Preprints
https://doi.org/10.5194/tc-2016-165
https://doi.org/10.5194/tc-2016-165
14 Jul 2016
 | 14 Jul 2016
Status: this preprint was under review for the journal TC. A revision for further review has not been submitted.

Slight glacier reduction over the northwestern Tibetan Plateau despite significant recent warming

Yetang Wang, Shugui Hou, Wenling An, Hongxi Pang, and Yaping Liu

Abstract. "Pamir–Karakoram–Western-Kunlun-Mountain (northwestern Tibetan Plateau) Glacier Anomaly" has been a topic of debate due to the balanced, or even slightly positive glacier mass budgets in the early 21st century. Here we focus on the evolution of glaciers on the western Kunlun Mountain and its comparison with those from other regions of the Tibetan Plateau. The possible driver for the glacier evolution is also discussed. Western Kunlun Mountain glaciers reduce in area by 0.12 % yr−1 from 1970s to 2007–2011. However, there is no significant area change after 1999. Averaged glacier thickness loss is 0.08 ± 0.09 m yr−1 from 1970s to 2000, which is in accordance with elevation change during the period 2003–2008 estimated by the ICESat laser altimetry measurements. These further confirm the anomaly of glaciers in this region. Slight glacier reduction over the northwestern Tibetan Plateau may result from more accumulation from increased precipitation in winter which to great extent protects it from mass reductions under climate warming during 1961–2000. Warming slowdown since 2000 happening at this region may further mitigate glacier mass reduction, especially for the early 21st century.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
Yetang Wang, Shugui Hou, Wenling An, Hongxi Pang, and Yaping Liu
 
Status: closed (peer review stopped)
Status: closed (peer review stopped)
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement
 
Status: closed (peer review stopped)
Status: closed (peer review stopped)
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement
Yetang Wang, Shugui Hou, Wenling An, Hongxi Pang, and Yaping Liu
Yetang Wang, Shugui Hou, Wenling An, Hongxi Pang, and Yaping Liu

Viewed

Total article views: 2,447 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,608 602 237 2,447 149 236
  • HTML: 1,608
  • PDF: 602
  • XML: 237
  • Total: 2,447
  • BibTeX: 149
  • EndNote: 236
Views and downloads (calculated since 14 Jul 2016)
Cumulative views and downloads (calculated since 14 Jul 2016)

Cited

Latest update: 02 Nov 2024
Download
Short summary
This study further confirms "Pamir–Karakoram–Western-Kunlun-Mountain (northwestern Tibetan Plateau) Glacier Anomaly". Slight glacier reduction over the northwestern Tibetan Plateau may result from more accumulation from increased precipitation in winter which to great extent protects it from mass reductions under climate warming during 1961–2000. Warming slowdown since 2000 happening at this region may further mitigate glacier mass reduction.