Modeling ecohydrological processes and spatial patterns in the upstream of the Heihe river basin (1960-2014) V3.0- A Big Earth Data Platform for Three Poles

The output data of the distributed eco hydrological model (gbehm) in the upper reaches of Heihe River includes the spatial distribution data series of 1-km grid. Region: Heihe River (Yingluo gorge), Beida River (Binggou new land), temporal resolution: Monthly Scale, spatial resolution: 1km, period: 1960-2014.

Data include precipitation, evapotranspiration, runoff depth, soil volume water content (0-100cm).

All data are in ASCII format. Please refer to the basin.asc file in the reference directory for the spatial range of the basin.

Projection parameters of model results: sphere_Arc_Info_Lambert_Azimuthal_Equal_Area

File naming and required software

The data is stored in text format, which can be opened and read by a text program (such as Notepad). If you want to display it with a diagram, you can open it by ArcGIS, and a file in grid format will be generated during the reading process.

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Cite as:

Yang, D. (2017). Modeling ecohydrological processes and spatial patterns in the upstream of the Heihe river basin (1960-2014) V3.0. A Big Earth Data Platform for Three Poles, DOI: 10.3972/heihe.9966.2013.db. CSTR: 18406.11.heihe.9966.2013.db. (Download the reference： RIS | Bibtex )

Related Literatures:

1. Gao, B., Qin, Y., Wang, Y.H., Yang, D.W., &Zheng, Y.R. (2016). Modeling Ecohydrological Processes and Spatial Patterns in the Upper Heihe Basin in China. Forests, 7(1), 10.( View Details | Bibtex)

2. Gao, B., Yang, D., Qin, Y., Wang, Y., Li, H., Zhang, Y., & Zhang, T. (2018). Change in Frozen grounds and Its Effect on Regional Hydrology in the Upper Heihe Basin, on the Northeastern Qinghai-Tibetan Plateau. The Cryosphere. 12(2), 657-673.( View Details | Bibtex)

Using this data, the data citation is required to be referenced and the related literatures are suggested to be cited.

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License： This work is licensed under an Attribution 4.0 International (CC BY 4.0)