由GPM-DPRR检测到的中国北部夏季降水的垂直结构和微物理特征
Donghuan Li1, Youcun Qi1, Huiqi Li2
1Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, China; University of Chinese Academy of Sciences, Beijing, China.
The Science of the total environment
|May 11, 2024
概括
中国北部的对流降水 (CP) 和分层降水 (SP) 显示出明显的山平区差异. 平原由于强烈的CP而收到更多的降水量,而山区则有较高的频率从轻的SP.
科学领域:
- 大气科学 大气科学
- 气象学 天气学
- 水文学的水文学
背景情况:
- 层状降水 (SP) 和对流降水 (CP) 呈现出不同的垂直结构和微物理特征.
- 地形影响,如山脉和平原,可以显著改变降水模式.
研究的目的:
- 分析中国北部SP和CP的垂直结构和微物理特征.
- 调查山区和平原地区降水特征的差异.
- 了解当地地形对降水估计和预测的影响.
主要方法:
- 使用了全球降雨测量 (GPM) 任务的双频降雨雷达 (DPR) 产品.
- 分析了2014年至2021年北极夏季期间的数据.
- 在山区和平原地区比较降水特征.
主要成果:
- 降水量在平原较高,而在山区的频率更高,受气候和地形的影响.
- CP对总降水频率的贡献约为四分之一;SP和CP在平原上都比平原大20%更强烈.
- 平原表现出更深的降水系统,风暴最高高度 (STA) 和结水平更高,导致更强烈的CP和显著的低水平水流星增长.
结论:
- 地形显著影响降水特征,平原偏好强烈的CP,山脉偏好频繁的光SP.
- 较深的风暴系统和平原中低层微物理过程的增强有助于降水量增加.
- 这些发现对于改善山区的定量降水估计和预测至关重要.
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