Details

Autor(en) / Beteiligte

• Commane, Róisín
• Lindaas, Jakob
• Benmergui, Joshua
• Luus, Kristina A.
• Chang, Rachel Y.-W.
• Daube, Bruce C.
• Euskirchen, Eugénie S.
• Henderson, John M.
• Karion, Anna
• Miller, John B.
• Miller, Scot M.
• Parazoo, Nicholas C.
• Randerson, James T.
• Sweeney, Colm
• Tans, Pieter
• Thoning, Kirk
• Veraverbeke, Sander
• Miller, Charles E.
• Wofsy, Steven C.

Titel

Carbon dioxide sources from Alaska driven by increasing early winter respiration from Arctic tundra

Ist Teil von

• Proceedings of the National Academy of Sciences - PNAS, 2017-05, Vol.114 (21), p.5361-5366

Ort / Verlag

United States: National Academy of Sciences

Erscheinungsjahr

2017

Link zum Volltext

Quelle

Free E-Journal (出版社公開部分のみ）

Beschreibungen/Notizen

• High-latitude ecosystems have the capacity to release large amounts of carbon dioxide (CO₂) to the atmosphere in response to increasing temperatures, representing a potentially significant positive feedback within the climate system. Here, we combine aircraft and tower observations of atmospheric CO₂ with remote sensing data and meteorological products to derive temporally and spatially resolved year-round CO₂ fluxes across Alaska during 2012–2014. We find that tundra ecosystems were a net source of CO₂ to the atmosphere annually, with especially high rates of respiration during early winter (October through December). Long-term records at Barrow, AK, suggest that CO₂ emission rates from North Slope tundra have increased during the October through December period by 73% ± 11% since 1975, and are correlated with rising summer temperatures. Together, these results imply increasing early winter respiration and net annual emission of CO₂ in Alaska, in response to climate warming. Our results provide evidence that the decadal-scale increase in the amplitude of the CO₂ seasonal cycle may be linked with increasing biogenic emissions in the Arctic, following the growing season. Early winter respiration was not well simulated by the Earth System Models used to forecast future carbon fluxes in recent climate assessments. Therefore, these assessments may underestimate the carbon release from Arctic soils in response to a warming climate.