Intra-Seasonal and Intra-Annual Variation of the Latent Heat Flux Transfer Coefficient for a Freshwater Lake

In the case of lakes, evaporation is one of the most significant losses of water and energy. Based on high-frequency eddy-covariance (EC) measurements between May and September of 2019, the offshore heat and water vapor exchanges are evaluated for the large (~600 km<sup>2</sup>) but shal...

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Main Authors: Gabriella Lükő, Péter Torma, Tamás Weidinger
Format: Article
Language:English
Published: MDPI AG 2022-02-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/13/2/352
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author Gabriella Lükő
Péter Torma
Tamás Weidinger
author_facet Gabriella Lükő
Péter Torma
Tamás Weidinger
author_sort Gabriella Lükő
collection DOAJ
description In the case of lakes, evaporation is one of the most significant losses of water and energy. Based on high-frequency eddy-covariance (EC) measurements between May and September of 2019, the offshore heat and water vapor exchanges are evaluated for the large (~600 km<sup>2</sup>) but shallow (~3.2 m deep) Lake Balaton (Transdanubian region, Hungary). The role of local driving forces of evaporation in different time scales (from 20 min to one month) is explored, such as water surface and air temperatures, humidity, atmospheric stability, net radiation, and energy budget components. EC-derived water vapor roughness lengths and transfer coefficients (<i>C<sub>q</sub></i>) show an apparent intra-seasonal variation. Different energy balance-based evaporation estimation methods (such as the Priestley-Taylor and the Penman-Monteith) confirm this observation. Furthermore, this has suggested the existence of an intra-annual variation in these parameters. This hypothesis is verified using ten years of water balance measurements, from which, as a first step, evaporation rates and, second, transfer coefficients are derived on a monthly scale. <i>C<sub>q</sub></i> is highly reduced in winter months (~1 × 10<sup>−3</sup>) compared to summer months (~2.5 × 10<sup>−3</sup>) and strongly correlated with net radiation. The application of time-varying <i>C<sub>q</sub></i> significantly increases the accuracy of evaporation estimation when the Monin-Obukhov similarity theory-based aerodynamic method is applied. The determination coefficient increases to 0.84 compared to 0.52 when a constant <i>C<sub>q</sub></i> is employed.
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spelling doaj.art-f1bc20148f3b4ffe86cff2af9fa42ce42023-11-23T18:46:18ZengMDPI AGAtmosphere2073-44332022-02-0113235210.3390/atmos13020352Intra-Seasonal and Intra-Annual Variation of the Latent Heat Flux Transfer Coefficient for a Freshwater LakeGabriella Lükő0Péter Torma1Tamás Weidinger2Department of Hydraulic and Water Resources Engineering, Faculty of Civil Engineering, Budapest University of Technology and Economics, H-1111 Budapest, HungaryDepartment of Hydraulic and Water Resources Engineering, Faculty of Civil Engineering, Budapest University of Technology and Economics, H-1111 Budapest, HungaryDepartment of Meteorology, Institute of Geography and Geosciences, Eötvös Loránd University, H-1117 Budapest, HungaryIn the case of lakes, evaporation is one of the most significant losses of water and energy. Based on high-frequency eddy-covariance (EC) measurements between May and September of 2019, the offshore heat and water vapor exchanges are evaluated for the large (~600 km<sup>2</sup>) but shallow (~3.2 m deep) Lake Balaton (Transdanubian region, Hungary). The role of local driving forces of evaporation in different time scales (from 20 min to one month) is explored, such as water surface and air temperatures, humidity, atmospheric stability, net radiation, and energy budget components. EC-derived water vapor roughness lengths and transfer coefficients (<i>C<sub>q</sub></i>) show an apparent intra-seasonal variation. Different energy balance-based evaporation estimation methods (such as the Priestley-Taylor and the Penman-Monteith) confirm this observation. Furthermore, this has suggested the existence of an intra-annual variation in these parameters. This hypothesis is verified using ten years of water balance measurements, from which, as a first step, evaporation rates and, second, transfer coefficients are derived on a monthly scale. <i>C<sub>q</sub></i> is highly reduced in winter months (~1 × 10<sup>−3</sup>) compared to summer months (~2.5 × 10<sup>−3</sup>) and strongly correlated with net radiation. The application of time-varying <i>C<sub>q</sub></i> significantly increases the accuracy of evaporation estimation when the Monin-Obukhov similarity theory-based aerodynamic method is applied. The determination coefficient increases to 0.84 compared to 0.52 when a constant <i>C<sub>q</sub></i> is employed.https://www.mdpi.com/2073-4433/13/2/352latent heat fluxtransfer coefficienteddy-covariancelake evaporationenergy balancewater balance
spellingShingle Gabriella Lükő
Péter Torma
Tamás Weidinger
Intra-Seasonal and Intra-Annual Variation of the Latent Heat Flux Transfer Coefficient for a Freshwater Lake
Atmosphere
latent heat flux
transfer coefficient
eddy-covariance
lake evaporation
energy balance
water balance
title Intra-Seasonal and Intra-Annual Variation of the Latent Heat Flux Transfer Coefficient for a Freshwater Lake
title_full Intra-Seasonal and Intra-Annual Variation of the Latent Heat Flux Transfer Coefficient for a Freshwater Lake
title_fullStr Intra-Seasonal and Intra-Annual Variation of the Latent Heat Flux Transfer Coefficient for a Freshwater Lake
title_full_unstemmed Intra-Seasonal and Intra-Annual Variation of the Latent Heat Flux Transfer Coefficient for a Freshwater Lake
title_short Intra-Seasonal and Intra-Annual Variation of the Latent Heat Flux Transfer Coefficient for a Freshwater Lake
title_sort intra seasonal and intra annual variation of the latent heat flux transfer coefficient for a freshwater lake
topic latent heat flux
transfer coefficient
eddy-covariance
lake evaporation
energy balance
water balance
url https://www.mdpi.com/2073-4433/13/2/352
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AT tamasweidinger intraseasonalandintraannualvariationofthelatentheatfluxtransfercoefficientforafreshwaterlake