Climatic and lake environmental changes in the Serling Co region of Tibet over a variety of timescales
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摘要
<正>The Serling Co region is located at the transitional zone of the interaction between the Indian monsoon and the westerlies over the Tibetan Plateau. The Serling Co lake covers a water area of2,389 km2(June 2017) in a 45,530 km2drainage basin. Under the dramatic hydro-meteorological changes on the Tibetan Plateau in recent decades, and complex hydrological compositions of rivers and lakes in the basin, the lake area expanded by 43%, from1,667 km2in 1976, to 2,389 km2in 2017 [1]. In 2014 it surpassed Nam Co as the largest lake on the Tibetan Plateau [2], and exerts significant effect on regional environmental conditions.
引文
[1]Yang RM,Zhu LP,Wang JB,et al.Spatiotemporal variations in volume of closed lakes on the Tibetan Plateau and their climatic responses from 1976 to 2013.Clim Change 2017;140:621-33.
[2]Song CQ,Ye QH,Cheng X.Shifts in water-level variation of Namco in the central Tibetan Plateau from ICESat and CryoSat-2 altimetry and station observations.Sci Bull 2015;60:1287-97.
[3]Ding J,Zhang Y,Guo Y,et al.Quantitative comparison of river inflows to a rapidly expanding lake in central Tibetan Plateau.Hydrol Process2018;32:3241-53.
[4]Liu C,Zhu LP,Wang JB,et al.Remote sensing-based estimation of lake water clarity and application in a typical lake on the Tibetan Plateau(in Chinese).Prog Geogr 2017;36:597-609.
[5]Yang Y,Hu R,Lin QQ,et al.Spatial structure and b-diversity of phytoplankton in Tibetan Plateau lakes:nestedness or replacement?Hydrobiologia2018;808:301-14.
[6]Lin QQ,Xu L,Hou JZ,et al.Responses of trophic structure and zooplankton community to salinity and temperature in Tibetan lakes:implication for the effect of climate warming.Water Res 2017;124:618-29.
[7]Hou JZ,D’Andrea W,Wang M,et al.Influence of the Indian monsoon and the subtropical jet on climate change on the Tibetan Plateau since the late Pleistocene.Quat Sci Rev 2017;163:84-94.
[8]Gyawali AR,Wang JB,Ma QF,et al.Paleo-environmental change since the Late Glacial inferred from lacustrine sediment in Selin Co,central Tibet.Palaeogeogr Palaeoclim Palaeoecol 2019;516:101-12.
[9]Berger A,Loutre MF.Insolation values for the climate of the last 10 million years.Quat Sci Rev 1991;10:297-317.
[10]Zhu LP,LüXM,Wang JB,et al.Climate change on the Tibetan Plateau in response to shifting atmospheric circulation since the LGM.Sci Rep2015;5:13318.
[11]Herzschuh U,Winter K,Wünnemann B,et al.A general cooling trend on the central Tibetan Plateau throughout the Holocene recorded by the Lake Zigetang pollen spectra.Quat Int 2006;154-155:113-21.
[12]He Y,Bao ZY,Hou JZ,et al.Variation of the mid-latitude westerlies and Indian summer monsoon since the last deglaciation:evidence from grain-size data from Linggo Co,central Tibet.Chin Sci Bull 2016;61:3583-95(in Chinese).
[13]He Y,Hou JZ,Brown ET,et al.Timing of the Indian Summer Monsoon onset during the early Holocene:evidence from a sediment core at Lingge Co,central Tibetan Plateau.Holocene 2017;28:755-66.
[14]Hou JZ,Tian Q,Liang J,et al.Climatic implications of hydrologic changes in two lake catchments on the central Tibetan Plateau since the last glacial.JPaleolimnol 2017;58:257-73.
[2]Song CQ,Ye QH,Cheng X.Shifts in water-level variation of Namco in the central Tibetan Plateau from ICESat and CryoSat-2 altimetry and station observations.Sci Bull 2015;60:1287-97.
[3]Ding J,Zhang Y,Guo Y,et al.Quantitative comparison of river inflows to a rapidly expanding lake in central Tibetan Plateau.Hydrol Process2018;32:3241-53.
[4]Liu C,Zhu LP,Wang JB,et al.Remote sensing-based estimation of lake water clarity and application in a typical lake on the Tibetan Plateau(in Chinese).Prog Geogr 2017;36:597-609.
[5]Yang Y,Hu R,Lin QQ,et al.Spatial structure and b-diversity of phytoplankton in Tibetan Plateau lakes:nestedness or replacement?Hydrobiologia2018;808:301-14.
[6]Lin QQ,Xu L,Hou JZ,et al.Responses of trophic structure and zooplankton community to salinity and temperature in Tibetan lakes:implication for the effect of climate warming.Water Res 2017;124:618-29.
[7]Hou JZ,D’Andrea W,Wang M,et al.Influence of the Indian monsoon and the subtropical jet on climate change on the Tibetan Plateau since the late Pleistocene.Quat Sci Rev 2017;163:84-94.
[8]Gyawali AR,Wang JB,Ma QF,et al.Paleo-environmental change since the Late Glacial inferred from lacustrine sediment in Selin Co,central Tibet.Palaeogeogr Palaeoclim Palaeoecol 2019;516:101-12.
[9]Berger A,Loutre MF.Insolation values for the climate of the last 10 million years.Quat Sci Rev 1991;10:297-317.
[10]Zhu LP,LüXM,Wang JB,et al.Climate change on the Tibetan Plateau in response to shifting atmospheric circulation since the LGM.Sci Rep2015;5:13318.
[11]Herzschuh U,Winter K,Wünnemann B,et al.A general cooling trend on the central Tibetan Plateau throughout the Holocene recorded by the Lake Zigetang pollen spectra.Quat Int 2006;154-155:113-21.
[12]He Y,Bao ZY,Hou JZ,et al.Variation of the mid-latitude westerlies and Indian summer monsoon since the last deglaciation:evidence from grain-size data from Linggo Co,central Tibet.Chin Sci Bull 2016;61:3583-95(in Chinese).
[13]He Y,Hou JZ,Brown ET,et al.Timing of the Indian Summer Monsoon onset during the early Holocene:evidence from a sediment core at Lingge Co,central Tibetan Plateau.Holocene 2017;28:755-66.
[14]Hou JZ,Tian Q,Liang J,et al.Climatic implications of hydrologic changes in two lake catchments on the central Tibetan Plateau since the last glacial.JPaleolimnol 2017;58:257-73.