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东北亚地区冷涡活动特征及其影响期间我国东北暖季降水分布

Characteristics of Cold Vortexes in Northeast Asia and Their Impacts on Precipitation Distribution of Warm Seasons over Northeast China

  • 摘要: 本文客观识别和追踪了2000~2019年东北亚地区持续时间为6 h, 24 h)和24 h, 48 h)以及≥48 h(传统东北冷涡)的3730次冷涡过程,分析了不同持续时间冷涡时空分布、强度和尺度特征的差异及其影响期间我国东北暖季降水分布。结果表明:(1)持续时间为6 h, 24 h)的冷涡发生频次最多(占比约60%),传统东北冷涡频次最少(占比约15%)。(2)冷涡存在明显的年际和月际变化,其更易出现在暖季5~8月,但不同持续时间冷涡频数峰值月份不同。(3)持续时间为6 h, 24 h)、24 h, 48 h)和≥48 h的冷涡中心活动主要高频区分别出现在识别区域东北角、东北象限和中部;冷涡中心初现时刻位置主要位于45°~55°N的识别区域西边界附近,另外,持续时间为6 h, 24 h)和24 h, 48 h)的冷涡中心初现时刻位置在识别区域东北象限(中北部)亦存在高频区;冷涡中心在分析区域内的最后出现时刻较多位于40°N以北的分析区域东边界附近。(4)冷涡持续时间越长,强度越强、半径越大;冷季冷涡强度和半径大于暖季。(5)东北暖季,冷涡背景下总降水量和短时强降水量占比均值均超过60%,后者更大,冷涡持续时间越长,上述占比相对越大;不同持续时间冷涡影响期间,总降水量/短时强降水量占比空间分布存在明显差异。

     

    Abstract: This study identifies and tracks 3730 CVs (cold vortexes) in Northeast Asia from 2000 to 2019, including “short duration” CVs lasting 6 h, 24 h) and 24 h, 48 h), as well as traditional northeast CVs lasting at least 48 h. It examines differences in the spatial and temporal distribution, intensity, and scale of CVs with different durations, along with their impact on precipitation in Northeast China during warm seasons. The results show the following: (1) CVs lasting 6 h, 24 h) are the most common, accounting for about 60%, while traditional CVs are the least common, at about 15%. (2) CVs demonstrate considerable interannual and intermonthly variations, with most occurring from May to August. However, CVs with different durations peak in different months. (3) The high occurrences of CV centers with durations of 6 h, 24 h), 24 h, 48 h), and ≥48 h appear in the northeast corner, northeast quadrant, and central part of the study region, respectively. Initial CV centers mainly occur near the western boundary between 45° and 55°N. CVs lasting 6 h, 24 h) and 24 h, 48 h) frequently emerge in the northeast quadrant and north-central part, respectively. They are typically found near the eastern boundary of the region north of 40°N. (4) CVs with longer durations exhibit stronger centers and larger sizes. They are also stronger and larger during cold seasons compared to warm seasons. (5) Under CV conditions, the average contribution of both total precipitation and short-duration heavy precipitation exceeds 60%, with the latter being significantly larger. Longer-lasting CVs correspond to higher precipitation ratios. The spatial distributions of total precipitation and short-time heavy precipitation under different CV durations present remarkable differences.

     

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