Analysis of the Radiation Fluxes over Complex Surfaces on the Tibetan Plateau

Analysis of long-term, ground-based observation data on the Tibetan Plateau help to enhance our understanding of land-atmosphere interactions and their influence on weather and climate in this region. In this paper, the daily, monthly, and annual averages of radiative fluxes, surface albedo, surface...

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Autores principales: Chunxiao Wang, Yaoming Ma, Binbin Wang, Weiqiang Ma, Xuelong Chen, Cunbo Han
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Publicado: MDPI AG 2021
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Acceso en línea:https://doaj.org/article/6de6288f81954c909aa48bfbebf9a1ce
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spelling oai:doaj.org-article:6de6288f81954c909aa48bfbebf9a1ce2021-11-11T19:56:49ZAnalysis of the Radiation Fluxes over Complex Surfaces on the Tibetan Plateau10.3390/w132130842073-4441https://doaj.org/article/6de6288f81954c909aa48bfbebf9a1ce2021-11-01T00:00:00Zhttps://www.mdpi.com/2073-4441/13/21/3084https://doaj.org/toc/2073-4441Analysis of long-term, ground-based observation data on the Tibetan Plateau help to enhance our understanding of land-atmosphere interactions and their influence on weather and climate in this region. In this paper, the daily, monthly, and annual averages of radiative fluxes, surface albedo, surface temperature, and air temperature were calculated for the period of 2006 to 2019 at six research stations on the Tibetan Plateau. The surface energy balance characteristics of these six stations, which include alpine meadow, alpine desert, and alpine steppe, were then compared. The downward shortwave radiation at stations BJ, QOMS, and NAMORS was found to decrease during the study period, due to increasing cloudiness. Meanwhile, the upward shortwave radiation and surface albedo at all stations were found to have decreased overall. Downward longwave radiation, upward longwave radiation, net radiation, surface temperature, and air temperature showed increasing trends on inter-annual time scales at most stations. Downward shortwave radiation was maximum in spring at BJ, QOMS, NADORS, and NAMORS, due to the influence of the summer monsoon. Upward shortwave radiation peaked in October and November due to the greater snow cover. BJ, QOMS, NADORS, and NAMORS showed strong sensible heat fluxes in the spring while MAWORS showed strong sensible heat fluxes in the summer. The monthly and diurnal variations of surface albedo at each station were “U” shaped. The diurnal variability of downward longwave radiation at each station was small, ranging from 220 to 295 W·m<sup>−2</sup>.The diurnal variation in surface temperature at each station slightly lagged behind changes in downward shortwave radiation, and the air temperature, in turn, slightly lagged behind the surface temperature.Chunxiao WangYaoming MaBinbin WangWeiqiang MaXuelong ChenCunbo HanMDPI AGarticleTibetan Plateausurface characteristic parameterradiation fluxesobservation dataland-atmosphere interactionHydraulic engineeringTC1-978Water supply for domestic and industrial purposesTD201-500ENWater, Vol 13, Iss 3084, p 3084 (2021)
institution DOAJ
collection DOAJ
language EN
topic Tibetan Plateau
surface characteristic parameter
radiation fluxes
observation data
land-atmosphere interaction
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
spellingShingle Tibetan Plateau
surface characteristic parameter
radiation fluxes
observation data
land-atmosphere interaction
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
Chunxiao Wang
Yaoming Ma
Binbin Wang
Weiqiang Ma
Xuelong Chen
Cunbo Han
Analysis of the Radiation Fluxes over Complex Surfaces on the Tibetan Plateau
description Analysis of long-term, ground-based observation data on the Tibetan Plateau help to enhance our understanding of land-atmosphere interactions and their influence on weather and climate in this region. In this paper, the daily, monthly, and annual averages of radiative fluxes, surface albedo, surface temperature, and air temperature were calculated for the period of 2006 to 2019 at six research stations on the Tibetan Plateau. The surface energy balance characteristics of these six stations, which include alpine meadow, alpine desert, and alpine steppe, were then compared. The downward shortwave radiation at stations BJ, QOMS, and NAMORS was found to decrease during the study period, due to increasing cloudiness. Meanwhile, the upward shortwave radiation and surface albedo at all stations were found to have decreased overall. Downward longwave radiation, upward longwave radiation, net radiation, surface temperature, and air temperature showed increasing trends on inter-annual time scales at most stations. Downward shortwave radiation was maximum in spring at BJ, QOMS, NADORS, and NAMORS, due to the influence of the summer monsoon. Upward shortwave radiation peaked in October and November due to the greater snow cover. BJ, QOMS, NADORS, and NAMORS showed strong sensible heat fluxes in the spring while MAWORS showed strong sensible heat fluxes in the summer. The monthly and diurnal variations of surface albedo at each station were “U” shaped. The diurnal variability of downward longwave radiation at each station was small, ranging from 220 to 295 W·m<sup>−2</sup>.The diurnal variation in surface temperature at each station slightly lagged behind changes in downward shortwave radiation, and the air temperature, in turn, slightly lagged behind the surface temperature.
format article
author Chunxiao Wang
Yaoming Ma
Binbin Wang
Weiqiang Ma
Xuelong Chen
Cunbo Han
author_facet Chunxiao Wang
Yaoming Ma
Binbin Wang
Weiqiang Ma
Xuelong Chen
Cunbo Han
author_sort Chunxiao Wang
title Analysis of the Radiation Fluxes over Complex Surfaces on the Tibetan Plateau
title_short Analysis of the Radiation Fluxes over Complex Surfaces on the Tibetan Plateau
title_full Analysis of the Radiation Fluxes over Complex Surfaces on the Tibetan Plateau
title_fullStr Analysis of the Radiation Fluxes over Complex Surfaces on the Tibetan Plateau
title_full_unstemmed Analysis of the Radiation Fluxes over Complex Surfaces on the Tibetan Plateau
title_sort analysis of the radiation fluxes over complex surfaces on the tibetan plateau
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/6de6288f81954c909aa48bfbebf9a1ce
work_keys_str_mv AT chunxiaowang analysisoftheradiationfluxesovercomplexsurfacesonthetibetanplateau
AT yaomingma analysisoftheradiationfluxesovercomplexsurfacesonthetibetanplateau
AT binbinwang analysisoftheradiationfluxesovercomplexsurfacesonthetibetanplateau
AT weiqiangma analysisoftheradiationfluxesovercomplexsurfacesonthetibetanplateau
AT xuelongchen analysisoftheradiationfluxesovercomplexsurfacesonthetibetanplateau
AT cunbohan analysisoftheradiationfluxesovercomplexsurfacesonthetibetanplateau
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