Articles | Volume 24, issue 12
Hydrol. Earth Syst. Sci., 24, 5745–5758, 2020
Hydrol. Earth Syst. Sci., 24, 5745–5758, 2020
Review article
01 Dec 2020
Review article | 01 Dec 2020

Last-decade progress in understanding and modeling the land surface processes on the Tibetan Plateau

Hui Lu et al.

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Cited articles

Bai, P., Liu, X. M., Yang, T. T., Liang, K., and Liu, C. M.: Evaluation of streamflow simulation results of land surface models in GLDAS on the Tibetan plateau, J. Geophys. Res.-Atmos., 121, 12180–12197, 2016. 
Bao, H., Koike, T., Yang, K., Wang, L., Shrestha, M., and Lawford, P.: Development of an enthalpy-based frozen soil model and its validation in a cold region in China, J. Geophys. Res.-Atmos., 121, 5259–5280,, 2016. 
Beljaars, A. C. M., Brown, A. R., and Wood, N.: A new parametrization of turbulent orographic form drag, Q. J. Roy. Meteor. Soc., 130, 1327–1347,, 2004. 
Chen, Y. Y., Yang, K., He, J., Qin, J., Shi, J. C., Du, J. Y., and He, Q.: Improving land surface temperature modeling for dry land of China, J. Geophys. Res.-Atmos., 116, D20104,, 2011. 
Short summary
The Tibetan Plateau (TP), known as the Asian water tower, plays an important role in the regional climate system, while the land surface process is a key component through which the TP impacts the water and energy cycles. In this paper, we reviewed the progress achieved in the last decade in understanding and modeling the land surface processes on the TP. Based on this review, perspectives on the further improvement of land surface modelling on the TP are also provided.