temperature variability. A test of whether the RCM can capture temperature extremes reveals a good quantitative agreement between simulated and observed values in appearance frequency of extreme high temperature for the daily minimum temperature during July and August. The spatial pattern of the upper tail of the frequency distribution for the daily maximum temperature is also in good agreement with observations, although the model values are underestimated.<br>Projected changes for extremely high daily minimum temperature are relatively large in July on the lee side of the Hidaka Mountains, southeast of Hokkaido. This finding can be explained by the foehn phenomenon: changes in the windward Froude number indicate that atmospheric conditions in the future climate are more favorable for the intensification of foehn. In terms of extremely high daily maximum temperature, the difference between the present-day and future climates during August is relatively large over the Tama area, west of Tokyo. Although the foehn phenomenon is not solely responsible for the projected changes, the phenomenon can explain the projected changes when westerly winds prevail over the Tama area, located on the lee side of the Kanto Mountains.
収録刊行物
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- 気象集誌. 第2輯
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気象集誌. 第2輯 90A (0), 101-122, 2012
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
- 1390282681479948288
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- NII論文ID
- 130004435183
- 40019200938
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- NII書誌ID
- AA00702524
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- ISSN
- 21869057
- 00261165
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- NDL書誌ID
- 023526844
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- 本文言語コード
- en
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- データソース種別
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- JaLC
- NDLサーチ
- Crossref
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- OpenAIRE
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- 抄録ライセンスフラグ
- 使用不可

