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东北冷涡暖季气候特征及其降水在黑龙江省的时空分布

Climatic characteristics of Northeast Cold Vortex and its precipitation during the warm season in Heilongjiang Province

  • 摘要: 本文使用黑龙江省80个国家站小时降水量资料及NCEP/ NCAR再分析资料,分析了1981—2022年暖季(5—9月)东北冷涡及其降水的气候特征,研究了冷涡降水在黑龙江省复杂地形下的时空分布特征。研究结果发现,(1)黑龙江省暖季年平均降水量、冷涡过程降水量及占比均呈现显著的年际、年代际变化特征。暖季年平均降水量在1998年以前为缓慢减弱趋势,之后为明显增强趋势;冷涡过程年平均降水量整体呈现增强趋势。(2)降水量和降水频次的峰值均位于14—17时。降水量较降水频次的日变化幅度更大。降水强度越大,其日变化和年际变化特征越显著。(3)强降水发生频次和贡献率均是白天大于夜间。降水强度越大对总降水的影响程度越大。东北冷涡过程中强降水的贡献在增加,降水强度越大增加趋势越显著;弱降水的贡献在减少。(4)极值空间分布特征与局地地形密切相关,平原向山区的过渡区域降水极值最大,极易发生强降水,山区和平原降水极值相对较小。

     

    Abstract: Based on the hourly precipitation data of 80 national stations in Heilongjiang Province and NCEP/ NCAR reanalysis data, the climatic characteristics of the Northeast cold vortex (NECV) and its precipitation during the warm season (May-September) from 1981 to 2022 were analyzed, and the spatio-temporal distribution characteristics of NECV precipitation in the complex terrain of Heilongjiang Province were studied. The results showed that (1)In Heilongjiang province, the average annual precipitation during the warm season, the precipitation of NECV processes and their proportion in the warm season showed significant interannual and interdecadal variation characteristics. Before 1998, the average annual precipitation in the warm season showed a slow weakening trend, and then an obvious increasing trend. The average annual precipitation of cold vortex processes showed an overall increasing trend. (2)The peak values of precipitation and precipitation frequency were from 14:00 to 17:00. The diurnal variation of precipitation was larger than that of precipitation frequency. The precipitation with greater intensity had more significant diurnal and interannual variation characteristics. (3)The frequency and contribution rate of heavy precipitation were greater in the daytime than at night. The greater the precipitation intensity, the greater the influence on the total precipitation. The contribution of heavy precipitation in the process of NECV was increasing, and the greater the precipitation intensity, the more significant the increasing trend. The contribution of weak precipitation was declining. (4)The spatial distribution of extreme values was closely related to the local topography. The transition area from plain to mountainous area had the largest precipitation extreme value, which was easy to have heavy precipitation, while the precipitation extreme value in mountainous area and plain area was relatively small.

     

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