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DOI | 10.1080/16000889.2018.1468705 |
Distributions and light absorption property of water soluble organic carbon in a typical temperate glacier, southeastern Tibetan Plateau | |
Niu, Hewen; Kang, Shichang; Lu, Xixi; Shi, Xiaofei | |
发表日期 | 2018 |
ISSN | 1600-0889 |
卷号 | 70 |
英文摘要 | Water-soluble organic carbon (WSOC) widely stored in glaciers from local and distant sources, and then released it to downstream environments under a warming climate. Climatic driven changes to glacial run-off are larger and represent an important flux of organic carbon. However, very few WSOC data are currently available to fully characterize WSOC variation in the temperate glacierized regions of the Tibetan Plateau (TP). This study first systematically evaluated the concentration characteristics and light absorbing property of WSOC, and insoluble particulate carbon (IPC) in snow and ice of a typical temperate glacier on Mt. Yulong. Average concentrations of WSOC were 0.610.21mg L-1 in Baishui glacier on Mt. Yulong. WSOC concentrations in surface aged snow were dramatically decreased with the time extension during the entire monsoon season due to extensive glacial melting and scavenging effects by meltwater.The MAC values of WSOC calculated at 365nm was 6.31 +/- 0.34 m(2) g(-1) on Mt. Yulong, and there exists distinct spectral dependence of MAC(wsoc) within the wavelength range (260-700nm). The low AAE(330-400) values suggest the light absorption of WSOC is more spectrally neutral. The flux of WSOC in Baishui glacier was 0.99 gC m(-2)yr(-1), while the IPC flux was 4.77 gC m(-2)yr(-1). Total WSOC storage in the Baishui glacier was estimated to be 1.5 tone C and total IPC storage was 7.25 tone C (1 tone =10(6)g). Moreover, glacial melting was reinforced by the soluble and insoluble light absorbing impurities (ILAIs) in glaciers, Baishui glacier can be considered as a fraction of carbon source under the scenario of a warming climate, more importantly, WSOC in snow and ice needs to be taken into account in calculating the radiative forcing of ILAIs and accelerating glacial melting. |
关键词 | fluxglacierMtYulongTibetan PlateauWSOC |
学科领域 | Meteorology & Atmospheric Sciences |
语种 | 英语 |
WOS研究方向 | Meteorology & Atmospheric Sciences |
来源期刊 | TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY |
来源机构 | 中国科学院西北生态环境资源研究院 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/111960 |
作者单位 | Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Cryospher Sci, Yulong Snow Mt Glacier Environm Observat & Res St, Lanzhou, Gansu, Peoples R China |
推荐引用方式 GB/T 7714 | Niu, Hewen,Kang, Shichang,Lu, Xixi,et al. Distributions and light absorption property of water soluble organic carbon in a typical temperate glacier, southeastern Tibetan Plateau[J]. 中国科学院西北生态环境资源研究院,2018,70. |
APA | Niu, Hewen,Kang, Shichang,Lu, Xixi,&Shi, Xiaofei.(2018).Distributions and light absorption property of water soluble organic carbon in a typical temperate glacier, southeastern Tibetan Plateau.TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY,70. |
MLA | Niu, Hewen,et al."Distributions and light absorption property of water soluble organic carbon in a typical temperate glacier, southeastern Tibetan Plateau".TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY 70(2018). |
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