Articles | Volume 14, issue 3
https://doi.org/10.5194/gmd-14-1753-2021
https://doi.org/10.5194/gmd-14-1753-2021
Model evaluation paper
 | 
30 Mar 2021
Model evaluation paper |  | 30 Mar 2021

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

Xiangfei Li, Tonghua Wu, Xiaodong Wu, Jie Chen, Xiaofan Zhu, Guojie Hu, Ren Li, Yongping Qiao, Cheng Yang, Junming Hao, Jie Ni, and Wensi Ma

Viewed

Total article views: 3,410 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,458 863 89 3,410 251 85 100
  • HTML: 2,458
  • PDF: 863
  • XML: 89
  • Total: 3,410
  • Supplement: 251
  • BibTeX: 85
  • EndNote: 100
Views and downloads (calculated since 30 Jun 2020)
Cumulative views and downloads (calculated since 30 Jun 2020)

Viewed (geographical distribution)

Total article views: 3,410 (including HTML, PDF, and XML) Thereof 3,157 with geography defined and 253 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 13 Dec 2024
Download
Short summary
In this study, an ensemble simulation of 55296 scheme combinations for at a typical permafrost site on the Qinghai–Tibet Plateau (QTP) was conducted. The general performance of the Noah-MP model for snow cover events (SCEs), soil temperature (ST) and soil liquid water content (SLW) was assessed, and the sensitivities of parameterization schemes at different depths were investigated. We show that Noah-MP tends to overestimate SCEs and underestimate ST and topsoil SLW on the QTP.