Carbonaceous matter deposition in the high glacial regions of the Tibetan Plateau
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- 作者：Chaoliu Lia ; d ; lichaoliu@itpcas.ac.cn" class="auth_mail" title="E-mail the corresponding author ; Pengfei Chena ; c ; Shichang Kangb ; d ; shichang.kang@lzb.ac.cn" class="auth_mail" title="E-mail the corresponding author ; Fangping Yanb ; c ; Xiaofei Lib ; c ; Bin Que ; Mika Sillanpä ; ä ; e
- 关键词：Carbonaceous matter ; Dissolved organic carbon ; Flux ; The Tibetan Plateau ; Glacier
- 刊名：Atmospheric Environment
- 出版年：2016
- 出版时间：September 2016
- 年：2016
- 卷：141
- 期：Complete
- 页码：203-208
- 全文大小：847 K
文摘
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DOC at glacial region of the TP is low and mainly contributed by natural dust.
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DOC at glacial region is significantly related to that of IPC for all the TP.
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DOC flux is 0.11 ± 0.05 g-C m−2 yr−1 at glacial region of the TP.