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过去2000年东亚夏季风降水百年际变化特征及成因的模拟研究

DOI: 10.11867/j.issn.1001-8166.2015.07.0780, PP. 780-790

Keywords: 过去2000年,气候模拟,东亚夏季风,外强迫因子,百年尺度

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Abstract:

利用地球系统模式CESM过去2000年气候模拟试验结果,探讨了在百年尺度上东亚夏季风降水的时空变化特征及其成因,对于认识百年尺度气候变化规律、区分外强迫因子对东亚季风的影响有着重要的科学意义。研究表明①东亚夏季风降水与温度基本同相变化,降水存在准100年、准150年和准200年周期。②降水标准化EOF第一模态为由北向南“负—正—负—正”的条带状空间分布,而EOF第二模态基本为全区一致的分布型态。③东亚夏季风降水准100年周期主要受太阳辐射、火山活动和气候系统内部变率的共同影响;准150年周期主要受太阳辐射的影响;准200年周期主要受太阳辐射和火山活动的影响。东亚夏季风降水在温带地区主要受温室气体和土地利用/覆盖的影响;在副热带地区主要受太阳辐射和火山活动的影响;在热带地区主要受太阳辐射、火山活动和气候系统内部变率的影响。

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