The biophysical climate mitigation potential of boreal peatlands during the growing season

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Helbig , M , Waddington , J M , Alekseychik , P , Amiro , B , Aurela , M , Barr , A G , Black , T A , Carey , S K , Chen , J , Chi , J , Desai , A R , Dunn , A , Euskirchen , E S , Flanagan , L B , Friborg , T , Garneau , M , Grelle , A , Harder , S , Heliasz , M , Humphreys , E R , Ikawa , H , Isabelle , P-E , Iwata , H , Jassal , R , Korkiakoski , M , Kurbatova , J , Kutzbach , L , Lapshina , E , Lindroth , A , Lofvenius , M O , Lohila , A , Mammarella , I , Marsh , P , Moore , P A , Maximov , T , Nadeau , D F , Nicholls , E M , Nilsson , M B , Ohta , T , Peichl , M , Petrone , R M , Prokushkin , A , Quinton , W L , Roulet , N , Runkle , B R K , Sonnentag , O , Strachan , I B , Taillardat , P , Tuittila , E-S , Tuovinen , J-P , Turner , J , Ueyama , M , Varlagin , A , Vesala , T , Wilmking , M , Zyrianov , V & Schulze , C 2020 , ' The biophysical climate mitigation potential of boreal peatlands during the growing season ' , Environmental Research Letters , vol. 15 , no. 10 , 104004 . https://doi.org/10.1088/1748-9326/abab34

Title: The biophysical climate mitigation potential of boreal peatlands during the growing season
Author: Helbig, Manuel; Waddington, James M.; Alekseychik, Pavel; Amiro, Brian; Aurela, Mika; Barr, Alan G.; Black, T. Andrew; Carey, Sean K.; Chen, Jiquan; Chi, Jinshu; Desai, Ankur R.; Dunn, Allison; Euskirchen, Eugenie S.; Flanagan, Lawrence B.; Friborg, Thomas; Garneau, Michelle; Grelle, Achim; Harder, Silvie; Heliasz, Michal; Humphreys, Elyn R.; Ikawa, Hiroki; Isabelle, Pierre-Erik; Iwata, Hiroki; Jassal, Rachhpal; Korkiakoski, Mika; Kurbatova, Juliya; Kutzbach, Lars; Lapshina, Elena; Lindroth, Anders; Lofvenius, Mikaell Ottosson; Lohila, Annalea; Mammarella, Ivan; Marsh, Philip; Moore, Paul A.; Maximov, Trofim; Nadeau, Daniel F.; Nicholls, Erin M.; Nilsson, Mats B.; Ohta, Takeshi; Peichl, Matthias; Petrone, Richard M.; Prokushkin, Anatoly; Quinton, William L.; Roulet, Nigel; Runkle, Benjamin R. K.; Sonnentag, Oliver; Strachan, Ian B.; Taillardat, Pierre; Tuittila, Eeva-Stiina; Tuovinen, Juha-Pekka; Turner, Jessica; Ueyama, Masahito; Varlagin, Andrej; Vesala, Timo; Wilmking, Martin; Zyrianov, Vyacheslav; Schulze, Christopher
Contributor organization: Institute for Atmospheric and Earth System Research (INAR)
Micrometeorology and biogeochemical cycles
Biosciences
Viikki Plant Science Centre (ViPS)
Ecosystem processes (INAR Forest Sciences)
Date: 2020-10-15
Language: eng
Number of pages: 14
Belongs to series: Environmental Research Letters
ISSN: 1748-9326
DOI: https://doi.org/10.1088/1748-9326/abab34
URI: http://hdl.handle.net/10138/321067
Abstract: Peatlands and forests cover large areas of the boreal biome and are critical for global climate regulation. They also regulate regional climate through heat and water vapour exchange with the atmosphere. Understanding how land-atmosphere interactions in peatlands differ from forests may therefore be crucial for modelling boreal climate system dynamics and for assessing climate benefits of peatland conservation and restoration. To assess the biophysical impacts of peatlands and forests on peak growing season air temperature and humidity, we analysed surface energy fluxes and albedo from 35 peatlands and 37 evergreen needleleaf forests-the dominant boreal forest type-and simulated air temperature and vapour pressure deficit (VPD) over hypothetical homogeneous peatland and forest landscapes. We ran an evapotranspiration model using land surface parameters derived from energy flux observations and coupled an analytical solution for the surface energy balance to an atmospheric boundary layer (ABL) model. We found that peatlands, compared to forests, are characterized by higher growing season albedo, lower aerodynamic conductance, and higher surface conductance for an equivalent VPD. This combination of peatland surface properties results in a similar to 20% decrease in afternoon ABL height, a cooling (from 1.7 to 2.5 degrees C) in afternoon air temperatures, and a decrease in afternoon VPD (from 0.4 to 0.7 kPa) for peatland landscapes compared to forest landscapes. These biophysical climate impacts of peatlands are most pronounced at lower latitudes (similar to 45 degrees N) and decrease toward the northern limit of the boreal biome (similar to 70 degrees N). Thus, boreal peatlands have the potential to mitigate the effect of regional climate warming during the growing season. The biophysical climate mitigation potential of peatlands needs to be accounted for when projecting the future climate of the boreal biome, when assessing the climate benefits of conserving pristine boreal peatlands, and when restoring peatlands that have experienced peatland drainage and mining.
Subject: peatlands
boreal forest
climate mitigation
regional climate
energy balance
LAND-COVER CHANGE
SURFACE CONDUCTANCE
STOMATAL CONDUCTANCE
PERMAFROST THAW
ENERGY-BALANCE
NORTH-AMERICA
FOREST
CARBON
IMPACT
RESTORATION
1172 Environmental sciences
4112 Forestry
Peer reviewed: Yes
Rights: cc_by
Usage restriction: openAccess
Self-archived version: publishedVersion


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