Satellite measurements reveal strong anisotropy in spatial coherence of climate variations over the Tibet Plateau
Author:
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/srep30304.pdf
Reference42 articles.
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2. Bookhagen, B. Appearance of extreme monsoonal rainfall events and their impact on erosion in the Himalaya. Geomatics, Natural Hazards and Risk 1, 37–50 (2010).
3. Joswiak, D. R., Yao, T., Wu, G., Xu, B. & Zheng, W. A 70-yr record of oxygen-18 variability in 551 an ice core from the Tanggula Mountains, central Tibetan Plateau. Clim. Past 6, 219–227 (2010).
4. Kaspari, S. et al. Snow accumulation rate on Qomolangma (Mount Everest), Himalaya: synchroneity with sites across the Tibetan Plateau on 50–100 year timescales. J. Glaciol. 54(185), 343–352 (2008).
5. Okamoto, S. et al. Reevaluation of the reconstruction of summer temperatures from melt features in Belukha ice cores, Siberian Altai. J Geophys Res 116(D2), D02110, 10.1029/2010JD013977 (2011).
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