Groundwater level dataset in the middle and lower of Heihe River Basin (2013-2015)

Groundwater level dataset in the middle and lower of Heihe River Basin (2013-2015)


Through e-Sense / diver hydrological monitoring equipment and dynamic remote monitoring system, the hydrological monitoring data of key stations in Heihe River Basin in the three years from 2013 to 2015 in non freezing period are obtained, mainly including the temperature and water level of three groundwater (Qilian station, Linze station, Ejina station) and six river surface water (Yingluoxia station, Gaoya station, Zhengyixia station, shaomaying station, langxinshan station, Juyanhai station) According to the data, the time resolution is 1H.


File naming and required software

The data is stored in the form of XLS and can be read by office, WPS and other office software


Data Citations Data citation guideline What's data citation?
Cite as:

Zheng, C. (2017). Groundwater level dataset in the middle and lower of Heihe River Basin (2013-2015). A Big Earth Data Platform for Three Poles, DOI: 10.11888/Hydro.tpdc.270841. CSTR: 18406.11.Hydro.tpdc.270841. (Download the reference: RIS | Bibtex )

Related Literatures:

1. Tian, Y., Zheng, Y., Zheng, C., et al (2015). Exploring scale‐dependent ecohydrological responses in a large endorheic river basin through integrated surface water‐groundwater modeling. Water Resources Research, 51(6): 4065-4085.( 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)


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Keywords
Geographic coverage
East: 103.00 West: 96.00
South: 38.00 North: 43.00
Details
  • Temporal resolution: Yearly
  • File size: 10 MB
  • Views: 4817
  • Downloads: 24
  • Access: Requestable
  • Temporal coverage: 2013-11-05 To 2016-05-06
  • Updated time: 2021-04-19
Contacts
: ZHENG Chunmiao  

Distributor: A Big Earth Data Platform for Three Poles

Email: poles@itpcas.ac.cn

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