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1000 Titel
  • Recent Third Pole’s Rapid Warming Accompanies Cryospheric Melt and Water Cycle Intensification and Interactions between Monsoon and Environment: Multidisciplinary Approach with Observations, Modeling, and Analysis
1000 Autor/in
  1. Yao, Tandong |
  2. xue, yongkang |
  3. Chen, Deliang |
  4. Chen, Fahu |
  5. Thompson, Lonnie |
  6. Cui, Peng |
  7. Koike, Toshio |
  8. Lau, William K. M. |
  9. Lettenmaier, Dennis |
  10. Mosbrugger, Volker |
  11. Zhang, Renhe |
  12. Yu, Baiqing |
  13. Dozier, Jeff |
  14. Gillespie, Thomas |
  15. Gu, Yu |
  16. Kang, Shichang |
  17. Piao, Shilong |
  18. Sugimoto, Shiori |
  19. Ueno, Kenichi |
  20. Wang, Lei |
  21. Wang, Weicai |
  22. Zhang, Fan |
  23. Sheng, Yongwei |
  24. Guo, Weidong |
  25. Ailikun |
  26. Yang, Xiaoxin |
  27. Ma, Yaoming |
  28. Shen, Samuel S. P. |
  29. Su, Zhongbo |
  30. Chen, Fei |
  31. Liang, Shunlin |
  32. Liu, Yimin |
  33. Singh, Vijay P. |
  34. Yang, Kun |
  35. Yang, Daqing |
  36. Zhao, Xinquan |
  37. Qian, Yun |
  38. Zhang, Yu |
  39. Li, Qian |
1000 Erscheinungsjahr 2018
1000 LeibnizOpen
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2018-08-30
1000 Erschienen in
1000 Quellenangabe
  • 100(3):423-444
1000 FRL-Sammlung
1000 Copyrightjahr
  • 2018
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.1175/BAMS-D-17-0057.1 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • The Third Pole (TP) is experiencing rapid warming and is currently in its warmest period in the past 2,000 years. This paper reviews the latest development in multidisciplinary TP research associated with this warming. The rapid warming facilitates intense and broad glacier melt over most of the TP, although some glaciers in the northwest are advancing. By heating the atmosphere and reducing snow/ice albedo, aerosols also contribute to the glaciers melting. Glacier melt is accompanied by lake expansion and intensification of the water cycle over the TP. Precipitation has increased over the eastern and northwestern TP. Meanwhile, the TP is greening and most regions are experiencing advancing phenological trends, although over the southwest there is a spring phenological delay mainly in response to the recent decline in spring precipitation. Atmospheric and terrestrial thermal and dynamical processes over the TP affect the Asian monsoon at different scales. Recent evidence indicates substantial roles that mesoscale convective systems play in the TP’s precipitation as well as an association between soil moisture anomalies in the TP and the Indian monsoon. Moreover, an increase in geohazard events has been associated with recent environmental changes, some of which have had catastrophic consequences caused by glacial lake outbursts and landslides. Active debris flows are growing in both frequency of occurrences and spatial scale. Meanwhile, new types of disasters, such as the twin ice avalanches in Ali in 2016, are now appearing in the region. Adaptation and mitigation measures should be taken to help societies’ preparation for future environmental challenges. Some key issues for future TP studies are also discussed.
1000 Fächerklassifikation (DDC)
1000 Liste der Beteiligten
  1. https://orcid.org/0000-0002-8485-9140|https://orcid.org/0000-0002-6169-9631|https://frl.publisso.de/adhoc/uri/Q2hlbiwgRGVsaWFuZw==|https://orcid.org/0000-0002-8874-1035|https://orcid.org/0000-0001-5371-2579|https://frl.publisso.de/adhoc/uri/Q3VpLCBQZW5n|https://frl.publisso.de/adhoc/uri/S29pa2UsIFRvc2hpbw==|https://orcid.org/0000-0002-3587-3691|https://frl.publisso.de/adhoc/uri/TGV0dGVubWFpZXIsIERlbm5pcw==|https://orcid.org/0000-0002-9524-7473|https://frl.publisso.de/adhoc/uri/WmhhbmcsIFJlbmhl|https://orcid.org/0000-0002-2765-6558|https://orcid.org/0000-0001-8542-431X|https://frl.publisso.de/adhoc/uri/R2lsbGVzcGllLCBUaG9tYXM=|https://frl.publisso.de/adhoc/uri/R3UsIFl1|https://frl.publisso.de/adhoc/uri/S2FuZywgU2hpY2hhbmc=|https://frl.publisso.de/adhoc/uri/UGlhbywgU2hpbG9uZw==|https://frl.publisso.de/adhoc/uri/U3VnaW1vdG8sIFNoaW9yaQ==|https://frl.publisso.de/adhoc/uri/VWVubywgS2VuaWNoaQ==|https://frl.publisso.de/adhoc/uri/V2FuZywgTGVp|https://frl.publisso.de/adhoc/uri/V2FuZywgV2VpY2Fp|https://frl.publisso.de/adhoc/uri/WmhhbmcsIEZhbg==|https://frl.publisso.de/adhoc/uri/U2hlbmcsIFlvbmd3ZWk=|https://frl.publisso.de/adhoc/uri/R3VvLCBXZWlkb25n|https://frl.publisso.de/adhoc/uri/QWlsaWt1bg==|https://frl.publisso.de/adhoc/uri/WWFuZywgWGlhb3hpbg==|https://frl.publisso.de/adhoc/uri/TWEsIFlhb21pbmc=|https://frl.publisso.de/adhoc/uri/U2hlbiwgU2FtdWVsIFMuIFAu|https://frl.publisso.de/adhoc/uri/U3UsIFpob25nYm8=|https://frl.publisso.de/adhoc/uri/Q2hlbiwgRmVp|https://frl.publisso.de/adhoc/uri/TGlhbmcsIFNodW5saW4=|https://frl.publisso.de/adhoc/uri/TGl1LCBZaW1pbg==|https://frl.publisso.de/adhoc/uri/U2luZ2gsIFZpamF5IFAu|https://frl.publisso.de/adhoc/uri/WWFuZywgS3Vu|https://frl.publisso.de/adhoc/uri/WWFuZywgRGFxaW5n|https://frl.publisso.de/adhoc/uri/WmhhbywgWGlucXVhbg==|https://frl.publisso.de/adhoc/uri/UWlhbiwgWXVu|https://frl.publisso.de/adhoc/uri/WmhhbmcsIFl1|https://frl.publisso.de/adhoc/uri/TGksIFFpYW4=
1000 Label
1000 Förderer
  1. Chinese Academy of Sciences |
  2. National Natural Science Foundation of China |
  3. National Science Foundation |
1000 Fördernummer
  1. XDA20000000
  2. -
  3. AGS-1419526
1000 Förderprogramm
  1. Strategic Priority Research Program, Frontier Research Program
  2. -
  3. -
1000 Dateien
1000 Förderung
  1. 1000 joinedFunding-child
    1000 Förderer Chinese Academy of Sciences |
    1000 Förderprogramm Strategic Priority Research Program, Frontier Research Program
    1000 Fördernummer XDA20000000
  2. 1000 joinedFunding-child
    1000 Förderer National Natural Science Foundation of China |
    1000 Förderprogramm -
    1000 Fördernummer -
  3. 1000 joinedFunding-child
    1000 Förderer National Science Foundation |
    1000 Förderprogramm -
    1000 Fördernummer AGS-1419526
1000 Objektart article
1000 Beschrieben durch
1000 @id frl:6424688.rdf
1000 Erstellt am 2020-12-10T15:05:57.696+0100
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1000 Zuletzt bearbeitet Fri May 20 18:43:13 CEST 2022
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