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作 者:Yamei SHAO Huizhi LIU Qun DU Yang LIU Jihua SUN Yaohui LI Jinlian LI
机构地区:[1]State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029,China [2]University of Chinese Academy of Sciences,Beijing 100029,China [3]Yunnan Meteorological Observatory,Kunming 530100,China [4]College of Aviation Meteorology,Civil Aviation Flight University of China,Guanghan 618307,China [5]Meteorological Bureau of Tengchong County,Baoshan 679100,China
出 处:《Advances in Atmospheric Sciences》2024年第2期355-368,共14页大气科学进展(英文版)
基 金:funded by the National Natural Science Foundation of China (Grant No. 91937301);the Second Tibetan Plateau Scientific Expedition and Research (STEP) program (Grant No. 2019QZKK0105);the National Natural Science Foundation of China (Grant Nos. 41975017, 41905010)。
摘 要:Based on eddy covariance(EC) measurements during 2016–20, the effects of sky conditions on the net ecosystem productivity(NEP) over a subtropical “floating blanket ” wetland were investigated. Sky conditions were divided into overcast, cloudy, and sunny conditions. On the half-hourly timescale, the daytime NEP responded more rapidly to the changes in the total photosynthetic active radiation(PARt) under overcast and cloudy skies than that under sunny skies. The increase in the apparent quantum yield under overcast and cloudy conditions was the greatest in spring and the least in summer. Additionally, lower atmospheric vapor pressure deficit(VPD) and moderate air temperature were more conducive to enhancing the apparent quantum yield under cloudy skies. On the daily timescale, NEP and the gross primary production(GPP) were higher under cloudy or sunny conditions than those under overcast conditions across seasons. The daily NEP and GPP during the wet season peaked under cloudy skies. The daily ecosystem light use efficiency(LUE) and water use efficiency(WUE) during the wet season also changed with sky conditions and reached their maximum under overcast and cloudy skies, respectively. The diffuse photosynthetic active radiation(PAR_d) and air temperature were primarily responsible for the variation of daily NEP from half-hourly to monthly timescales, and the direct photosynthetic active radiation(PAR_b) had a secondary effect on NEP. Under sunny conditions, PAR_b and air temperature were the dominant factors controlling daily NEP. While daily NEP was mainly controlled by PAR_d under cloudy and overcast conditions.
关 键 词:diffuse radiation eddy covariance NEP controlling factors WETLAND path analysis
分 类 号:P412[天文地球—大气科学及气象学]
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