Increased mass over the Tibetan Plateau: From lakes or glaciers?
Version of Record online: 30 MAY 2013
©2013. American Geophysical Union. All Rights Reserved.
Geophysical Research Letters
Volume 40, Issue 10, pages 2125–2130, 28 May 2013
How to Cite
2013), Increased mass over the Tibetan Plateau: From lakes or glaciers?, Geophys. Res. Lett., 40, 2125–2130, doi:10.1002/grl.50462., , , , and (
- Issue online: 1 JUL 2013
- Version of Record online: 30 MAY 2013
- Accepted manuscript online: 11 APR 2013 12:00AM EST
- Manuscript Accepted: 10 APR 2013
- Manuscript Revised: 1 APR 2013
- Manuscript Received: 18 FEB 2013
- National Natural Science Foundation of China. Grant Numbers: 41190081, 31228021
- China Postdoctoral Science Foundation. Grant Number: 2011M500405
Additional supporting information may be found in the online version of this article.
|grl50462-sup-0001-Table_S1.pdf||PDF document||92K||The Number of Lakes (Percentage %), Water Level Change Rate (m/yr, Increasing (I) or Decreasing (D)), Area of Lakes With ICESat Data (104 km2) and Mass Change Rate (Gt/yr) of Basins in the Inner Tibet Plateau (I). The Inner Tibet Plateau is Further Divided Into Six Sub-basins (A, B, C, D, E, F).|
|grl50462-sup-0002-Figure S1.tif||TIFF image||26622K||Rate of lake level change vs. mass change by basin (left) and six sub-basins (A-F) in the ITP (right).|
|grl50462-sup-0003-2013GL055626_readme.txt||plain text document||1K||Supplementary Information|
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