[1] IPCC (2013) Climate Change (2013): The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press. doi:10.1017/CBO9781107415324
[2] Schuur EA, McGuire AD, Schadel C, Grosse G, Harden JW, Hayes DJ, Hugelius G, Koven CD, Kuhry P, Lawrence DM, Natali SM, Olefeldt D, Romanovsky VE, Schaefer K, Turetsky MR, Treat CC, Vonk JE (2015): Climate change and the permafrost carbon feedback. Nature 520 (7546):171-179. doi:10.1038/nature14338
[3] Van Huissteden, J. (2020): Thawing Permafrost.Permafrost carbon in a warming Arctic. Springer Nature, 508 p.10. doi:1007/978-3-030-31379-1
[4] Chadburn SE, Burke E, Cox P, Friedlingstein P, Hugelius G, Westermann S (2017) An observation-based constraint on permafrost loss as a function of global warming. Nature Climate Change 7 (5):340 https://doi.org/10.1038/nclimate3262
[5] Osborn T, Jones P, (2020) Global Temperature Record. Climatic Research Unit School of Environmental Sciences, University of East Anglia. https://sites.uea.ac.uk/documents/421974/1295957/CRU-Info+sheet+1-2020.pdf/537e7c57-a746-0af2-5e7e-da3348cff961, geraadpleegd 26/11/2020 https://sites.uea.ac.uk/documents/421974/1295957/CRU-Info+sheet+1-2020.pdf/537e7c57-a746-0af2-5e7e-da3348cff961
[6] Lewkowicz AG, Way RG (2019): Extremes of summer climate trigger thousands of thermokarst landslides in a High Arctic environment. Nature Communications 10 (1):1329. doi:10.1038/s41467-019-09314-7
[7] Walter KM, Zimov SA, Chanton JP, Verbyla D, Chapin FS, 3rd (2006): Methane bubbling from Siberian thaw lakes as a positive feedback to climate warming. Nature 443 (7107):71-75. doi:10.1038/nature05040.
[8] Abbott BW, Jones JB (2015): Permafrost collapse alters soil carbon stocks, respiration, CH 4, and N2O in upland tundra. Global change biology 21 (12):4570-4587 https://doi.org/10.1111/gcb.13069
[9] Liljedahl AK, Boike J, Daanen RP, Fedorov AN, Frost GV, Grosse G, Hinzman LD, Iijma Y, Jorgenson JC, Matveyeva N, Necsoiu M, Raynolds MK, Romanovsky VE, Schulla J, Tape KD, Walker DA, Wilson CJ, Yabuki H, Zona D (2016): Pan-Arctic ice-wedge degradation in warming permafrost and its influence on tundra hydrology. Nature Geoscience 9 (4):312-318. doi:10.1038/ngeo2674
[10] Parmentier FW, Zhang W, Mi Y, Zhu X, van Huissteden J, Hayes DJ, Zhuang Q, Christensen TR, McGuire AD (2015) Rising methane emissions from northern wetlands associated with sea ice decline. Geophys Res Lett 42 (17):7214-7222. doi:10.1002/2015GL065013
[11] Parmentier F, Van Der Molen M, Van Huissteden J, Karsanaev S, Kononov A, Suzdalov D, Maximov T, Dolman A (2011): Longer growing seasons do not increase net carbon uptake in the northeastern Siberian tundra. Journal of Geophysical Research: Biogeosciences 116 (G4) https://doi.org/10.1029/2011JG001653
[12] Witze, A. (2020). The Arctic is burning like never before-and that’s bad news for climate change. Nature, 585(7825), 336-337. https://doi.org/10.1038/d41586-020-02568-y
[13] Walter Anthony KM, Anthony P, Grosse G, Chanton J (2012): Geologic methane seeps along boundaries of Arctic permafrost thaw and melting glaciers. Nature Geoscience 5 (6):419-426. doi:10.1038/ngeo1480
[14] Leibman MO, Kizyakov AI, Plekhanov AV, Streletskaya ID (2014) :New permafrost feature–deep crater in Central Yamal (West Siberia, Russia) as a response to local climate fluctuations. Environment Sustainability 4:68-80 https://doi.org/10.24057/2071-9388-2014-7-4-68-79
[15] Shakhova N, Semiletov I, Salyuk A, Yusupov V, Kosmach D, Gustafsson Ö (2010): Extensive methane venting to the atmosphere from sediments of the East Siberian Arctic Shelf. Science 327 (5970):1246-1250 DOI: 10.1126/science.1182221
[16] Anisimov O, Reneva S (2006) Permafrost and changing climate: the Russian perspective. AMBIO: A Journal of the Human Environment 35 (4):169-176 https://doi.org/10.1579/0044-7447(2006)35[169:PACCTR]2.0.CO;2
[17] Walter KM, Edwards ME, Grosse G, Zimov SA, Chapin FS, 3rd (2007):Thermokarst lakes as a source of atmospheric CH4 during the last deglaciation. Science 318 (5850):633-636. doi:10.1126/science.1142924
©De tekst is beschikbaar onder de licentie Creative Commons
Naamsvermelding-NietCommercieel-GelijkDelen 4.0 Internationaal, er kunnen aanvullende voorwaarden van
toepassing zijn. Zie de gebruiksvoorwaarden voor meer informatie.