The Biophysical Climate Mitigation Potential of Boreal Peatlands During the Growing Season

Manuel Helbig
James Michael Waddington
Pavel Alekseychik
Brian Amiro
Mika Aurela
Alan Barr
Andrew Black
Sean Carey
Jiquan Chen
Jinshu Chi
Ankur Desai
Allison Dunn
Eugenie Euskirchen
Lawrence Flanagan
Thomas Friborg
Michelle Garneau
Achim Grelle
Silvie Harder
Michal Heliasz
Elyn Humphrey
Hiroki Ikawa
Pierre-Erik Isabelle
Hiroki Iwata
Rachhpal Jassal
Mika Korkiakoski
Juliya Kurbatova
Lars Kutzbach
Elena Lapshina
Anders Lindroth
Mikaell Ottosson Lofvenius
Annalea Lohila
Ivan Mammarella
Philip Marsh
Paul Moore
Trofim Maximov
Daniel Nadeau
Erin Nicholls
Mats Nilsson
Takeshi Ohta
Matthias Peichl
Richard Petrone
Anatoly Prokushkin
William Quinton
Nigel Roulet
Benjamin Runkle
Oliver Sonnentag
Ian Strachan
Pierre Taillardat
Eeva-Stiina Tuittula
Juha-Pekka Tuovinen
Jessica Turner
Masahito Ueyama
Andrej Varlagin
Timo Vesala
Martin Wilmking
Vyacheslav Zyrianov
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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 ∼20% decrease in afternoon ABL height, a cooling (from 1.7 to 2.5 ◦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 (∼45◦N) and decrease toward the northern limit of the boreal biome (∼70◦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.