Articles | Volume 23, issue 4
https://doi.org/10.5194/hess-23-2173-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-23-2173-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Modeling experiments on seasonal lake ice mass and energy balance in the Qinghai–Tibet Plateau: a case study
Key Laboratory of Subsurface Hydrology and Ecological Effects in
Arid Region (the Ministry of Education), Chang'an University, Xi'an 710054,
China
School of Environmental Science and Engineering, Chang'an
University, Xi'an 710054, China
Bin Cheng
Finnish Meteorological Institute, Helsinki, Finland
Jinrong Zhang
Key Laboratory of Subsurface Hydrology and Ecological Effects in
Arid Region (the Ministry of Education), Chang'an University, Xi'an 710054,
China
School of Environmental Science and Engineering, Chang'an
University, Xi'an 710054, China
Zheng Zhang
Key Laboratory of Subsurface Hydrology and Ecological Effects in
Arid Region (the Ministry of Education), Chang'an University, Xi'an 710054,
China
School of Environmental Science and Engineering, Chang'an
University, Xi'an 710054, China
Timo Vihma
Finnish Meteorological Institute, Helsinki, Finland
Zhijun Li
State Key Laboratory of Coastal and Offshore Engineering, Dalian
University of Technology, Dalian 116024, China
State Key Laboratory of Frozen Soil Engineering, Northwest
Institute of Eco-Environment and Resources, Chinese Academy of Sciences,
Lanzhou 730000, China
Fujun Niu
State Key Laboratory of Frozen Soil Engineering, Northwest
Institute of Eco-Environment and Resources, Chinese Academy of Sciences,
Lanzhou 730000, China
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26 citations as recorded by crossref.
- Contrasting hydrological and thermal intensities determine seasonal lake-level variations – a case study at Paiku Co on the southern Tibetan Plateau Y. Lei et al. 10.5194/hess-25-3163-2021
- Quantifying the evaporation amounts of 75 high-elevation large dimictic lakes on the Tibetan Plateau B. Wang et al. 10.1126/sciadv.aay8558
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- Air/snow, snow/ice and ice/water interfaces detection from high-resolution vertical temperature profiles measured by ice mass-balance buoys on an Arctic lake Y. Cheng et al. 10.1017/aog.2020.51
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- Inter-annual variation in lake ice composition in the European Arctic: observations based on high-resolution thermistor strings B. Cheng et al. 10.5194/essd-13-3967-2021
- Effect of climate warming on a change in thermal and ice conditions in the largest lake in Poland – Lake Śniardwy M. Ptak et al. 10.2478/johh-2020-0024
- Mass and Heat Balance of a Lake Ice Cover in the Central Asian Arid Climate Zone P. Lu et al. 10.3390/w12102888
- Retention time of lakes in the Larsemann Hills oasis, East Antarctica E. Shevnina et al. 10.5194/tc-15-2667-2021
- Autonomous System for Lake Ice Monitoring I. Aslamov et al. 10.3390/s21248505
- Under‐Ice Dissolved Oxygen and Metabolism Dynamics in a Shallow Lake: The Critical Role of Ice and Snow W. Huang et al. 10.1029/2020WR027990
- Sunlight penetration dominates the thermal regime and energetics of a shallow ice-covered lake in arid climate W. Huang et al. 10.5194/tc-16-1793-2022
- Critical Role of Groundwater Inflow in Sustaining Lake Water Balance on the Western Tibetan Plateau Y. Lei et al. 10.1029/2022GL099268
- Differential Heating Drives Downslope Flows that Accelerate Mixed‐Layer Warming in Ice‐Covered Waters H. Ulloa et al. 10.1029/2019GL085258
- Lake Ice Simulation and Evaluation for a Typical Lake on the Tibetan Plateau Y. Si et al. 10.3390/w15173088
- Fine-scale monitoring of lake ice phenology by synthesizing remote sensed and climatologic features based on high-resolution satellite constellation and modeling J. Tong et al. 10.1016/j.scitotenv.2023.169002
- Thermal structure and water-ice heat transfer in a shallow ice-covered thermokarst lake in central Qinghai-Tibet Plateau W. Huang et al. 10.1016/j.jhydrol.2019.124122
- A floating remote observation system (FROS) for full seasonal lake ice evolution studies F. Xie et al. 10.1016/j.coldregions.2022.103557
- What caused the spatial heterogeneity of lake ice phenology changes on the Tibetan Plateau? Y. Cai et al. 10.1016/j.scitotenv.2022.155517
- Seasonal change in heat flux at the water-bottom sediment boundary in a small lake G. Zdorovennova et al. 10.1088/1742-6596/2131/3/032080
- Spatiotemporal variation of surface albedo and its influencing factors in northern Xinjiang, China S. Yuan et al. 10.1007/s40333-023-0069-5
- Ice Phenology in Eurasian Lakes over Spatial Location and Altitude M. Leppäranta & L. Wen 10.3390/w14071037
- Energetics of Radiatively Heated Ice‐Covered Lakes K. Winters et al. 10.1029/2019GL084182
- Solar radiation transfer for an ice-covered lake in the central Asian arid climate zone X. Cao et al. 10.1080/20442041.2020.1790274
- Overview: Recent advances in the understanding of the northern Eurasian environments and of the urban air quality in China – a Pan-Eurasian Experiment (PEEX) programme perspective H. Lappalainen et al. 10.5194/acp-22-4413-2022
- Understanding two key processes associated with alpine lake ice phenology using a coupled atmosphere-lake model X. Zhou et al. 10.1016/j.ejrh.2023.101334
Latest update: 14 Dec 2024
Short summary
Up to now, little has been known on ice thermodynamics and lake–atmosphere interaction over the Tibetan Plateau during ice-covered seasons due to a lack of field data. Here, model experiments on ice thermodynamics were conducted in a shallow lake using HIGHTSI. Water–ice heat flux was a major source of uncertainty for lake ice thickness. Heat and mass budgets were estimated within the vertical air–ice–water system. Strong ice sublimation occurred and was responsible for water loss during winter.
Up to now, little has been known on ice thermodynamics and lake–atmosphere interaction over the...