Improved parameterization of snow albedo in Noah coupled with Weather Research and Forecasting: applicability to snow estimates for the Tibetan Plateau

<p>Snow albedo is important to the land surface energy balance and to the water cycle. During snowfall and subsequent snowmelt, snow albedo is usually parameterized as functions of snow-related variables in land surface models. However, the default snow albedo scheme in the widely used Noah la...

Full description

Bibliographic Details
Main Authors: L. Liu, Y. Ma, M. Menenti, R. Su, N. Yao, W. Ma
Format: Article
Language:English
Published: Copernicus Publications 2021-09-01
Series:Hydrology and Earth System Sciences
Online Access:https://hess.copernicus.org/articles/25/4967/2021/hess-25-4967-2021.pdf
id doaj-d6e615e4a352477bbe3826fa2618c9bf
record_format Article
collection DOAJ
language English
format Article
sources DOAJ
author L. Liu
L. Liu
Y. Ma
Y. Ma
Y. Ma
Y. Ma
M. Menenti
M. Menenti
R. Su
R. Su
R. Su
N. Yao
N. Yao
N. Yao
W. Ma
W. Ma
W. Ma
W. Ma
spellingShingle L. Liu
L. Liu
Y. Ma
Y. Ma
Y. Ma
Y. Ma
M. Menenti
M. Menenti
R. Su
R. Su
R. Su
N. Yao
N. Yao
N. Yao
W. Ma
W. Ma
W. Ma
W. Ma
Improved parameterization of snow albedo in Noah coupled with Weather Research and Forecasting: applicability to snow estimates for the Tibetan Plateau
Hydrology and Earth System Sciences
author_facet L. Liu
L. Liu
Y. Ma
Y. Ma
Y. Ma
Y. Ma
M. Menenti
M. Menenti
R. Su
R. Su
R. Su
N. Yao
N. Yao
N. Yao
W. Ma
W. Ma
W. Ma
W. Ma
author_sort L. Liu
title Improved parameterization of snow albedo in Noah coupled with Weather Research and Forecasting: applicability to snow estimates for the Tibetan Plateau
title_short Improved parameterization of snow albedo in Noah coupled with Weather Research and Forecasting: applicability to snow estimates for the Tibetan Plateau
title_full Improved parameterization of snow albedo in Noah coupled with Weather Research and Forecasting: applicability to snow estimates for the Tibetan Plateau
title_fullStr Improved parameterization of snow albedo in Noah coupled with Weather Research and Forecasting: applicability to snow estimates for the Tibetan Plateau
title_full_unstemmed Improved parameterization of snow albedo in Noah coupled with Weather Research and Forecasting: applicability to snow estimates for the Tibetan Plateau
title_sort improved parameterization of snow albedo in noah coupled with weather research and forecasting: applicability to snow estimates for the tibetan plateau
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2021-09-01
description <p>Snow albedo is important to the land surface energy balance and to the water cycle. During snowfall and subsequent snowmelt, snow albedo is usually parameterized as functions of snow-related variables in land surface models. However, the default snow albedo scheme in the widely used Noah land surface model shows evident shortcomings in land–atmosphere interaction estimates during snow events on the Tibetan Plateau. Here, we demonstrate that our improved snow albedo scheme performs well after including snow depth as an additional factor. By coupling the Weather Research and Forecasting (WRF) and Noah models, this study comprehensively evaluates the performance of the improved snow albedo scheme in simulating eight snow events on the Tibetan Plateau. The modeling results are compared with WRF run with the default Noah scheme and in situ observations. The improved snow albedo scheme significantly outperforms the default Noah scheme in relation to air temperature, albedo and sensible heat flux estimates by alleviating cold bias estimates, albedo overestimates and sensible heat flux underestimates, respectively. This in turn contributes to more accurate reproductions of snow event evolution. The averaged root mean square error (RMSE) relative reductions (and relative increase in correlation coefficients) for air temperature, albedo, sensible heat flux and snow depth reach 27 % (5 %), 32 % (69 %), 13 % (17 %) and 21 % (108 %), respectively. These results demonstrate the strong potential of our improved snow albedo parameterization scheme for snow event simulations on the Tibetan Plateau. Our study provides a theoretical reference for researchers committed to further improving the snow albedo parameterization scheme.</p>
url https://hess.copernicus.org/articles/25/4967/2021/hess-25-4967-2021.pdf
work_keys_str_mv AT lliu improvedparameterizationofsnowalbedoinnoahcoupledwithweatherresearchandforecastingapplicabilitytosnowestimatesforthetibetanplateau
AT lliu improvedparameterizationofsnowalbedoinnoahcoupledwithweatherresearchandforecastingapplicabilitytosnowestimatesforthetibetanplateau
AT yma improvedparameterizationofsnowalbedoinnoahcoupledwithweatherresearchandforecastingapplicabilitytosnowestimatesforthetibetanplateau
AT yma improvedparameterizationofsnowalbedoinnoahcoupledwithweatherresearchandforecastingapplicabilitytosnowestimatesforthetibetanplateau
AT yma improvedparameterizationofsnowalbedoinnoahcoupledwithweatherresearchandforecastingapplicabilitytosnowestimatesforthetibetanplateau
AT yma improvedparameterizationofsnowalbedoinnoahcoupledwithweatherresearchandforecastingapplicabilitytosnowestimatesforthetibetanplateau
AT mmenenti improvedparameterizationofsnowalbedoinnoahcoupledwithweatherresearchandforecastingapplicabilitytosnowestimatesforthetibetanplateau
AT mmenenti improvedparameterizationofsnowalbedoinnoahcoupledwithweatherresearchandforecastingapplicabilitytosnowestimatesforthetibetanplateau
AT rsu improvedparameterizationofsnowalbedoinnoahcoupledwithweatherresearchandforecastingapplicabilitytosnowestimatesforthetibetanplateau
AT rsu improvedparameterizationofsnowalbedoinnoahcoupledwithweatherresearchandforecastingapplicabilitytosnowestimatesforthetibetanplateau
AT rsu improvedparameterizationofsnowalbedoinnoahcoupledwithweatherresearchandforecastingapplicabilitytosnowestimatesforthetibetanplateau
AT nyao improvedparameterizationofsnowalbedoinnoahcoupledwithweatherresearchandforecastingapplicabilitytosnowestimatesforthetibetanplateau
AT nyao improvedparameterizationofsnowalbedoinnoahcoupledwithweatherresearchandforecastingapplicabilitytosnowestimatesforthetibetanplateau
AT nyao improvedparameterizationofsnowalbedoinnoahcoupledwithweatherresearchandforecastingapplicabilitytosnowestimatesforthetibetanplateau
AT wma improvedparameterizationofsnowalbedoinnoahcoupledwithweatherresearchandforecastingapplicabilitytosnowestimatesforthetibetanplateau
AT wma improvedparameterizationofsnowalbedoinnoahcoupledwithweatherresearchandforecastingapplicabilitytosnowestimatesforthetibetanplateau
AT wma improvedparameterizationofsnowalbedoinnoahcoupledwithweatherresearchandforecastingapplicabilitytosnowestimatesforthetibetanplateau
AT wma improvedparameterizationofsnowalbedoinnoahcoupledwithweatherresearchandforecastingapplicabilitytosnowestimatesforthetibetanplateau
_version_ 1717758664209596416
spelling doaj-d6e615e4a352477bbe3826fa2618c9bf2021-09-10T05:52:07ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382021-09-01254967498110.5194/hess-25-4967-2021Improved parameterization of snow albedo in Noah coupled with Weather Research and Forecasting: applicability to snow estimates for the Tibetan PlateauL. Liu0L. Liu1Y. Ma2Y. Ma3Y. Ma4Y. Ma5M. Menenti6M. Menenti7R. Su8R. Su9R. Su10N. Yao11N. Yao12N. Yao13W. Ma14W. Ma15W. Ma16W. Ma17Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100101, ChinaLand–Atmosphere Interaction and its Climatic Effects Group, State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100101, ChinaKey Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100101, ChinaLand–Atmosphere Interaction and its Climatic Effects Group, State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100101, ChinaCAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing, 100101, ChinaCollege of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing, 100049, ChinaState Key Laboratory of Remote Sensing Science, Institute of Remote Sensing and Digital Earth, Chinese Academy of Sciences, Beijing, 100101, ChinaDepartment of Geoscience and Remote Sensing, Delft University of Technology, Delft, the NetherlandsKey Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100101, ChinaLand–Atmosphere Interaction and its Climatic Effects Group, State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100101, ChinaCollege of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing, 100049, ChinaKey Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100101, ChinaLand–Atmosphere Interaction and its Climatic Effects Group, State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100101, ChinaCollege of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing, 100049, ChinaKey Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100101, ChinaLand–Atmosphere Interaction and its Climatic Effects Group, State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100101, ChinaCAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing, 100101, ChinaCollege of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing, 100049, China<p>Snow albedo is important to the land surface energy balance and to the water cycle. During snowfall and subsequent snowmelt, snow albedo is usually parameterized as functions of snow-related variables in land surface models. However, the default snow albedo scheme in the widely used Noah land surface model shows evident shortcomings in land–atmosphere interaction estimates during snow events on the Tibetan Plateau. Here, we demonstrate that our improved snow albedo scheme performs well after including snow depth as an additional factor. By coupling the Weather Research and Forecasting (WRF) and Noah models, this study comprehensively evaluates the performance of the improved snow albedo scheme in simulating eight snow events on the Tibetan Plateau. The modeling results are compared with WRF run with the default Noah scheme and in situ observations. The improved snow albedo scheme significantly outperforms the default Noah scheme in relation to air temperature, albedo and sensible heat flux estimates by alleviating cold bias estimates, albedo overestimates and sensible heat flux underestimates, respectively. This in turn contributes to more accurate reproductions of snow event evolution. The averaged root mean square error (RMSE) relative reductions (and relative increase in correlation coefficients) for air temperature, albedo, sensible heat flux and snow depth reach 27 % (5 %), 32 % (69 %), 13 % (17 %) and 21 % (108 %), respectively. These results demonstrate the strong potential of our improved snow albedo parameterization scheme for snow event simulations on the Tibetan Plateau. Our study provides a theoretical reference for researchers committed to further improving the snow albedo parameterization scheme.</p>https://hess.copernicus.org/articles/25/4967/2021/hess-25-4967-2021.pdf