Articles | Volume 12, issue 9
https://doi.org/10.5194/tc-12-3067-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-12-3067-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
27 Sep 2018
Research article |
| 27 Sep 2018
| 27 Sep 2018
The physical properties of coarse-fragment soils and their effects on permafrost dynamics: a case study on the central Qinghai–Tibetan Plateau
Shuhua Yi
School of Geographic Sciences, Nantong University, 999 Tongjing Road, Nantong, 226007, China
State Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment
and Resources, Chinese Academy of Sciences, 320 Donggang West Road, 730000, Lanzhou, Gansu, China
Yujie He
Chinese Research Academy of Environmental Sciences, No.8 Dayangfang, Chaoyang District, 100012, Beijing, China
Xinlei Guo
Department of Ecosystem and Landscape Dynamics, Institute for Biodiversity and
Ecosystem Dynamics, University of Amsterdam, Science Park 904, 1098 XH Amsterdam, The Netherlands
Jianjun Chen
College of Geomatics and Geoinformation, Guilin University of Technology, 12 Jiangan Road, Guilin, 541004, China
Guangxi Key Laboratory of Spatial Information and Geomatics, 12 Jiangan Road, Guilin, 541004, China
Qingbai Wu
State Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment
and Resources, Chinese Academy of Sciences, 320 Donggang West Road, 730000, Lanzhou, Gansu, China
Yu Qin
State Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment
and Resources, Chinese Academy of Sciences, 320 Donggang West Road, 730000, Lanzhou, Gansu, China
Yongjian Ding
CORRESPONDING AUTHOR
State Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment
and Resources, Chinese Academy of Sciences, 320 Donggang West Road, 730000, Lanzhou, Gansu, China
Key Laboratory of Ecohydrology of Inland River Basin, Chinese Academy of Sciences, Lanzhou 730000, China
University of Chinese Academy Sciences, Beijing, 100049, China
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Cited
17 citations as recorded by crossref.
- Sensitivity of soil freeze/thaw dynamics to environmental conditions at different spatial scales in the central Tibetan Plateau H. Jiang et al. 10.1016/j.scitotenv.2020.139261
- Evaluation of soil thermal conductivity schemes incorporated into CLM5.0 in permafrost regions on the Tibetan Plateau S. Yang et al. 10.1016/j.geoderma.2021.115330
- Progress and Challenges in Studying Regional Permafrost in the Tibetan Plateau Using Satellite Remote Sensing and Models H. Jiang et al. 10.3389/feart.2020.560403
- Evaluation of the Performance of CLM5.0 in Soil Hydrothermal Dynamics in Permafrost Regions on the Qinghai–Tibet Plateau S. Yang et al. 10.3390/rs14246228
- Last-decade progress in understanding and modeling the land surface processes on the Tibetan Plateau H. Lu et al. 10.5194/hess-24-5745-2020
- Soil Physical, Hydraulic, and Thermal Properties in Interior Alaska, USA: Implications for Hydrologic Response to Thawing Permafrost Conditions B. Ebel et al. 10.1029/2018WR023673
- Water and heat coupling processes and its simulation in frozen soils: Current status and future research directions G. Hu et al. 10.1016/j.catena.2022.106844
- Physical and Thermal Properties of Coarse-Fragment Soil in the Moraine-Talus Zone of the Qilian Mountains X. Wang et al. 10.3390/su15021183
- Improving the Noah‐MP Model for Simulating Hydrothermal Regime of the Active Layer in the Permafrost Regions of the Qinghai‐Tibet Plateau X. Li et al. 10.1029/2020JD032588
- Characteristics of Freeze–Thaw Cycles in an Endorheic Basin on the Qinghai-Tibet Plateau Based on SBAS-InSAR Technology H. Zhou et al. 10.3390/rs14133168
- Implications of elevation-dependent warming to water resources over the Chinese Qilian Mountains P. Zhao et al. 10.2166/wcc.2022.391
- Detecting Permafrost in Plateau and Mountainous Areas by Airborne Transient Electromagnetic Sensing B. Su et al. 10.3390/electronics9081229
- Evaluation of CLM5.0 for simulating surface energy budget and soil hydrothermal regime in permafrost regions of the Qinghai-Tibet Plateau J. Ma et al. 10.1016/j.agrformet.2023.109380
- Simulating the thermal regime of a railway embankment structure on the Tibetan Plateau under climate change R. Chen et al. 10.1016/j.coldregions.2023.103881
- Synergetic variations of active layer soil water and salt in a permafrost-affected meadow in the headwater area of the Yellow River, northeastern Qinghai–Tibet plateau Q. Wang et al. 10.1016/j.iswcr.2021.08.004
- Effects of Patchiness on Surface Soil Moisture of Alpine Meadow on the Northeastern Qinghai-Tibetan Plateau: Implications for Grassland Restoration W. Zhang et al. 10.3390/rs12244121
- Spatiotemporally heterogeneous soil thermohydraulic processes in the frozen soil of the Tibetan Plateau L. Cuo et al. 10.1016/j.geoderma.2023.116634
17 citations as recorded by crossref.
- Sensitivity of soil freeze/thaw dynamics to environmental conditions at different spatial scales in the central Tibetan Plateau H. Jiang et al. 10.1016/j.scitotenv.2020.139261
- Evaluation of soil thermal conductivity schemes incorporated into CLM5.0 in permafrost regions on the Tibetan Plateau S. Yang et al. 10.1016/j.geoderma.2021.115330
- Progress and Challenges in Studying Regional Permafrost in the Tibetan Plateau Using Satellite Remote Sensing and Models H. Jiang et al. 10.3389/feart.2020.560403
- Evaluation of the Performance of CLM5.0 in Soil Hydrothermal Dynamics in Permafrost Regions on the Qinghai–Tibet Plateau S. Yang et al. 10.3390/rs14246228
- Last-decade progress in understanding and modeling the land surface processes on the Tibetan Plateau H. Lu et al. 10.5194/hess-24-5745-2020
- Soil Physical, Hydraulic, and Thermal Properties in Interior Alaska, USA: Implications for Hydrologic Response to Thawing Permafrost Conditions B. Ebel et al. 10.1029/2018WR023673
- Water and heat coupling processes and its simulation in frozen soils: Current status and future research directions G. Hu et al. 10.1016/j.catena.2022.106844
- Physical and Thermal Properties of Coarse-Fragment Soil in the Moraine-Talus Zone of the Qilian Mountains X. Wang et al. 10.3390/su15021183
- Improving the Noah‐MP Model for Simulating Hydrothermal Regime of the Active Layer in the Permafrost Regions of the Qinghai‐Tibet Plateau X. Li et al. 10.1029/2020JD032588
- Characteristics of Freeze–Thaw Cycles in an Endorheic Basin on the Qinghai-Tibet Plateau Based on SBAS-InSAR Technology H. Zhou et al. 10.3390/rs14133168
- Implications of elevation-dependent warming to water resources over the Chinese Qilian Mountains P. Zhao et al. 10.2166/wcc.2022.391
- Detecting Permafrost in Plateau and Mountainous Areas by Airborne Transient Electromagnetic Sensing B. Su et al. 10.3390/electronics9081229
- Evaluation of CLM5.0 for simulating surface energy budget and soil hydrothermal regime in permafrost regions of the Qinghai-Tibet Plateau J. Ma et al. 10.1016/j.agrformet.2023.109380
- Simulating the thermal regime of a railway embankment structure on the Tibetan Plateau under climate change R. Chen et al. 10.1016/j.coldregions.2023.103881
- Synergetic variations of active layer soil water and salt in a permafrost-affected meadow in the headwater area of the Yellow River, northeastern Qinghai–Tibet plateau Q. Wang et al. 10.1016/j.iswcr.2021.08.004
- Effects of Patchiness on Surface Soil Moisture of Alpine Meadow on the Northeastern Qinghai-Tibetan Plateau: Implications for Grassland Restoration W. Zhang et al. 10.3390/rs12244121
- Spatiotemporally heterogeneous soil thermohydraulic processes in the frozen soil of the Tibetan Plateau L. Cuo et al. 10.1016/j.geoderma.2023.116634
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Short summary
Coarse-fragment soil on the Qinghai–Tibetan Plateau has different thermal and hydrological properties to soils commonly used in modeling studies. We took soil samples and measured their physical properties in a laboratory, which were used in a model to simulate their effects on permafrost dynamics. Model errors were reduced using the measured properties, in which porosity played an dominant role.
Coarse-fragment soil on the Qinghai–Tibetan Plateau has different thermal and hydrological...
