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首页> 外文期刊>Journal of hydrometeorology >An Increasing Trend in the Early Winter Precipitation during Recent Decades along the Coastal Areas of the Sea of Japan
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An Increasing Trend in the Early Winter Precipitation during Recent Decades along the Coastal Areas of the Sea of Japan

机译:近几十年沿着日本海洋沿海地区近几十年来较早趋势的趋势

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摘要

Long-term changes in the monthly precipitation along the coastal areas of the Sea of Japan are examined using monthly operational observation data from the Japan Meteorological Agency. The monthly precipitation in December significantly increased from the mid-1980s to 2015, even though no remarkable changes were found in January, February, or November. Significant positive trends in the December precipitation extend widely over the coastal areas of the Sea of Japan, and the amounts increase to approximately 50% of the climatological precipitation in December at most observational stations. The interannual variations in other variables, including the monthly accumulated actual sunshine duration, days with lightning detection, and satellite-retrieved outgoing longwave radiation, also show significant trends that are consistent with the precipitation increase in December. The effect of the sea surface temperature (SST) on precipitation change is discussed based on correlation and regression analyses. The interannual variations in the December precipitation averaged over the observational stations near the Sea of Japan are significantly correlated with the SSTs in the prior month (November). However, the SST increase in November is insufficient to account for the increase in precipitation. In addition, it was found that the satellite-retrieved surface wind speed in December has grown stronger in recent years over the Sea of Japan. It is suggested that the stronger wind corresponds to the enhanced monsoonal flow and is the primary cause of the precipitation increase in December.
机译:使用日本气象学局的每月运行观测数据检查日本海洋沿海地区的月度降水的长期变化。 12月份的月度降水量从20世纪80年代中期到2015年的月度显着增加,尽管在1月,2月或11月没有发现了显着变化。 12月降水量的显着积极趋势在日本海洋沿海地区广泛扩大,在大多数观察站的12月份的大约50%的占气球降水量的大约50%。其他变量的续集变化,包括每月累计的实际阳光持续时间,避雷检测的天数,以及卫星检索的龙波辐射,也显示出与12月份降水量增加一致的显着趋势。基于相关性和回归分析,讨论了海表面温度(SST)对沉淀变化的影响。 12月降水量的持续变化在日本海洋附近的观测站平均与现有月(11月)的SST相关。然而,11月的SST增加不足以解释降水量的增加。此外,有人发现,在日本海洋近年来,12月份的卫星检索的表面风速越来越强。建议,较强的风对应于增强的季风流动,是12月降水量增加的主要原因。

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