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DOI10.1007/s11629-021-7157-9
Reconstructed annual glacier surface mass balance in the anyemaqen Mountains, Yellow River source, based on snow line altitude
Li, Kai-ji; Cao, Bo; Guan, Wei-jin; Pan, Bao-tian; Shangguan, Dong-hui
通讯作者Cao, B (通讯作者),Lanzhou Univ, Coll Earth & Environm Sci, Key Lab Western Chinas Environm Syst MOE, Lanzhou 730000, Peoples R China. ; Cao, B (通讯作者),Shiyang River Basin Sci Observing Stn, Lanzhou 730000, Gansu, Peoples R China.
发表日期2022
ISSN1672-6316
EISSN1993-0321
起始页码1070
结束页码1081
卷号19期号:4
英文摘要Annual mass balance is an important factor that reflects glacier change and glacier meltwater resources. In this study, we analyzed the changes in glacier area, snow line altitude (SLA) and surface elevation in the anyemaqen Mountain region using multisource remote sensing data. Then, the annual mass balance of two glaciers was reconstructed by using SLA-mass-balance gradient method. The results showed that the glacier area in the anyemaqen Mountains decreased by 29.4 km(2) from 1985 to 2017. The average SLAs of the Halong Glacier and Yehelong Glacier were approximately 5290 m and 5188 m, respectively. The glacier mass balance for the two glaciers from 1990 to 2020 was - 0.71 m w.e. a(-1) and -0.63 m w.e. a(-1), respectively. Our results indicate that SLA is an important indicator of glacier changes, and a long sequence of SLAs can more accurately reconstruct the glacier mass balance of the glacier. The mean annual glacial meltwater-fed streamflow is 1.45 x 10(7) m(3) and 1.12 x 10(7) m(3), respectively. Sensitivity analysis indicates that summer air temperature plays a leading role in regard to the influential climatic factors of glacial retreat in the Anyemaqen Mountains. This highlights the potential of the methodology for application on reconstructing annual glacier surface mass balance at larger scales without direct measurements.
关键词EQUILIBRIUM-LINETIBETAN PLATEAULANDSAT IMAGERYGONGGA MOUNTAINSTOPOGRAPHIC MAPSRESOLUTIONINVENTORYVOLUMECOVERSRTM
英文关键词Snow line altitude (SLA); Glacier annual mass balance reconstruction; Glacier changes; Anyemaqen Mountains
语种英语
WOS研究方向Environmental Sciences & Ecology
WOS类目Environmental Sciences
WOS记录号WOS:000783541800011
来源期刊JOURNAL OF MOUNTAIN SCIENCE
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/254787
作者单位[Li, Kai-ji; Cao, Bo; Guan, Wei-jin; Pan, Bao-tian] Lanzhou Univ, Coll Earth & Environm Sci, Key Lab Western Chinas Environm Syst MOE, Lanzhou 730000, Peoples R China; [Cao, Bo; Pan, Bao-tian] Shiyang River Basin Sci Observing Stn, Lanzhou 730000, Gansu, Peoples R China; [Shangguan, Dong-hui] Chinese Acad Sci, State Key Lab Cryospher Sci SKLCS, Northwest Inst Ecoenvironm & Resources, Lanzhou 730000, Peoples R China
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GB/T 7714
Li, Kai-ji,Cao, Bo,Guan, Wei-jin,et al. Reconstructed annual glacier surface mass balance in the anyemaqen Mountains, Yellow River source, based on snow line altitude[J]. 中国科学院西北生态环境资源研究院,2022,19(4).
APA Li, Kai-ji,Cao, Bo,Guan, Wei-jin,Pan, Bao-tian,&Shangguan, Dong-hui.(2022).Reconstructed annual glacier surface mass balance in the anyemaqen Mountains, Yellow River source, based on snow line altitude.JOURNAL OF MOUNTAIN SCIENCE,19(4).
MLA Li, Kai-ji,et al."Reconstructed annual glacier surface mass balance in the anyemaqen Mountains, Yellow River source, based on snow line altitude".JOURNAL OF MOUNTAIN SCIENCE 19.4(2022).
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