台湾夏季降雨的微物理属性的区域差异,使用GPM DPR
Jayalakshmi Janapati1, Balaji Kumar Seela1, Pay-Liam Lin2,3,4
1Institute of Atmospheric Physics, Department of Atmospheric Sciences, National Central University, Zhongli District, Taoyuan City, 320317, Taiwan.
Scientific reports
|July 26, 2023
概括
台湾夏季降雨量在雨滴大小和度上呈现出明显的区域差异. 台湾中部和南部由于降雨量较高而经历了更大的下降,影响了云模型.
科学领域:
- 大气科学 大气科学
- 气象学 天气学
- 水文学 水文学
背景情况:
- 台湾复杂的地形与温暖季节的降雨相互作用,导致地区差异很大.
- 了解降雨微物理对于在山区准确的天气和气候建模至关重要.
研究的目的:
- 调查台湾各地夏季降雨微物理特征的区域差异.
- 分析雨滴大小分布及其与降水类型和地形的关系.
- 确定影响台湾夏季季风雨的主要微物理过程.
主要方法:
- 利用了9年的 (2014-2022) 全球降雨量测量 (GPM) 双频降雨雷达 (DPR) 数据.
- 通过高度图 (CFADs) 来分析轮频率,以检测雷达反射率,降雨率,下降直径和度.
- 在四个不同的地理区域比较了微物理特性:北,南,东和台湾中部.
主要成果:
- 在降雨量和雨滴大小分布方面观察到显著的区域差异.
- 在融化层上方占主导地位的大型超冷液体和冰颗粒,下方是雨颗粒,在台湾南部和中部被注意到.
- 台湾中部出现大降雨 (对流降雨),台湾北部降雨量较小;南部和中部地区降雨量较大.
结论:
- 台湾的夏季季风降雨主要由凝聚和分离过程控制.
- 降雨微物理的区域差异,特别是滴量大小,与地理位置和降水类型有关.
- 这些发现可以改善对台湾等复杂地形的云建模模拟.
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