Interannual variations in the hydrothermal regime around a thermokarst lake in Beiluhe, Qinghai-Tibet Plateau

Geomorphology ◽  
2017 ◽  
Vol 276 ◽  
pp. 16-26 ◽  
Author(s):  
Z.J. Lin ◽  
F.J. Niu ◽  
J.H. Fang ◽  
J. Luo ◽  
G.A. Yin
Keyword(s):  
Tibet Plateau ◽  
Interannual Variations ◽  
Hydrothermal Regime ◽  
Thermokarst Lake ◽  
Qinghai Tibet Plateau

Using stable isotopes to illuminate thermokarst lake hydrology in permafrost regions on the Qinghai-Tibet plateau, China

2019 ◽  
Vol 30 (1) ◽  
pp. 58-71 ◽  
Author(s):  
Yuzhong Yang ◽  
Qingbai Wu ◽  
Yandong Hou ◽  
Peng Zhang ◽  
Hanbo Yun ◽  
...  
Keyword(s):  
Stable Isotopes ◽  
Tibet Plateau ◽  
Lake Hydrology ◽  
Thermokarst Lake ◽  
Qinghai Tibet Plateau ◽  
Permafrost Regions

Mapping Permafrost Features that Influence the Hydrological Processes of a Thermokarst Lake on the Qinghai-Tibet Plateau, China

2014 ◽  
Vol 25 (1) ◽  
pp. 60-68 ◽  
Author(s):  
Xicai Pan ◽  
Yanhui You ◽  
Kurt Roth ◽  
Lei Guo ◽  
Xinbing Wang ◽  
...  
Keyword(s):  
Hydrological Processes ◽  
Tibet Plateau ◽  
Thermokarst Lake ◽  
Qinghai Tibet Plateau

scholarly journals Assessing the simulated soil hydrothermal regime of the active layer from the Noah-MP land surface model (v1.1) in the permafrost regions of the Qinghai–Tibet Plateau

2021 ◽  
Vol 14 (3) ◽  
pp. 1753-1771
Author(s):  
Xiangfei Li ◽  
Tonghua Wu ◽  
Xiaodong Wu ◽  
Jie Chen ◽  
Xiaofan Zhu ◽  
...  
Keyword(s):  
Soil Temperature ◽  
Snow Cover ◽  
Land Surface ◽  
Tibet Plateau ◽  
Cold Bias ◽  
Surface Model ◽  
Model Parameters ◽  
Hydrothermal Regime ◽  
Qinghai Tibet Plateau ◽  
Permafrost Regions

Abstract. Extensive and rigorous model intercomparison is of great importance before model application due to the uncertainties in current land surface models (LSMs). Without considering the uncertainties in forcing data and model parameters, this study designed an ensemble of 55 296 experiments to evaluate the Noah LSM with multi-parameterization (Noah-MP) for snow cover events (SCEs), soil temperature (ST) and soil liquid water (SLW) simulation, and investigated the sensitivity of parameterization schemes at a typical permafrost site on the Qinghai–Tibet Plateau (QTP). The results showed that Noah-MP systematically overestimates snow cover, which could be greatly resolved when adopting the sublimation from wind and a semi-implicit snow/soil temperature time scheme. As a result of the overestimated snow, Noah-MP generally underestimates ST, which is mostly influenced by the snow process. A systematic cold bias and large uncertainties in soil temperature remain after eliminating the effects of snow, particularly in the deep layers and during the cold season. The combination of roughness length for heat and under-canopy (below-canopy) aerodynamic resistance contributes to resolving the cold bias in soil temperature. In addition, Noah-MP generally underestimates top SLW. The runoff and groundwater (RUN) process dominates the SLW simulation in comparison to the very limited impacts of all other physical processes. The analysis of the model structural uncertainties and characteristics of each scheme would be constructive to a better understanding of the land surface processes in the permafrost regions of the QTP as well as to further model improvements towards soil hydrothermal regime modeling using LSMs.

Thermal effects of lateral supra-permafrost water flow around a thermokarst lake on the Qinghai-Tibet Plateau

2017 ◽  
Vol 31 (13) ◽  
pp. 2429-2437 ◽  
Author(s):  
Yanhui You ◽  
Qihao Yu ◽  
Xicai Pan ◽  
Xinbin Wang ◽  
Lei Guo ◽  
...  
Keyword(s):  
Water Flow ◽  
Thermal Effects ◽  
Tibet Plateau ◽  
Thermokarst Lake ◽  
Qinghai Tibet Plateau

scholarly journals Contribution of supra-permafrost discharge to thermokarst lake water balances on the northeastern Qinghai-Tibet Plateau

2017 ◽  
Vol 555 ◽  
pp. 621-630 ◽  
Author(s):  
Xicai Pan ◽  
Qihao Yu ◽  
Yanhui You ◽  
Kwok Pan Chun ◽  
Xiaogang Shi ◽  
...  
Keyword(s):  
Lake Water ◽  
Tibet Plateau ◽  
Thermokarst Lake ◽  
Water Balances ◽  
Qinghai Tibet Plateau
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