在全球风暴解决模拟中,陆地与大气的合较弱.
Junhong Lee1, Cathy Hohenegger1
1Max Planck Institute for Meteorology, Hamburg 20146, Germany.
概括
全球气候模型显示,与粗分辨率模型不同的是,与显式对流相比,土壤湿度-降水反是负的. 这一发现影响了对陆地气候变化的理解,包括干旱和热浪.
科学领域:
- 气候科学 气候科学
- 大气科学 大气科学
- 水文学的水文学
背景情况:
- 土壤湿度-降雨反的标志是有争议的,粗度分辨率模型表明积极的反和区域模型表明负面的反.
- 粗分辨率模型很难明确表示对流,而区域模型通常规定大规模循环.
研究的目的:
- 为了研究土壤湿度-降水反,使用全球,结合模拟与明确的对流.
- 将这些结果与使用参数化对流的粗分辨率模拟进行比较.
主要方法:
- 全球,合模拟进行了一年,有明确的对流.
- 结果与使用参数化对流的粗分辨率模拟进行了比较.
主要成果:
- 使用明确对流的模拟显示了较弱且主要是负的土壤湿度-降水反.
- 显式对流模型倾向于在异质条件下在干燥的土壤上触发对流,与粗度分辨率模型不同.
- 土壤水分,蒸发和降水之间的反在明确的对流中较弱,与观测数据更好地对齐.
结论:
- 粗略分辨率的气候模型可能不足以研究干旱和热浪等陆地气候变化影响.
- 明确的对流表示对于准确模拟土壤湿度-沉反至关重要.
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