Authors
Susan Natali, Benjamin W Abbott, Gerardo Celis, Paul Grogan, Casper Tai Christiansen, Patrick M Crill, Sergei P Davydov, Eugenie Susanne Euskirchen, Thomas Friborg, Helene Genet, Mathias Goeckede, Jordan P Goodrich, Elchin E Jafarov, Julie D Jastrow, Jocelyn E Egan, Aram AM Kalhori, Mark J Lara, Klaus Stenberg Larsen, Michael M Loranty, Sarah Ludwig, Massimo Lupascu, Avni Malhotra, Jack W Mcfarland, Anders Michelsen, Elisabeth Cooper, Walter C Oechel, David Olefeldt, Fereidoun Rezanezhad, David A Risk, Kevin M Schaefer, Niels Martin Schmidt, Anne-Katrin Selbmann, Claire C Treat, Mark P Waldrop, Donatella Zona, Edward Schuur, Philipp R Semenchuk, PF Sullivan, Bo Elberling, Kyle Andreas Arndt
Publication date
2016/12
Journal
AGU Fall Meeting Abstracts
Volume
2016
Pages
B41J-01
Description
Over the past several decades, surface air temperatures in the Arctic have increased at approximately twice the global rate, and climate models project that this rate of warming will continue through the century, with the greatest warming occurring during the winter months. Carbon emissions during the cold season (ie, fall, winter and spring) are an important component of annual respiratory loss, yet there are large uncertainties in local and regional estimates of cold season carbon emissions. To address these uncertainties, we conducted a pan-Arctic synthesis of cold season CO2 emissions from northern high latitude terrestrial ecosystems. We compiled data from more than 70 studies from sites located throughout the permafrost region. We examined differences in cold season respiration among permafrost zones, biomes, and ecosystem types. We found that cold season CO2 emissions were positively related to …
Scholar articles
S Natali, BW Abbott, G Celis, P Grogan… - AGU Fall Meeting Abstracts, 2016