Your browser doesn't support javascript.
loading
Vegetation type is an important predictor of the arctic summer land surface energy budget.
Oehri, Jacqueline; Schaepman-Strub, Gabriela; Kim, Jin-Soo; Grysko, Raleigh; Kropp, Heather; Grünberg, Inge; Zemlianskii, Vitalii; Sonnentag, Oliver; Euskirchen, Eugénie S; Reji Chacko, Merin; Muscari, Giovanni; Blanken, Peter D; Dean, Joshua F; di Sarra, Alcide; Harding, Richard J; Sobota, Ireneusz; Kutzbach, Lars; Plekhanova, Elena; Riihelä, Aku; Boike, Julia; Miller, Nathaniel B; Beringer, Jason; López-Blanco, Efrén; Stoy, Paul C; Sullivan, Ryan C; Kejna, Marek; Parmentier, Frans-Jan W; Gamon, John A; Mastepanov, Mikhail; Wille, Christian; Jackowicz-Korczynski, Marcin; Karger, Dirk N; Quinton, William L; Putkonen, Jaakko; van As, Dirk; Christensen, Torben R; Hakuba, Maria Z; Stone, Robert S; Metzger, Stefan; Vandecrux, Baptiste; Frost, Gerald V; Wild, Martin; Hansen, Birger; Meloni, Daniela; Domine, Florent; Te Beest, Mariska; Sachs, Torsten; Kalhori, Aram; Rocha, Adrian V; Williamson, Scott N.
Afiliação
  • Oehri J; Department of Evolutionary Biology and Environmental Studies, University of Zurich, Winterthurerstrasse 190, 8057, Zurich, Switzerland. jacqueline.oehri@gmail.com.
  • Schaepman-Strub G; Department of Biology, McGill University, 1205 Docteur Penfield, H3A 1B1, Montreal, QC, Canada. jacqueline.oehri@gmail.com.
  • Kim JS; Department of Evolutionary Biology and Environmental Studies, University of Zurich, Winterthurerstrasse 190, 8057, Zurich, Switzerland. gabriela.schaepman@ieu.uzh.ch.
  • Grysko R; Department of Evolutionary Biology and Environmental Studies, University of Zurich, Winterthurerstrasse 190, 8057, Zurich, Switzerland.
  • Kropp H; Low-Carbon and Climate Impact Research Centre, School of Energy and Environment, City University of Hong Kong, Tat Chee Ave, Kowloon Tong, Hongkong, People's Republic of China.
  • Grünberg I; Department of Evolutionary Biology and Environmental Studies, University of Zurich, Winterthurerstrasse 190, 8057, Zurich, Switzerland.
  • Zemlianskii V; Environmental Studies Program, Hamilton College, 198 College Hill Rd, Clinton, NY, USA.
  • Sonnentag O; Permafrost Research Section, Alfred-Wegener Institute, Telegrafenberg, 14473, Potsdam, Germany.
  • Euskirchen ES; Department of Evolutionary Biology and Environmental Studies, University of Zurich, Winterthurerstrasse 190, 8057, Zurich, Switzerland.
  • Reji Chacko M; Département de géographie, Université de Montréal, 2900 Edouard Montpetit Blvd, Montreal, QC, H3T 1J4, Canada.
  • Muscari G; Institute of Arctic Biology, University of Alaska Fairbanks, 2140 Koyukuk Dr, Fairbanks, AK, USA.
  • Blanken PD; Department of Evolutionary Biology and Environmental Studies, University of Zurich, Winterthurerstrasse 190, 8057, Zurich, Switzerland.
  • Dean JF; Institute of Terrestrial Ecosystems, ETH Zurich, CHN, Universitätstrasse 16, 8006, Zurich, Switzerland.
  • di Sarra A; Land Change Science Unit, Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), Zürcherstrasse 111, 8903, Birmensdorf, ZH, Switzerland.
  • Harding RJ; Istituto Nazionale di Geofisica e Vulcanologia, Via di Vigna Murata, 605, Rome, Italy.
  • Sobota I; Department of Geography, University of Colorado, Boulder, CO, USA.
  • Kutzbach L; School of Geographical Sciences, University of Bristol, University Rd, Bristol, UK.
  • Plekhanova E; Department for Sustainability, ENEA, Via Enrico Fermi 45, Frascati, Italy.
  • Riihelä A; UK Centre for Ecology & Hydrology (UKCEH), MacLean Bldg, Benson Ln, Crowmarsh Gifford, Wallingford, UK.
  • Boike J; Department of Hydrology and Water Management, Faculty of Earth Sciences and Spatial Management, Nicolaus Copernicus University, Lwowska, 87-100, Torun, Poland.
  • Miller NB; Center for Earth System Research and Sustainability (CEN), University of Hamburg, Bundesstrasse 53, 20146, Hamburg, Germany.
  • Beringer J; Department of Evolutionary Biology and Environmental Studies, University of Zurich, Winterthurerstrasse 190, 8057, Zurich, Switzerland.
  • López-Blanco E; Finnish Meteorological Institute, Erik Palménin aukio 1, 00560, Helsinki, Finland.
  • Stoy PC; Permafrost Research Section, Alfred-Wegener Institute, Telegrafenberg, 14473, Potsdam, Germany.
  • Sullivan RC; Geography Department, Humboldt-Universität zu Berlin, Unter den Linden 6, 10117, Berlin, Germany.
  • Kejna M; University of Wisconsin-Madison, Madison, WI, USA.
  • Parmentier FW; School of Agriculture and Environment, The University of Western Australia, 35 Stirling Hwy, Crawley, WA 6009, WA, Australia.
  • Gamon JA; Department of Environment and Minerals, Greenland Institute of Natural Resources, Kivioq 2, Nuuk, 3900, Greenland.
  • Mastepanov M; Department of Ecoscience, Aarhus University, Nordre Ringgade 1, 8000, Aarhus C, Denmark.
  • Wille C; University of Wisconsin-Madison, Madison, WI, USA.
  • Jackowicz-Korczynski M; Environmental Science Division, Argonne National Laboratory, 9700 S Cass Ave, Lemont, IL, USA.
  • Karger DN; Department of Meteorology and Climatology, Faculty of Earth Sciences and Spatial Management, Nicolaus Copernicus University, Lwowska, 87-100, Torun, Poland.
  • Quinton WL; Center for Biogeochemistry of the Anthropocene, Department of Geosciences, University of Oslo, Sem Sælands vei 1, 0371, Oslo, Norway.
  • Putkonen J; Department of Physical Geography and Ecosystem Science, Lund University, Geocentrum II, Sölvegatan 12, 223 62, Lund, Sweden.
  • van As D; University of Nebraska - Lincoln, 1400 R St, Lincoln, NE, USA.
  • Christensen TR; Department of Ecoscience, Aarhus University, Nordre Ringgade 1, 8000, Aarhus C, Denmark.
  • Hakuba MZ; Oulanka Research Station, University of Oulu, Pentti Kaiteran katu 1, 90570, Oulu, Finland.
  • Stone RS; GFZ German Research Centre for Geosciences, Wissenschaftspark Albert Einstein, Telegrafenberg, 14473, Potsdam, Germany.
  • Metzger S; Department of Ecoscience, Aarhus University, Nordre Ringgade 1, 8000, Aarhus C, Denmark.
  • Vandecrux B; Department of Physical Geography and Ecosystem Science, Lund University, Geocentrum II, Sölvegatan 12, 223 62, Lund, Sweden.
  • Frost GV; Swiss Federal Institute for Forest, Snow, and Landscape Research (WSL), Zürcherstrasse 111, 8903, Birmensdorf, ZH, Switzerland.
  • Wild M; Cold Regions Research Centre, Wilfrid Laurier University, 75 University Ave W, Waterloo, ON, Canada.
  • Hansen B; Harold Hamm School of Geology and Geological Engineering, University of North Dakota, Grand Forks, ND, USA.
  • Meloni D; Department of Glaciology and Climate, Geological Survey of Denmark and Greenland (GEUS), Øster Voldgade 10, 1350, Copenhagen, Denmark.
  • Domine F; Department of Ecoscience, Aarhus University, Nordre Ringgade 1, 8000, Aarhus C, Denmark.
  • Te Beest M; Oulanka Research Station, University of Oulu, Pentti Kaiteran katu 1, 90570, Oulu, Finland.
  • Sachs T; Jet Propulsion Laboratory, CalTech, 4800, Oak Grove Dr, Pasadena, CA, USA.
  • Kalhori A; NOAA Global Monitoring Laboratory, 325 Broadway, Boulder, CO, USA.
  • Rocha AV; National Ecological Observatory Network, Battelle, 1685 38th St #100, Boulder, CO, USA.
  • Williamson SN; Department of Atmospheric and Oceanic Sciences, University of Wisconsin-Madison, 1225 W Dayton St, Madison, WI, USA.
Nat Commun ; 13(1): 6379, 2022 10 31.
Article em En | MEDLINE | ID: mdl-36316310
ABSTRACT
Despite the importance of high-latitude surface energy budgets (SEBs) for land-climate interactions in the rapidly changing Arctic, uncertainties in their prediction persist. Here, we harmonize SEB observations across a network of vegetated and glaciated sites at circumpolar scale (1994-2021). Our variance-partitioning analysis identifies vegetation type as an important predictor for SEB-components during Arctic summer (June-August), compared to other SEB-drivers including climate, latitude and permafrost characteristics. Differences among vegetation types can be of similar magnitude as between vegetation and glacier surfaces and are especially high for summer sensible and latent heat fluxes. The timing of SEB-flux summer-regimes (when daily mean values exceed 0 Wm-2) relative to snow-free and -onset dates varies substantially depending on vegetation type, implying vegetation controls on snow-cover and SEB-flux seasonality. Our results indicate complex shifts in surface energy fluxes with land-cover transitions and a lengthening summer season, and highlight the potential for improving future Earth system models via a refined representation of Arctic vegetation types.
Assuntos

Texto completo: 1 Base de dados: MEDLINE Assunto principal: Ecossistema / Pergelissolo Tipo de estudo: Health_economic_evaluation / Prognostic_studies / Risk_factors_studies Idioma: En Ano de publicação: 2022 Tipo de documento: Article

Texto completo: 1 Base de dados: MEDLINE Assunto principal: Ecossistema / Pergelissolo Tipo de estudo: Health_economic_evaluation / Prognostic_studies / Risk_factors_studies Idioma: En Ano de publicação: 2022 Tipo de documento: Article