【摘 要】
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The basic climatic characteristics about the Tibetan Plateau surface heating field intensity (TPSHFI) and its anomalous change trend are analyzed by using Lhasa
【出 处】
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Science in China(Series D:Earth Sciences)
论文部分内容阅读
The basic climatic characteristics about the Tibetan Plateau surface heating field intensity (TPSHFI) and its anomalous change trend are analyzed by using Lhasa, Yushu and Wu-daoliang as the representatves of north-part, east-part and mid-north part of the Tibetan Plateau, respectively. The impact of heating intensity anomalism on NH general circulation and the climate of China is diagnosed.
The basic climatic characteristics about the Tibetan Plateau surface heating field intensity (TPSHFI) and its anomalous change trend are analyzed by using Lhasa, Yushu and Wu-daoliang as the representatves of north-part, east-part and mid-north part of the Tibetan Plateau, respectively. The impact of heating intensity anomalism on NH general circulation and the climate of China is diagnosed.
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