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[3] Yu WS,Yao TD,Tian LD,et al. Relationships Between Delta O-18 In Precipitation And Air Temperature And Moisture Origin On A South-north Transect Of The Tibetan Plateau[J]. Atmospheric Research,2008,87(2):158-169.
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[5] 马耀明. 青藏高原多圈层相互作用观测工程及其应用[J]. 中国工程科学,2012(9).
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[6] 马耀明,王永杰,马伟强,等. 珠峰复杂地表区域能量通量的卫星遥感[J]. 高原气象,2007(6).
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[7] 马耀明,马伟强,胡晓,等. 卫星遥感确定沙特阿拉伯吉达地区非均匀地表区域地表参数和能量通量[J]. 干旱气象,2004(4).
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[8] 仲雷,马耀明,马伟强,等. 西藏中部“一江两河”地区地表通量的卫星遥感估算[J]. 冰川冻土,2011(2).
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[9] 马耀明,姚檀栋,王介民. 青藏高原能量和水循环试验研究——game/tibet与camp/tibet研究进展[J]. 高原气象,2006(2).
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[10] 马耀明,姚檀栋,胡泽勇,等. 青藏高原能量与水循环国际合作研究的进展与展望[J]. 地球科学进展,2009(11).
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[11] 王宾宾,马耀明,马伟强. 青藏高原那曲地区modis地表温度估算[J]. 遥感学报,2012(6).
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[12] 余武生,马耀明,孙维贞,等. 青藏高原西部降水中δ~(18)o变化特征及其气候意义[J]. 科学通报,2009(15).
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