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Aufeis

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form when the cross-sectional area of a stream channel becomes locally restricted as ice accumulates during winter. Such restrictions or “choke-points” result in bulk overflow and local increases in hydrostatic pressure, causing water to move upward through fissures onto the original ice layer. This
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until discharge occurs along the bank and over the top of the previously formed ice. Successive ice layers can grow and expand, attaining areas of ~25+ km and thicknesses of 6+ m. Aufeis typically melts out during summer and will often form in the same place year after year.
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Aufeis can present an extreme danger to recreational boaters even during summer months, who can find themselves trapped between walls of ice or pulled under aufeis by the current of the river. Breaking dams of aufeis can cause flash floods downriver.
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to widen as spring floodwaters are forced to flow around the ice. Research on aufeis has to a large extent been motivated by the variety of engineering problems the ice sheets can cause (e.g. blocking drainages and causing flooding of roads).
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Reise in den äussersten Norden und Osten Sibiriens während der Jahre 1843 und 1844 mit Allerhöchster Genehmigung auf Veranstaltung der Kaiserlichen Akademie der Wissenschaften zu St. Petersburg ausgef
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Terry, Neil; Grunewald, Elliot; Briggs, Martin; Gooseff, Michael; Huryn, Alexander D.; Kass, M. Andy; Tape, Ken D.; Hendrickson, Patrick; Lane, John W. (March 2020).
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streams as they freeze solid. Ground-water discharge is blocked by ice, perturbing the steady-state condition and causing a small incremental rise in the local
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Hu, Xiaogang; Pollard, Wayne H. (September 1997). "The Hydrologic Analysis and Modeling of River Icing Growth, North Fork Pass, Yukon Territory, Canada".
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in arctic Alaska—where they are also known as “icings”—attaining areas of 20+ km and localized thicknesses of 6+ m. The cumulative area of late-winter
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Clark, Ian D.; Lauriol, Bernard (1997). "Aufeis of the Firth River Basin, Northern Yukon, Canada: Insights into Permafrost Hydrogeology and Karst".
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Recent U.S. Geological Survey Studies in the Tintina Gold Province, Alaska, United States, and Yukon, Canada — Results of a 5-Year Project
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Reedyk, Sharon; Woo, Ming-Ko; Prowse, Terry D. (1995). "Contribution of icing ablation to streamflow in a discontinuous permafrost area".
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Analysis of satellite imagery from 2000 to 2015 has shown that the extent and duration of many Alaskan river icings has decreased due to
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Priesnitz, Kuno; Schunke, Ekkehard (2002). "The fluvial morphodynamics of two small permafrost drainage basins, northwestern Canada".
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are common and widespread features of the arctic cryosphere, particularly in northern Alaska and Siberia. In eastern Siberia, where
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Veillette, J.J.; Thomas, R.D. (November 1979). "Icings and seepage in frozen glacio-fluvial deposits, District of Keewatin, NWT".
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Huryn, Alexander D.; Gooseff, Michael N.; Hendrickson, Patrick J.; Briggs, Martin A.; Tape, Ken D.; Terry, Neil C. (2020-10-13).
797: 1290:(Report). Vol. Scientific Investigations Report 2007–5289–F. U.S. Department of the Interior and U.S. Geological Survey. 1229:"Rapid decline in river icings detected in Arctic Alaska: Implications for a changing hydrologic cycle and river ecosystems" 873:
Huryn, Alexander D; Slavik, Karie A; Lowe, Rex L; Parker, Stephanie M; Anderson, Dennis S; Peterson, Bruce J (2005-08-01).
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that forms from successive flows of ground or river water during freezing temperatures. This form of ice is also called
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Aufeis Accumulations in Stream Bottoms in Arctic and Subarctic Environments as an Indicator of Geologic Structure
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overflowing water subsequently freezes to produce additional ice layers, thus explaining the origin of the term
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Wanty, Richard B.; Wang, Bronwen; Vohden, Jim; et al. (2007). Gough, Larry P.; Day, Warren C. (eds.).
1141: 626:"Aufeis of the Firth River Basin, Northern Yukon, Canada: Insights into Permafrost Hydrogeology and Karst" 1570: 875:"Landscape heterogeneity and the biodiversity of Arctic stream communities: a habitat template analysis" 1509: 196:. This process, repeated through the long arctic winter, can generate large volumes of ice, with some 131:
Aufeis literally translates from German to “on-ice”. In 1859 the Baltic German scientist and explorer
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In late 2011, Mongolia planned to test the use and storage of artificial naleds as a way of cooling
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Ashton, George D. 1986. River and lake ice engineering. Chelsea, Michigan, USA: Book Crafters, Inc.
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barrens are distinctive landscape features of the arctic tundra and provide reliable indicators of
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with a cumulative area of ~ 50,000 km containing 30 km of water have been documented in 2015.
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in the Sagavanirktok River drainage alone, for example, ranges from 102 to 103 km.
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Swanson-Hysell, Nicholas; Dander, Enkhbayar (2005). Eberhart, Marlene (ed.).
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used this term to describe his observations of the phenomenon in northern
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10.1002/(SICI)1099-1530(199709)8:3<279::AID-PPP260>3.0.CO;2-7
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Yoshikawa, Kenji; Hinzman, Larry D.; Kane, Douglas L. (December 2007).
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in the hot Mongolian summer, and reducing the use of energy-intensive
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Froehlich, Wojciech; Slupik, January (1982). French, H.M. (ed.).
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Kane, Douglas L. (1981). "Physical mechanics of aufeis growth".
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A Sheet of Aufeis in the Kharkhiraa Mountains, Mongolian Altai
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USSR Contribution, Permafrost: Second International Conference
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Sheets of aufeis may block stream channels and cause their
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environments. It forms by upwelling of river water behind
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following his observations of the phenomenon in northern
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glades or, perhaps more accurately in tundra habitats,
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Harden, Deborah; Barnes, Peter; Reimnitz, Erk (1977).
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Pavelsky, Tamlin M.; Zarnetske, Jay P. (2017-01-01).
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due to ice cover during much of the growing season.
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due to ice cover during much of the growing season.
1130:Sokolov, B. L. (1978). Sanger, Frederick J. (ed.). 586: 584: 582: 349:"Mineral Precipitation in North Slope River Icings" 36: 879:Canadian Journal of Fisheries and Aquatic Sciences 68:for "ice on top") is a sheet-like mass of layered 1226: 151:A sheet of aufeis in a glacial valley in Mongolia 1953: 1079: 579: 1278: 1174:Proceedings, 4th Canadian Permafrost Conference 1164: 1009: 982: 597:Journal of Geophysical Research: Biogeosciences 445: 443: 307:Sheets of aufeis have been observed in Alaska, 96:). The term "Aufeis" was first used in 1859 by 677:Journal of Geophysical Research: Earth Surface 539:"Cryogenesis and geodynamics of icing valleys" 1329: 1114: 1044: 624:Clark, Ian D.; Lauriol, Bernard (May 1997). 623: 440: 427:"The Canning River region, northern Alaska" 424: 390: 216:Backpackers cross a sheet of aufeis in the 1336: 1322: 1252: 959: 898: 771: 769: 608: 562: 536: 498: 467: 364: 386: 384: 252:barrens, because of the near absence of 211: 146: 119:barrens, because of the near absence of 18: 1129: 942: 816: 814: 155:Aufeis accumulates during winter along 23:Laminations of ice in a sheet of aufeis 1954: 766: 725: 342: 340: 338: 1317: 921: 849:"Dangers of Aufeis on Alaskan Rivers" 823:Canadian Journal of Civil Engineering 409: 381: 1082:Permafrost and Periglacial Processes 922:Watts, Jonathan (15 November 2011). 820: 811: 502:Permafrost and Periglacial Processes 346: 335: 13: 1272: 1012:Canadian Journal of Earth Sciences 425:Leffingwell, Ernest de K. (1919). 14: 1993: 1295: 240:leave footprints in the form of “ 1941:Template:Periglacial environment 1301: 1115:Alekseev, V.; Savko, N. (1975). 543:Geodynamics & Tectonophysics 391:Middendorff, A. Th. von (1847). 111:leave footprints in the form of 32: 1220: 1180: 1158: 1123: 1108: 1073: 1038: 1003: 976: 936: 915: 866: 841: 719: 664: 347:Hall, Dorothy K. (1980-01-01). 267: 617: 492: 418: 244:glades” or more accurately in 16:Sheet-like mass of layered ice 1: 1117:The theory of naled processes 985:Canadian Geotechnical Journal 943:Sokolov, B. L. (1991-08-01). 752:10.1016/s0034-4257(96)00167-8 732:Remote Sensing of Environment 329: 283: 1343: 1233:Geophysical Research Letters 1142:National Academy of Sciences 142: 126: 7: 10: 1998: 1047:Arctic and Alpine Research 630:Arctic and Alpine Research 456:Limnology and Oceanography 1921: 1854: 1793: 1670: 1661: 1630: 1609: 1533: 1422: 1351: 537:Alekseyev, V. R. (2015). 207: 133:Alexander von Middendorff 98:Alexander von Middendorff 93: 1119:. Nayka. pp. 1–205. 564:10.5800/gt-2015-6-2-0177 1977:Geography of the Arctic 403:10.5962/bhl.title.52029 726:Shusun, L (May 1997). 434:U.S. Geological Survey 221: 152: 24: 1879:Giant current ripples 215: 150: 22: 1310:at Wikimedia Commons 1254:10.1002/2016GL072397 1144:. pp. 408–411. 961:10.2166/nh.1991.0015 697:10.1029/2019JF005345 610:10.1029/2006JG000294 1816:Moraine-dammed lake 1643:Subglacial eruption 1245:2017GeoRL..44.3228P 1239:(7): 2016GL072397. 1024:1995CaJES..32...13R 794:10.14430/arctic2681 744:1997RSEnv..60..131S 689:2020JGRF..12505345T 555:2015GeTec...6..171A 366:10.14430/arctic2567 1648:Subglacial volcano 1631:Volcanic relations 948:Hydrology Research 222: 153: 25: 1949: 1948: 1917: 1916: 1435:Accumulation zone 1306:Media related to 469:10.1002/lno.11626 1989: 1836:Terminal moraine 1668: 1667: 1404:Piedmont glacier 1338: 1331: 1324: 1315: 1314: 1305: 1291: 1285: 1267: 1266: 1256: 1224: 1218: 1217: 1211: 1207: 1205: 1197: 1195: 1184: 1178: 1177: 1171: 1162: 1156: 1155: 1133:Regime of Naleds 1127: 1121: 1120: 1112: 1106: 1105: 1077: 1071: 1070: 1042: 1036: 1035: 1007: 1001: 1000: 980: 974: 973: 963: 940: 934: 933: 919: 913: 912: 902: 885:(8): 1905–1919. 870: 864: 863: 861: 859: 845: 839: 838: 818: 809: 808: 806: 805: 796:. 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balance 1610:Measurements 1546:Accumulation 1470:Glacier head 1465:Glacier cave 1409:Rock glacier 1358: 1287: 1236: 1232: 1222: 1189: 1182: 1173: 1160: 1137: 1132: 1125: 1116: 1110: 1085: 1081: 1075: 1050: 1046: 1040: 1018:(1): 13–20. 1015: 1011: 1005: 988: 984: 978: 951: 947: 938: 929:The Guardian 927: 917: 882: 878: 868: 856:. 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Index


/ˈfs/
OW-fysse
German
ice
Russian
Russian
Alexander von Middendorff
Siberia
vascular plants
Alexander von Middendorff
Siberia

stream
river
arctic
subarctic
ice dams
alpine
water table

Anaktuvuk River
flood plains
tundra
vascular plants
Ulan Bator
air conditioning
Arctic Canada
Russia
Mongolia

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