Canopy Resistance and Estimation of Evapotranspiration above a Humid Cypress Forest

This study presented a two-year data set of sensible heat and water vapor fluxes above a humid subtropical montane Cypress forest, located at 1650 m a.s.l. in northeastern Taiwan. The focuses of this study were to investigate (1) the diurnal and seasonal variations of canopy resistance and fluxes of...

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Main Authors: Bau-Show Lin, Huimin Lei, Ming-Che Hu, Supattra Visessri, Cheng-I Hsieh
Format: Article
Language:English
Published: Wiley 2020-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2020/4232138
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author Bau-Show Lin
Huimin Lei
Ming-Che Hu
Supattra Visessri
Cheng-I Hsieh
author_facet Bau-Show Lin
Huimin Lei
Ming-Che Hu
Supattra Visessri
Cheng-I Hsieh
author_sort Bau-Show Lin
collection DOAJ
description This study presented a two-year data set of sensible heat and water vapor fluxes above a humid subtropical montane Cypress forest, located at 1650 m a.s.l. in northeastern Taiwan. The focuses of this study were to investigate (1) the diurnal and seasonal variations of canopy resistance and fluxes of sensible heat and water vapor above this forest; and (2) the mechanism of why a fixed canopy resistance could work when implementing the Penman–Monteith equation for diurnal hourly evapotranspiration estimation. Our results showed distinct seasonal variations in canopy resistance and water vapor flux, but on the contrary, the sensible heat flux did not change as much as the water vapor flux did with seasons. The seasonal variation patterns of the canopy resistance and water vapor flux were highly coupled with the meteorological factors. Also, the results demonstrated that a constant (fixed) canopy resistance was good enough for estimating the diurnal variation of evapotranspiration using Penman–Monteith equation. We observed a canopy resistance around 190 (s/m) for both the two warm seasons; and canopy resistances were around 670 and 320 (s/m) for the two cool seasons, respectively. In addition, our analytical analyses demonstrated that when the average canopy resistance is higher than 200 (s/m), the Penman–Monteith equation is less sensitive to the change of canopy resistance; hence, a fixed canopy resistance is suitable for the diurnal hourly evapotranspiration estimation. However, this is not the case when the average canopy resistance is less than 100 (s/m), and variable canopy resistances are needed. These two constraints (200 and 100) were obtained based on purely analytical analyses under a moderate meteorological condition (Rn = 600 W·m−2, RH = 60%, Ta = 20°C, U = 2 m·s−1) and a measurement height around two times of the canopy height.
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issn 1687-9309
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publishDate 2020-01-01
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spelling doaj-art-0dbb024cefbd4723ad4c729f3f9be8592025-08-20T03:54:24ZengWileyAdvances in Meteorology1687-93091687-93172020-01-01202010.1155/2020/42321384232138Canopy Resistance and Estimation of Evapotranspiration above a Humid Cypress ForestBau-Show Lin0Huimin Lei1Ming-Che Hu2Supattra Visessri3Cheng-I Hsieh4Department of Horticulture and Landscape Architecture, National Taiwan University, Taipei 10617, TaiwanDepartment of Hydraulic Engineering, Tsinghua University, Beijing 100084, ChinaDepartment of Bioenvironmental Systems Engineering, National Taiwan University, Taipei 10617, TaiwanDepartment of Water Resources Engineering, Chulalongkorn University, Bangkok 10330, ThailandDepartment of Bioenvironmental Systems Engineering, National Taiwan University, Taipei 10617, TaiwanThis study presented a two-year data set of sensible heat and water vapor fluxes above a humid subtropical montane Cypress forest, located at 1650 m a.s.l. in northeastern Taiwan. The focuses of this study were to investigate (1) the diurnal and seasonal variations of canopy resistance and fluxes of sensible heat and water vapor above this forest; and (2) the mechanism of why a fixed canopy resistance could work when implementing the Penman–Monteith equation for diurnal hourly evapotranspiration estimation. Our results showed distinct seasonal variations in canopy resistance and water vapor flux, but on the contrary, the sensible heat flux did not change as much as the water vapor flux did with seasons. The seasonal variation patterns of the canopy resistance and water vapor flux were highly coupled with the meteorological factors. Also, the results demonstrated that a constant (fixed) canopy resistance was good enough for estimating the diurnal variation of evapotranspiration using Penman–Monteith equation. We observed a canopy resistance around 190 (s/m) for both the two warm seasons; and canopy resistances were around 670 and 320 (s/m) for the two cool seasons, respectively. In addition, our analytical analyses demonstrated that when the average canopy resistance is higher than 200 (s/m), the Penman–Monteith equation is less sensitive to the change of canopy resistance; hence, a fixed canopy resistance is suitable for the diurnal hourly evapotranspiration estimation. However, this is not the case when the average canopy resistance is less than 100 (s/m), and variable canopy resistances are needed. These two constraints (200 and 100) were obtained based on purely analytical analyses under a moderate meteorological condition (Rn = 600 W·m−2, RH = 60%, Ta = 20°C, U = 2 m·s−1) and a measurement height around two times of the canopy height.http://dx.doi.org/10.1155/2020/4232138
spellingShingle Bau-Show Lin
Huimin Lei
Ming-Che Hu
Supattra Visessri
Cheng-I Hsieh
Canopy Resistance and Estimation of Evapotranspiration above a Humid Cypress Forest
Advances in Meteorology
title Canopy Resistance and Estimation of Evapotranspiration above a Humid Cypress Forest
title_full Canopy Resistance and Estimation of Evapotranspiration above a Humid Cypress Forest
title_fullStr Canopy Resistance and Estimation of Evapotranspiration above a Humid Cypress Forest
title_full_unstemmed Canopy Resistance and Estimation of Evapotranspiration above a Humid Cypress Forest
title_short Canopy Resistance and Estimation of Evapotranspiration above a Humid Cypress Forest
title_sort canopy resistance and estimation of evapotranspiration above a humid cypress forest
url http://dx.doi.org/10.1155/2020/4232138
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AT supattravisessri canopyresistanceandestimationofevapotranspirationaboveahumidcypressforest
AT chengihsieh canopyresistanceandestimationofevapotranspirationaboveahumidcypressforest