Shallow soils are warmer under trees and tall shrubs across Arctic and Boreal ecosystems ...

• Main Authors: Kropp, Heather, Loranty, Michael M, Natali, Susan M, Kholodov, Alexander L, Rocha, Adrian V, Myers-Smith, Isla, Abbot, Benjamin W, Abermann, Jakob, Blanc-Betes, Elena, Blok, Daan, Blume-Werry, Gesche, Boike, Julia, Breen, Amy L, Cahoon, Sean M P, Christiansen, Casper T, Douglas, Thomas A, Epstein, Howard E, Frost, Gerald V, Goeckede, Mathias, Høye, Toke T, Mamet, Steven D, O’Donnell, Jonathan A, Olefeldt, David, Phoenix, Gareth K, Salmon, Verity G, Sannel, A Britta K, Smith, Sharon L, Sonnentag, Oliver, Vaughn, Lydia Smith, Williams, Mathew, Elberling, Bo, Gough, Laura, Hjort, Jan, Lafleur, Peter M, Euskirchen, Eugenie S, Heijmans, Monique MPD, Humphreys, Elyn R, Iwata, Hiroki, Jones, Benjamin M, Jorgenson, M Torre, Grünberg, Inge, Kim, Yongwon, Laundre, James, Mauritz, Marguerite, Michelsen, Anders, Schaepman-Strub, Gabriela, Tape, Ken D, Ueyama, Masahito, Lee, Bang-Yong, Langley, Kirsty
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Humboldt-Universität zu Berlin 2020
• Subjects: Arctic; boreal forest; soil temperature; vegetation change; permafrost; 550 Geowissenschaften; Tundra
• Online Access: https://dx.doi.org/10.18452/27611; https://edoc.hu-berlin.de/handle/18452/28262

Soils are warming as air temperatures rise across the Arctic and Boreal region concurrent with the expansion of tall-statured shrubs and trees in the tundra. Changes in vegetation structure and function are expected to alter soil thermal regimes, thereby modifying climate feedbacks related to permafrost thaw and carbon cycling. However, current understanding of vegetation impacts on soil temperature is limited to local or regional scales and lacks the generality necessary to predict soil warming and permafrost stability on a pan-Arctic scale. Here we synthesize shallow soil and air temperature observations with broad spatial and temporal coverage collected across 106 sites representing nine different vegetation types in the permafrost region. We showed ecosystems with tall-statured shrubs and trees (>40 cm) have warmer shallow soils than those with short-statured tundra vegetation when normalized to a constant air temperature. In tree and tall shrub vegetation types, cooler temperatures in the warm season ...