Evapotranspiration (ET) is a key process of the climate system because it links water, energy and carbon cycles. In this study we modified a Penman–Monteith based algorithm to estimate ET on the Tibetan Plateau at a 1 km spatial resolution for the period 2000–2010 using meteorological and satellite remote sensing data.
Original Source [2]
Links:
[1] http://admin.indiaenvironmentportal.org.in/feature-article/spatio-temporal-dynamics-evapotranspiration-tibetan-plateau-2000-2010
[2] http://iopscience.iop.org/article/10.1088/1748-9326/aa527d
[3] http://admin.indiaenvironmentportal.org.in/category/author/lulu-song
[4] http://admin.indiaenvironmentportal.org.in/category/author/qianlai-zhuang
[5] http://admin.indiaenvironmentportal.org.in/category/author/yunhe-yin-et-al
[6] http://admin.indiaenvironmentportal.org.in/category/journal/environmental-research-letters
[7] http://admin.indiaenvironmentportal.org.in/category/thesaurus/climate-change
[8] http://admin.indiaenvironmentportal.org.in/category/thesaurus/remote-sensing
[9] http://admin.indiaenvironmentportal.org.in/category/thesaurus/rainfall-pattern
[10] http://admin.indiaenvironmentportal.org.in/category/thesaurus/asia