青藏高原东北部两次区域性大到暴雨对比分析 |
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引用本文: | 田成娟,朱平,马琼,等. 青藏高原东北部两次区域性大到暴雨对比分析[J]. 高原山地气象研究, 2017, 37(1): 1-6. DOI: 10.3969/j.issn.1674-2184·2017.01.001 |
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作者姓名: | 田成娟 朱平 马琼 等 |
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作者单位: | 青海省气象台, 西宁 810001 |
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基金项目: | 青海省气象局重点项目"多源数据融合的青海省强对流天气综合监测预警预报业务系统"青海省气象局预报员专项"2015年青海东部两次区域性大到暴雨个例对比分析 |
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摘 要: | 利用常规气象观测、自动站资料和NCEP/NCAR1°×1°再分析资料,对2015年6月19~20日(简称“6.19”)和8月1~3日(简称“8.1”)发生在青海省东部的两次区域性大到暴雨天气从环流背景、各物理量场特征进行对比分析,结果表明:两次过程都是地面有冷空气从河西走廊扩散南下,地面伴有辐合线;散度场上高层辐散,低层辐合的配置,整层大气都具有强烈的上升运动;水汽条件特征表现为高层干冷,中低层暖湿,700h Pa上比湿均在8g/kg以上;强降水产生的区域均为Ki>32℃的区域。
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关 键 词: | 青藏高原 大到暴雨 特征 对比分析 |
收稿时间: | 2017-01-12 |
Contrastive Analysis on Two Regional Heavy-Hard Rainfalls in the Northeast of Qinghai-Tibetan Plateau |
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Affiliation: | (Qinghai Meteorological Observatory, Xining 810001, China |
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Abstract: | By contrasting and analyzing two regional heavy-hard rainfalls in the east of Qinghai province on June 19 to 20 (“6. 9”for short) and August 1 to 3 (“8. 1”for short), 2015 using conventional meteorological observation, automatic station data and NCEP/NCAR1°×1° reanalysis data. The results show that: there are cold air from the hexi corridor southward on the ground with convergence line of two processes, it is high-level divergence, low-level convergence on the divergence field, there is a strong upward movement of the whole layer of the atmosphere. Water vapor characteristic shows that dry and cold on highlevel, and warm and wet on low-level, specific humidity are both more than 8g/kg on 700 h Pa, heavy rain all occurred area where is Ki>32℃. |
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