| Response of magnitude of δ~(18)O in shallow ice core of Dasuopu Glacier in the Tibetan Plateau to large scale sea-air interaction |
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| 作者姓名： | ZHANG Xin-ping YAO Tan-dong XIE Zi-chu |
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| 作者单位： | ZHANG Xin-ping; YAO Tan-dong; XIE Zi-chu(Hunan Normal University，Changsha 410081，China. E-mail; zxp@ hunnu.edu.cn;)(Lanzhou Institute of Glaciology and Geocryology，CAS，Lanzhou 73000，China) |
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| 摘 要： | lintroductionOceanandatmospherearetwoimposestmembersinclAnahcSystem.Thesea-airinterachon.showedbyfileglobalq'cleonthebasisofthemoist'Ureandenergy.formstheSynophcandclAnahcprocessesofthet!ariousspahalandtempolalscalesovertheealth.Thetheorehcanalysesshot'-thatthemostimportantph}'sicalprocessisnon-adiabahc11eatingforthelong-termatmosphericProcess.Themtalmtunheatsoufceonaleealth--oceanwhuencestheAnospllerebymeansoftilevariahonofitSseasaucetemperature(SST),andthereforechangesthetranSportahonof…
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| 关 键 词： | Dasuopu Glacier shallow ice core δ~(18)O SST atmospheric circulation |
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