Share Email Print
cover

Proceedings Paper

Three-dimensional monitoring of ice-snow in Qinghai-Tibet Plateau: a case of Geladandong
Author(s): Zhigang Hong; Nan Cong; Li Zhang; Bo Ai
Format Member Price Non-Member Price
PDF $14.40 $18.00
cover GOOD NEWS! Your organization subscribes to the SPIE Digital Library. You may be able to download this paper for free. Check Access

Paper Abstract

The research on ice-snow gained the concerns of a lot of researchers in ecology, geography, meteorology and so on in the past years, and a series of achievements in scientific research has been gained. Especially, remarkable advances have been made in ice-snow science after the application of remote sensing techniques. A snow mountain area in Qinghai-Tibet Plateau was chosen as the study area. The DEM was constructed by use of the peculiar stereo data collection function of HRS on SPOT5. The three-dimensional (3D for short) monitoring model was set up, and the superficial area was computed based on the TIN model. At last, the authors synthetically estimated the ice-snow resources status combining to the results gained before. The aim of this study is to provide theory and scientific evidence for the efficient management of ice-snow resource, and furthermore provide scientific evidence for the macroscopical adjust and control of water resource and sustainable development in China.

Paper Details

Date Published: 9 October 2009
PDF: 8 pages
Proc. SPIE 7471, Second International Conference on Earth Observation for Global Changes, 747113 (9 October 2009); doi: 10.1117/12.847905
Show Author Affiliations
Zhigang Hong, Chinese Academy of Surveying and Mapping (China)
Nan Cong, Chinese Academy of Surveying and Mapping (China)
Li Zhang, Chinese Academy of Surveying and Mapping (China)
Bo Ai, Chinese Academy of Surveying and Mapping (China)


Published in SPIE Proceedings Vol. 7471:
Second International Conference on Earth Observation for Global Changes
Xianfeng Zhang; Jonathan Li; Guoxiang Liu; Xiaojun Yang, Editor(s)

© SPIE. Terms of Use
Back to Top