Articles | Volume 21, issue 1
https://doi.org/10.5194/hess-21-377-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/hess-21-377-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
24 Jan 2017
Research article |
| 24 Jan 2017
Satellite-derived light extinction coefficient and its impact on thermal structure simulations in a 1-D lake model
Kiana Zolfaghari
CORRESPONDING AUTHOR
Interdisciplinary Centre on Climate Change and Department of Geography
& Environmental Management, University of Waterloo, Waterloo, Canada
Claude R. Duguay
Interdisciplinary Centre on Climate Change and Department of Geography
& Environmental Management, University of Waterloo, Waterloo, Canada
Homa Kheyrollah Pour
Interdisciplinary Centre on Climate Change and Department of Geography
& Environmental Management, University of Waterloo, Waterloo, Canada
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Cited
16 citations as recorded by crossref.
- Modeling subgrid lake energy balance in ORCHIDEE terrestrial scheme using the FLake lake model A. Bernus & C. Ottlé 10.5194/gmd-15-4275-2022
- Prediction of Photochemically Produced Reactive Intermediates in Surface Waters via Satellite Remote Sensing Y. Chen et al. 10.1021/acs.est.0c00344
- Deterministic modelling of freshwater lakes and reservoirs: Current trends and recent progress L. Soares & M. Calijuri 10.1016/j.envsoft.2021.105143
- How does lake water clarity affect lake thermal processes? Q. Zhang & X. Ma 10.1016/j.heliyon.2022.e10359
- Improvements and Evaluation of the FLake Model in Dagze Co, Central Tibetan Plateau B. Cao et al. 10.3390/w15173135
- Using automatic calibration to improve the physics behind complex numerical models: an example from a 3D lake model using Delft3D (v6.02.10) and DYNO-PODS (v1.0) M. Amadori et al. 10.5194/gmd-18-3473-2025
- Simulation of the Surface Energy Flux and Thermal Stratification of Lake Taihu with Three 1-D Models Y. Wang et al. 10.3390/w11051026
- Effects of the Largest Lake of the Tibetan Plateau on the Regional Climate D. Su et al. 10.1029/2020JD033396
- Mechanisms and effects of under-ice warming water in Ngoring Lake of Qinghai–Tibet Plateau M. Wang et al. 10.5194/tc-16-3635-2022
- Improvement and Evaluation of the Latest Version of WRF-Lake at a Deep Riverine Reservoir S. Guo et al. 10.1007/s00376-022-2180-5
- Study of freeze-thaw cycle and key radiation transfer parameters in a Tibetan Plateau lake using LAKE2.0 model and field observations Z. Li et al. 10.1017/jog.2020.87
- Numerical simulation of thermal stratification in Lake Qiandaohu using an improved WRF-Lake model X. Wang et al. 10.1016/j.jhydrol.2023.129184
- Evaluation of the WRF-Lake Model in the Large Dimictic Reservoir: Comparisons with Field Data and Another Water Temperature Model S. Guo et al. 10.1175/JHM-D-21-0220.1
- Validation and Sensitivity Analysis of a 1‐D Lake Model Across Global Lakes M. Guo et al. 10.1029/2020JD033417
- Satellite-derived light extinction coefficient and its impact on thermal structure simulations in a 1-D lake model K. Zolfaghari et al. 10.5194/hess-21-377-2017
- Airlake boundary layer and performance of a simple lake parameterization scheme over the Tibetan highlands L. Wen et al. 10.3402/tellusa.v68.31091
14 citations as recorded by crossref.
- Modeling subgrid lake energy balance in ORCHIDEE terrestrial scheme using the FLake lake model A. Bernus & C. Ottlé 10.5194/gmd-15-4275-2022
- Prediction of Photochemically Produced Reactive Intermediates in Surface Waters via Satellite Remote Sensing Y. Chen et al. 10.1021/acs.est.0c00344
- Deterministic modelling of freshwater lakes and reservoirs: Current trends and recent progress L. Soares & M. Calijuri 10.1016/j.envsoft.2021.105143
- How does lake water clarity affect lake thermal processes? Q. Zhang & X. Ma 10.1016/j.heliyon.2022.e10359
- Improvements and Evaluation of the FLake Model in Dagze Co, Central Tibetan Plateau B. Cao et al. 10.3390/w15173135
- Using automatic calibration to improve the physics behind complex numerical models: an example from a 3D lake model using Delft3D (v6.02.10) and DYNO-PODS (v1.0) M. Amadori et al. 10.5194/gmd-18-3473-2025
- Simulation of the Surface Energy Flux and Thermal Stratification of Lake Taihu with Three 1-D Models Y. Wang et al. 10.3390/w11051026
- Effects of the Largest Lake of the Tibetan Plateau on the Regional Climate D. Su et al. 10.1029/2020JD033396
- Mechanisms and effects of under-ice warming water in Ngoring Lake of Qinghai–Tibet Plateau M. Wang et al. 10.5194/tc-16-3635-2022
- Improvement and Evaluation of the Latest Version of WRF-Lake at a Deep Riverine Reservoir S. Guo et al. 10.1007/s00376-022-2180-5
- Study of freeze-thaw cycle and key radiation transfer parameters in a Tibetan Plateau lake using LAKE2.0 model and field observations Z. Li et al. 10.1017/jog.2020.87
- Numerical simulation of thermal stratification in Lake Qiandaohu using an improved WRF-Lake model X. Wang et al. 10.1016/j.jhydrol.2023.129184
- Evaluation of the WRF-Lake Model in the Large Dimictic Reservoir: Comparisons with Field Data and Another Water Temperature Model S. Guo et al. 10.1175/JHM-D-21-0220.1
- Validation and Sensitivity Analysis of a 1‐D Lake Model Across Global Lakes M. Guo et al. 10.1029/2020JD033417
2 citations as recorded by crossref.
- Satellite-derived light extinction coefficient and its impact on thermal structure simulations in a 1-D lake model K. Zolfaghari et al. 10.5194/hess-21-377-2017
- Airlake boundary layer and performance of a simple lake parameterization scheme over the Tibetan highlands L. Wen et al. 10.3402/tellusa.v68.31091
Saved (preprint)
Latest update: 30 Jun 2025
Short summary
A remotely-sensed water clarity value (Kd) was applied to improve FLake model simulations of Lake Erie thermal structure using a time-invariant (constant) annual value as well as monthly values of Kd. The sensitivity of FLake model to Kd values was studied. It was shown that the model is very sensitive to variations in Kd when the value is less than 0.5 m-1.
A remotely-sensed water clarity value (Kd) was applied to improve FLake model simulations of...
