The data is stored in raster tif format, File naming rules are as follows:
Monthly cumulative ET value file name: heihe-1km_2013m01_eta.tif
Heihe represents the heihe river basin, 1km represents the resolution of 1km, 2013 represents the year of 2013, m01 represents the month of January, eta represents the actual evapotranspiration data, and tif represents the data in tif format.
Name of quarterly cumulative ET value file: heihe-1km_2013s01_eta.tif
Heihe refers to heihe river basin, 1km refers to the resolution of 1km, 2013 refers to 2013, s01 refers to january-march, is the first quarter, eta refers to the actual evapotranspiration data, and tif refers to the data in tif format.
Annual cumulative value file name: heihe-1km_2013y_eta.tif
Among them, heihe represents heihe river basin, 1km represents the resolution of 1km, 2013 represents the year of 2013, y represents the year, eta represents the actual evapotranspiration data, and tif represents the data in tif format.
Data reading: Envi, Arcgis and other remote sensing software can be used to open and read
Monthly evapotranspiration dataset with 1 km spatial resolution over the Heihe River Basin Version 2.0 (2000-2013). A Big Earth Data Platform for Three Poles, 2015. doi: 10.11888/Hydro.tpdc.270884. (Download the reference： RIS | Bibtex )Related Literatures:
1. Bingfang Wu, Nana Yan, Jun Xiong, W.G.M.Bastiaanssen, Weiwei Zhu, Alfred Stein. Validation of ETWatch using field measurements at diverse landscapes: A case study in Hai Basin of China. Journal of Hydrlolgy. 436-437(2012) 67-80.( View Details | Bibtex)
2. Wu,B.F, Zhu,W.W, Yan,N.N, Xing,Q, Liu,S.F, Chang,S, Qi,F. Integration of parameterization based on mult-source remote sensing data for estimation evapotranspiration: A case study on Heihe River Basin. Manuscript under preparation.( View Details | Bibtex)
Using this data, the data citation is required to be referenced and the related literatures are suggested to be cited.
1.Wu, B. , Yan, N. , Xiong, J. , Bastiaanssen, W. G. M. , Zhu, W. , & Stein, A. . (2012). Validation of etwatch using field measurements at diverse landscapes: a case study in hai basin of china. Journal of Hydrology, 436-437(none), 67-80. (View Details )
2.Wu, B. , Xing, Q. , Yan, N. , Zhu, W. , & Zhuang, Q. . (2015). A linear relationship between temporal multiband modis brdf and aerodynamic roughness in hiwater wind gradient data. Geoscience and Remote Sensing Letters, IEEE, 12(3), 507-511. (View Details )
3.Feng,X.L, Wu,B.F,Yan,N.N, Zhu,W.W. Method to derived mixed boundary layer height from MODIS atmospheric profile data product at Heihe river basin. Boundary-layer Meteorology. Under Review. (View Details | Download )
4.Wu, B., Zhu, W., Yan, N., Feng, X., Xing, Q., Zhuang, Q., An improved method for deriving daily evapotranspiration estimates from satellite estimates on cloud-free days. IEEE Journal of Selected Topic in Applied Earth Observations and Remote Sensing. (Under Review). (View Details )
5.Wu, B. , Yan, N. , Xiong, J. , Bastiaanssen, W. G. M. , Zhu, W. , & Stein, A. . (2012). Validation of etwatch using field measurements at diverse landscapes: a case study in hai basin of china. Journal of Hydrology, 436-437(none), 67-80. (View Details )
6.Xiong, J. , Wu, B. F. , Yan, N. , Zeng, Y. , & Liu, S. . (2010). Estimation and validation of land surface evaporation using remote sensing and meteorological data in north china. Selected Topics in Applied Earth Observations and Remote Sensing, IEEE Journal of, 3(3), P.337-344. (View Details )
7.Zhang, H. , Wu, B. , Yan, N. , Zhu, W. , & Feng, X. . (2014). An improved satellite-based approach for estimating vapor pressure deficit from modis data. Journal of Geophysical Research: Atmospheres, 119(21), 12,256-12,271. (View Details )
8.Zhu, W. , Wu, B. , Yan, N. , Feng, X. , & Xing, Q. . (2014). A method to estimate diurnal surface soil heat flux from modis data for a sparse vegetation and bare soil. Journal of Hydrology, 511, 139-150. (View Details )
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License： This work is licensed under an Attribution 4.0 International (CC BY 4.0)
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|South: 37.00||North: 42.00|
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