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Thermoelastic Seasonal Deformation in Chinese Mainland
2017
Acta Geodaetica et Cartographica Sinica
In this paper, we explore the thermoelastic seasonal deformation in Chinese mainland based on the 260 GPS sites of crustal movement observation network of China (CMONOC). The results show that the change of land surface temperature can induce remarkable surface deformation in China. The most affected site is HLAR in Inner Mongolia, China. Its seasonal amplitude of surface deformation is about~2.293mm. and the site HIYS in Hainan is the least affected. The seasonal amplitude of surface
doi:10.11947/j.agcs.2017.20160628
doaj:2d4faa88cd5f46839995231db544263b
fatcat:onazjnfriffavdxi5onjspglcq