.mw-parser-output .hidden-begin{box-sizing:border-box;width:100%;padding:5px;border:none;font-size:95%}.mw-parser-output .hidden-title{font-weight:bold;line-height:1.6;text-align:left}.mw-parser-output .hidden-content{text-align:left}You can help expand this article with text translated from the corresponding article in Finnish. (March 2012) Click [show] for important translation instructions.
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The landscape of yedoma areas is of glacier plains and hills with shallow depressions known as alas.[3] Yedoma usually form in lowlands or stretches of land with rolling hills where ice wedge polygonal networks are present, in stable relief features with accumulation zones of poor drainage, severe cold and arid continental climate zones resulting in scanty vegetation cover, intense periglacial weathering processes, as well as the proximity of sediment sources, such as low mountain ranges and foothills.[2]
The amount of carbon trapped in this type of permafrost is much more prevalent than originally thought and may be about 210 to 500 Gt,[4] that is a multiple of the amount of carbon released into the air each year by the burning of fossil fuels.[5] Thawing yedoma is a significant source of atmospheric methane (about 4 Tg of CH 4 per year).
The Yedoma region currently occupies an area of more than one million square kilometers from northeast Siberia to Alaska and Canada, and in many regions is tens of meters thick. During the Last Glacial Maximum, when the global sea level was 120 m lower than that of today, similar deposits covered substantial areas of the exposed northeast Eurasian continental shelves. At the end of the last ice age, at the Pleistocene–Holocene transition, thawing yedoma and the resulting thermokarst lakes may have produced 33 to 87% of the high-latitude increase in atmospheric methane concentration.[6]
Frederick West (1996), American Beginnings The University of Chicago Press, ISBN0-226-89399-5, p52
Velichko 1984, p141, Chapter 15, Tomirdiaro: Periglacial Landscapes and loessa Accumulation in the late pleistocene arctic and subarctic
K. M. Walter, S. A. Zimov, J. P. Chanton, D. Verbyla & F. S. Chapin III, "Methane bubbling from Siberian thaw lakes as a positive feedback to climate warming", Nature, 443, 71-75, 2006
Rutter&Velichko (1997) "Quaternary of northern eurasia: Late pleistocene and holocene landscapes, stratigraphy and environments, Nat W. Rutter, editor-in-chief, Guest editors A. A. Velichko et al., Vols 41/42 July/August 1997, ISSN1040-6182
Late Quaternary environments of Soviet Union, A.A. Velichko, engl edition Wright&Narnosky, pp176-177, University of Minnesota Publ, Longman, London 1984, ISBN0-582-30125-4
Schirrmeister, L., Fedorov, A. N., Froese, D., Iwahana, G., Van Huissteden, K., Veremeeva, A., eds. (2022). Yedoma Permafrost Landscapes as Past Archives, Present and Future Change Areas. Lausanne: Frontiers Media SA. doi:10.3389/978-2-88976-466-2
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