Recommendations for gap-filling eddy covariance latent heat flux measurements using marginal distribution sampling
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作者:
Foltynova, Lenka
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Czech Acad Sci, Global Change Res Inst, Belidla 986-4a, Brno 60300, Czech Republic
Univ Helsinki, Fac Sci, Inst Atmospher & Earth Syst Res Phys, POB 68, FIN-00014 Helsinki, FinlandCzech Acad Sci, Global Change Res Inst, Belidla 986-4a, Brno 60300, Czech Republic
Foltynova, Lenka
[1
,2
]
Fischer, Milan
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Czech Acad Sci, Global Change Res Inst, Belidla 986-4a, Brno 60300, Czech Republic
Mendel Univ Brno, Fac Agron, Dept Agrosyst & Bioclimatol, Zemedelska 1, Brno 61300, Czech RepublicCzech Acad Sci, Global Change Res Inst, Belidla 986-4a, Brno 60300, Czech Republic
Fischer, Milan
[1
,3
]
McGloin, Ryan Patrick
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Czech Acad Sci, Global Change Res Inst, Belidla 986-4a, Brno 60300, Czech RepublicCzech Acad Sci, Global Change Res Inst, Belidla 986-4a, Brno 60300, Czech Republic
McGloin, Ryan Patrick
[1
]
机构:
[1] Czech Acad Sci, Global Change Res Inst, Belidla 986-4a, Brno 60300, Czech Republic
[2] Univ Helsinki, Fac Sci, Inst Atmospher & Earth Syst Res Phys, POB 68, FIN-00014 Helsinki, Finland
[3] Mendel Univ Brno, Fac Agron, Dept Agrosyst & Bioclimatol, Zemedelska 1, Brno 61300, Czech Republic
Accurate eddy covariance (EC) measurements require that the atmospheric and orographic conditions meet certain criteria. It is common that up to 60% of the original data must be rejected. In particular, a high percentage of data is often removed during nocturnal periods. Currently, the most widely used method for filling gaps in EC datasets is the tool developed at the Max Planck Institute for Biogeochemistry [as reported by Falge et al. (2001), Reichstein et al. (2005), and Wutzler et al. (2018)]. This tool has been primarily developed and tested for the gap-filling of CO2 fluxes. In this study, we provide the first detailed testing of this gap-filling tool on LE fluxes and explore alternative settings in the gap-filling procedure using different meteorological drivers. The tests were conducted using five EC data sets. Random artificial gaps of four different gap-length scenarios were used to compare the settings. Error propagation for both the default and alternative settings was computed for various time aggregations. In general, we confirm a good performance of the standard gap-filling tool with a bias error of - 0.09 and - 0.21 W m(-2) for nocturnal growing and non-growing season cases, respectively, while daytime average bias error was 0.01 W m(-2). Alternative settings produced similar results to the default settings for diurnal cases; however, the alternative settings substantially (81%) improved the performance of night-time gap-filling. At sites where night-time LE fluxes are significant, we recommend using net radiation instead of global radiation and relative air humidity instead of vapour pressure deficit to drive the LE gap-filling.