The Dynamics of Transpiration to Evapotranspiration Ratio under Wet and Dry Canopy Conditions in a Humid Boreal Forest

Humid boreal forests are unique environments characterized by a cold climate, abundant precipitation, and high evapotranspiration. Transpiration ( <math display="inline"> <semantics> <msub> <mi>E</mi> <mi>T</mi> </msub> </semantics> <...

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Bibliographic Details
Published in:Forests
Main Authors: Bram Hadiwijaya, Steeve Pepin, Pierre-Erik Isabelle, Daniel F. Nadeau
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2020
Subjects:
Online Access:https://doi.org/10.3390/f11020237
https://doaj.org/article/8a7cbc63a2b14ac988ed072d7e9e43a9
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Summary:Humid boreal forests are unique environments characterized by a cold climate, abundant precipitation, and high evapotranspiration. Transpiration ( <math display="inline"> <semantics> <msub> <mi>E</mi> <mi>T</mi> </msub> </semantics> </math> ), as a component of evapotranspiration ( E ), behaves differently under wet and dry canopy conditions, yet very few studies have focused on the dynamics of transpiration to evapotranspiration ratio ( <math display="inline"> <semantics> <mrow> <msub> <mi>E</mi> <mi>T</mi> </msub> <mo>/</mo> <mi>E</mi> </mrow> </semantics> </math> ) under transient canopy wetness states. This study presents field measurements of <math display="inline"> <semantics> <mrow> <msub> <mi>E</mi> <mi>T</mi> </msub> <mo>/</mo> <mi>E</mi> </mrow> </semantics> </math> at the Montmorency Forest, Québec, Canada: a balsam fir boreal forest that receives <math display="inline"> <semantics> <mrow> <mo>∼</mo> <mn>1600</mn> </mrow> </semantics> </math> mm of precipitation annually (continental subarctic climate; Köppen classification subtype Dfc). Half-hourly observations of E and <math display="inline"> <semantics> <msub> <mi>E</mi> <mi>T</mi> </msub> </semantics> </math> were obtained over two growing seasons using eddy-covariance and sap flow (Granier’s constant thermal dissipation) methods, respectively, under wet and dry canopy conditions. A series of calibration experiments were performed for sap flow, resulting in species-specific calibration coefficients that increased estimates of sap flux density by <math display="inline"> <semantics> <mrow> <mn>34</mn> <mo>%</mo> <mo>±</mo> ...