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Projection of Climatic Change over Japan Due to Global Warming by High-Resolution Regional Climate Model in MRI

机译:MRI高分辨率区域气候模型对全球变暖引起的日本气候变化的预测

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References(14) Cited-By(36) Supplementary materials(1) The Meteorological Research Institute (MRI) and the Japan Meteorological Agency (JMA) projected climate change over Japan due to global warming using a high-resolution Regional Climate Model of 20 km mesh size (RCM20) developed in MRI. Projection was made for 2081 to 2100 following a SRES-A2 scenario. Precipitation projected by RCM20 indicated that increased daily precipitation will be seen during the warm season from June to September. Except for this period, the precipitation amount will not change much or will slightly decrease around Japan. The increase during the warm season will be seen only in the western part of Japan. A possible cause of the increase is an El Niño-like SST pattern in the future. Due to the future increased summer SST in the eastern equatorial Pacific, anti-cyclonic circulation to the south of Japan will intensify and will induce a strong water vapor flux along the rim of the anti-cyclonic anomaly. The intensified flux will converge over the western part of Japan and may increase precipitation. Surface air temperature is projected to increase more than 2°C around Japan in January. In summer, the temperature increase will be lower by about 1°C than in winter.
机译:参考文献(14)被引用的文献(36)补充材料(1)气象研究所(MRI)和日本气象厅(JMA)使用20 km的高分辨率区域气候模型预测了全球变暖引起的日本各地的气候变化。 MRI中开发了网格尺寸(RCM20)。根据SRES-A2情景,预测了2081年至2100年。 RCM20预测的降水表明,在六月至九月的暖季期间,每天的降水将增加。除此期间外,日本各地的降水量变化不大或略有减少。暖季期间的增加仅在日本西部可见。增长的可能原因是将来出现类似厄尔尼诺现象的SST模式。由于未来赤道东太平洋夏季SST的增加,日本南部的反气旋环流将会加剧,并会在反气旋异常的边缘引起强烈的水汽通量。加剧的通量将汇聚到日本西部,并可能增加降水。预计1月份日本各地的地面气温会升高2°C以上。在夏季,温度升高将比冬季低约1°C。

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