南京大学学报(自然科学版) ›› 2011, Vol. 47 ›› Issue (3): 318329.
胡伯彦 1 , 王淑瑜 1, 2 **
Hu Bo -Yan 1 , Wang Shu -Yu 1, 2
摘要: 本文利用 NCEP/ NCAR 再分析资料驱动 MM5V3 区域气候模式, 对东亚地区的气候进行了20 年(1982- 2001)的长期模拟, 分析了模式对中国地区地面温度和降水的模拟能力. 分析结果表明: 模
式对中国地区地面温度和降水的空间分布形态具有较好的模拟能力, 但在中国大部分地区对地面温度的模拟偏冷, 对降水的模拟偏多; 模式对地面温度年际变化的模拟好于对降水年际变化的模拟; 模式能
较好地模拟地面温度和降水的季节变化特征, 其中地面温度在夏半年的模拟结果优于冬半年的, 降水则相反; 模式对于一些极端气候要素, 如日最高、 最低地面温度, 强降水等也具有一定的模拟能力.
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