This data was obtained using the carbon-water coupled remote sensing evapotranspiration model PML_V2, combined with vorticity-related flux station information from 14 typical subsurfaces on the Tibetan Plateau to calibrate the model, followed by inputting meteorological drivers, remote sensing leaf area index, albedo and emissivity to obtain 0.05 degree, month-by-month terrestrial evapotranspiration on the Tibetan Plateau. The time range is 1982-2016, which can be used for hydrological climate change studies on the Tibetan Plateau at long time scales.
collect time | 1982/01/01 - 2016/12/31 |
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collect place | Tibet Plateau |
data size | 484.5 MiB |
data format | |
Coordinate system |
This data was obtained using the carbon-water coupled remote sensing evapotranspiration model PML_V2, combined with vorticity-related flux station information from 14 typical subsurfaces on the Tibetan Plateau to calibrate the model, followed by inputting meteorological drivers, remote sensing leaf area index, albedo and emissivity to obtain 0.05 degree, month-by-month terrestrial evapotranspiration on the Tibetan Plateau. The time range is from 1982 to 2016. The data are actual land evapotranspiration only and do not include the water surface.
Remote Sensing Evapotranspiration Model PML for Carbon Water Coupling_ V2
Spatial resolution: 0.05 degrees; Time resolution: monthly; Space scope: Qinghai Tibet Plateau land; Time range: 1982-2016
# | title | file size |
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1 | ET_TP_1982_2016_mon_005_PML_V2.nc | 484.5 MiB |
1982 1983 1984 1985 1986 1987 1988 1989 1990 1991 1992 1993 1994 1995 1996 1997 1998 1999 2000 2001 2002 2003 2004 2005 2006 2007 2008 2009 2010 2011 2012 2013 2014 2015 2016
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