Surface DEM for typical glaciers on the Tibetan Plateau (Version 1.0) (2003)
Jiang, L. (2018). Surface DEM for typical glaciers on the Tibetan Plateau (Version 1.0) (2003). A Big Earth Data Platform for Three Poles, DOI: 10.11888/Glacio.tpdc.270046. CSTR: 18406.11.Glacio.tpdc.270046. (Download the reference: RIS | Bibtex )
Related Literatures:1. Sun, Y., Jiang, L., Liu, L., Sun, Q., & Hsu, H. (2017). Mapping glacier elevations and their changes in the western qilian mountains, northern tibetan plateau, by bistatic insar. IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, PP(99), 1-11.( View Details | Bibtex)
2. Sun, Y.F., Jiang, L., Sun, Q., Liu, L., Zhang, Z.M., & Sun, Y.L., et al. (2016). Glacial surface topography and its changes in the Western Qilian Mountains derived from TanDEM-X Bi-Static InSAR. Geoscience & Remote Sensing Symposium. IEEE.( View Details | Bibtex)
3. Liu, L., Jiang, L., Sun, Y., Yi, C., Wang, H., & Hsu, H. (2016). Glacier elevation changes (2012–2016) of the puruogangri ice field on the tibetan plateau derived from bi-temporal tandem-x insar data. International Journal of Remote Sensing, 37(24), 5687-5707.( View Details | Bibtex)
4. Sun, Y.F., Jiang, L.M., Liu, L., Sun, Y.L., Wang, H.S., (2016). Generating and evaluating digital terrain model with TanDEM-X bistatic SAR interferometry, Geomatics and Information Science of Wuhan University, 41(1), 100-105.( View Details | Bibtex)
5. Liu, L., Jiang, L., Sun, Y., Wang, H., Yi, C., & Hsu, H., et al. (2016). Morphometric controls on glacier mass balance of the puruogangri ice field, central tibetan plateau. WATER, 8(11).( View Details | Bibtex)
Using this data, the data citation is required to be referenced and the related literatures are suggested to be cited.
现代大地测量及其地学应用的研究 (No:4102100)
CASEarth:Big Earth Data for Three Poles(grant No. XDA19070000) (No:XDA19000000)
the Strategic Priority Research Program of the Chinese Academy of Sciences (No:XDA19070104) [XDA19070104]
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East: 97.00 | West: 80.00 |
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South: 33.00 | North: 40.00 |
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