Increasing contribution of peatlands to boreal evapotranspiration in a warming climate

Manuel Helbig*, James Michael Waddington, Pavel Alekseychik, Brian D. Amiro, Mika Aurela, Alan G. Barr, T. Andrew Black, Peter D. Blanken, Sean K. Carey, Jiquan Chen, Jinshu Chi, Ankur R. Desai, Allison Dunn, Eugenie S. Euskirchen, Lawrence B. Flanagan, Inke Forbrich, Thomas Friborg, Achim Grelle, Silvie Harder, Michal HeliaszElyn R. Humphreys, Hiroki Ikawa, Pierre Erik Isabelle, Hiroki Iwata, Rachhpal Jassal, Mika Korkiakoski, Juliya Kurbatova, Lars Kutzbach, Anders Lindroth, Mikaell Ottosson Löfvenius, Annalea Lohila, Ivan Mammarella, Philip Marsh, Trofim Maximov, Joe R. Melton, Paul A. Moore, Daniel F. Nadeau, Erin M. Nicholls, Mats B. Nilsson, Takeshi Ohta, Matthias Peichl, Richard M. Petrone, Roman Petrov, Anatoly Prokushkin, William L. Quinton, David E. Reed, Nigel T. Roulet, Benjamin R.K. Runkle, Oliver Sonnentag, Ian B. Strachan, Pierre Taillardat, Eeva Stiina Tuittila, Juha Pekka Tuovinen, Jessica Turner, Masahito Ueyama, Andrej Varlagin, Martin Wilmking, Steven C. Wofsy, Vyacheslav Zyrianov

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

142 Citations (Scopus)

Abstract

The response of evapotranspiration (ET) to warming is of critical importance to the water and carbon cycle of the boreal biome, a mosaic of land cover types dominated by forests and peatlands. The effect of warming-induced vapour pressure deficit (VPD) increases on boreal ET remains poorly understood because peatlands are not specifically represented as plant functional types in Earth system models. Here we show that peatland ET increases more than forest ET with increasing VPD using observations from 95 eddy covariance tower sites. At high VPD of more than 2 kPa, peatland ET exceeds forest ET by up to 30%. Future (2091–2100) mid-growing season peatland ET is estimated to exceed forest ET by over 20% in about one-third of the boreal biome for RCP4.5 and about two-thirds for RCP8.5. Peatland-specific ET responses to VPD should therefore be included in Earth system models to avoid biases in water and carbon cycle projections.

Original languageEnglish
Pages (from-to)555-560
Number of pages6
JournalNature Climate Change
Volume10
Issue number6
DOIs
Publication statusPublished - Jun 1 2020
Externally publishedYes

Bibliographical note

Publisher Copyright:
© 2020, The Author(s), under exclusive licence to Springer Nature Limited.

ASJC Scopus Subject Areas

  • Environmental Science (miscellaneous)
  • Social Sciences (miscellaneous)

Fingerprint

Dive into the research topics of 'Increasing contribution of peatlands to boreal evapotranspiration in a warming climate'. Together they form a unique fingerprint.

Cite this