Dissolved organic carbon fractionation accelerates glacier-melting: A case study in the northern Tibetan Plateau
Creators
- 1. University of Chinese Academy of Sciences, Beijing 100039 (China)
- 2. State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-environment and Resources, Chinese Academy of Sciences, Lanzhou 730000 (China)
- 3. CAS Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, Beijing 100101 (China)
- 4. Laboratory of Green Chemistry, Lappeenranta University of Technology, Sammonkatu 12, Mikkeli 50130 (Finland)
- 5. Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100085 (China)
Description
Highlights: • Fractionation and RF change of DOC during the melting process were investigated. • DOC with high MAC365 value was easy to keep in snow/ice during the melting process. • DOC with high MAC365 value also had low wavelength dependence. • RF caused by fresh snow DOC significantly increased during the melting process. In glacierized regions, melting process has a significant effect on concentrations and light absorption characteristics of dissolved organic carbon (DOC), potentially resulting in variations of its radiative forcing, which is not yet relevant research at glacier region of the Tibetan Plateau (TP). In this study, DOC fractionation and its radiative forcing change during the melting process were investigated at Laohugou glacier No. 12 (LHG glacier) in western Qilian Mts., northern TP. DOC concentrations in fresh snow, snowpit and surface ice samples were 0.38 ± 0.06, 0.22 ± 0.11 and 0.60 ± 0.21 mg L−1, respectively. Their mass absorption cross-section at 365 nm (MAC365) were 0.65 ± 0.16, 4.71 ± 3.68 and 1.44 ± 0.52 m2 g−1, respectively. The MAC365 values of snowpit samples showed a significant negative correlation with DOC concentrations, indicating DOC with high MAC365 values were likely to be kept in snow during the melting process. Topsoil samples of LHG glacierized region likely contributed a lot to snowpit DOC with high MAC365 values due to their similar absorption spectra. Spatially, the DOC concentration of surface ice samples increased from terminus to the upper part of the glacier. Correspondingly, the MAC365 value showed decreased trend. In the freezing experiment on surface ice and topsoil samples, small part of DOC with high MAC365 value was also likely to enter first frozen solid phase. In addition, the radiative forcing caused by snowpit and surface ice DOC increased around 7.64 ± 2.93 and 4.95 ± 1.19 times relative to fresh snow DOC, indicating the snow/ice melting caused by increased light-absorbing DOC needs to be considered in the future research.
Availability note (English)
Available from http://dx.doi.org/10.1016/j.scitotenv.2018.01.265Additional details
Identifiers
- DOI
- 10.1016/j.scitotenv.2018.01.265;
- PII
- S0048969718303073;
Publishing Information
- Journal Title
- Science of the Total Environment
- Journal Volume
- 627
- Journal Page Range
- p. 579-585
- ISSN
- 0048-9697
- CODEN
- STENDL
INIS
- Country of Publication
- Netherlands
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 53029309
- Subject category
- S54: ENVIRONMENTAL SCIENCES;
- Descriptors DEI
- ABSORPTION SPECTRA; CARBON; ECOLOGICAL CONCENTRATION; FREEZING; FREQUENCY DEPENDENCE; GLACIERS; ICE; MELTING; ORGANIC MATTER; RADIATIVE FORCING; SNOW; SOLIDS
- Descriptors DEC
- ATMOSPHERIC PRECIPITATIONS; ELEMENTS; MATTER; NONMETALS; PHASE TRANSFORMATIONS; SPECTRA
Optional Information
- Copyright
- Copyright (c) 2018 Elsevier B.V. All rights reserved.