The Arctic Coastal Dynamics Database: A New Classification Scheme and Statistics on Arctic Permafrost Coastlines
Arctic permafrost coasts are sensitive to changing climate. The lengthening open water season and the increasing open water area are likely to induce greater erosion and threaten community and industry infrastructure as well as dramatically change nutrient pathways in the near-shore zone. The shallo...
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creator | Lantuit, Hugues Overduin, Pier Paul Couture, Nicole Wetterich, Sebastian Aré, Felix Atkinson, David Brown, Jerry Cherkashov, Georgy Drozdov, Dmitry Forbes, Donald Lawrence Graves-Gaylord, Allison Grigoriev, Mikhail Hubberten, Hans-Wolfgang Jordan, James Jorgenson, Torre Ødegård, Rune Strand Ogorodov, Stanislav Pollard, Wayne H. Rachold, Volker Sedenko, Sergey Solomon, Steve Steenhuisen, Frits Streletskaya, Irina Vasiliev, Alexander |
description | Arctic permafrost coasts are sensitive to changing climate. The lengthening open water season and the increasing open water area are likely to induce greater erosion and threaten community and industry infrastructure as well as dramatically change nutrient pathways in the near-shore zone. The shallow, mediterranean Arctic Ocean is likely to be strongly affected by changes in currently poorly observed arctic coastal dynamics. We present a geomorphological classification scheme for the arctic coast, with 101,447 km of coastline in 1,315 segments. The average rate of erosion for the arctic coast is 0.5 m year⁻¹ with high local and regional variability. Highest rates are observed in the Laptev, East Siberian, and Beaufort Seas. Strong spatial variability in associated database bluff height, ground carbon and ice content, and coastline movement highlights the need to estimate the relative importance of shifting coastal fluxes to the Arctic Ocean at multiple spatial scales. |
doi_str_mv | 10.1007/s12237-010-9362-6 |
format | Article |
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The lengthening open water season and the increasing open water area are likely to induce greater erosion and threaten community and industry infrastructure as well as dramatically change nutrient pathways in the near-shore zone. The shallow, mediterranean Arctic Ocean is likely to be strongly affected by changes in currently poorly observed arctic coastal dynamics. We present a geomorphological classification scheme for the arctic coast, with 101,447 km of coastline in 1,315 segments. The average rate of erosion for the arctic coast is 0.5 m year⁻¹ with high local and regional variability. Highest rates are observed in the Laptev, East Siberian, and Beaufort Seas. Strong spatial variability in associated database bluff height, ground carbon and ice content, and coastline movement highlights the need to estimate the relative importance of shifting coastal fluxes to the Arctic Ocean at multiple spatial scales.</description><identifier>ISSN: 1559-2723</identifier><identifier>EISSN: 1559-2731</identifier><identifier>DOI: 10.1007/s12237-010-9362-6</identifier><language>eng</language><publisher>New York: Spring Science + Business Media</publisher><subject>Beaches ; Carbon cycle ; Climate change ; Coastal Sciences ; Coastal zone management ; Coasts ; Datasets ; Earth and Environmental Science ; Ecology ; Environment ; Environmental Management ; Erosion ; Erosion rates ; Estuaries ; Freshwater & Marine Ecology ; Ice ; Marine ; Permafrost ; Seas ; Sediments ; Soil organic carbon ; SPECIAL SECTION: THE ARCTIC OCEAN ESTUARY ; Water and Health</subject><ispartof>Estuaries and coasts, 2012-03, Vol.35 (2), p.383-400</ispartof><rights>2012 Coastal and Estuarine Research Federation</rights><rights>Coastal and Estuarine Research Federation 2011</rights><rights>Coastal and Estuarine Research Federation 2012</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a501t-d86206afc1821d9286459ddf60995488e38b8713328a4a66262e597562d7ce273</citedby><cites>FETCH-LOGICAL-a501t-d86206afc1821d9286459ddf60995488e38b8713328a4a66262e597562d7ce273</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/41486638$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/41486638$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,777,781,800,27905,27906,41469,42538,51300,57998,58231</link.rule.ids></links><search><creatorcontrib>Lantuit, Hugues</creatorcontrib><creatorcontrib>Overduin, Pier Paul</creatorcontrib><creatorcontrib>Couture, Nicole</creatorcontrib><creatorcontrib>Wetterich, Sebastian</creatorcontrib><creatorcontrib>Aré, Felix</creatorcontrib><creatorcontrib>Atkinson, David</creatorcontrib><creatorcontrib>Brown, Jerry</creatorcontrib><creatorcontrib>Cherkashov, Georgy</creatorcontrib><creatorcontrib>Drozdov, Dmitry</creatorcontrib><creatorcontrib>Forbes, Donald Lawrence</creatorcontrib><creatorcontrib>Graves-Gaylord, Allison</creatorcontrib><creatorcontrib>Grigoriev, Mikhail</creatorcontrib><creatorcontrib>Hubberten, Hans-Wolfgang</creatorcontrib><creatorcontrib>Jordan, James</creatorcontrib><creatorcontrib>Jorgenson, Torre</creatorcontrib><creatorcontrib>Ødegård, Rune Strand</creatorcontrib><creatorcontrib>Ogorodov, Stanislav</creatorcontrib><creatorcontrib>Pollard, Wayne H.</creatorcontrib><creatorcontrib>Rachold, Volker</creatorcontrib><creatorcontrib>Sedenko, Sergey</creatorcontrib><creatorcontrib>Solomon, Steve</creatorcontrib><creatorcontrib>Steenhuisen, Frits</creatorcontrib><creatorcontrib>Streletskaya, Irina</creatorcontrib><creatorcontrib>Vasiliev, Alexander</creatorcontrib><title>The Arctic Coastal Dynamics Database: A New Classification Scheme and Statistics on Arctic Permafrost Coastlines</title><title>Estuaries and coasts</title><addtitle>Estuaries and Coasts</addtitle><description>Arctic permafrost coasts are sensitive to changing climate. The lengthening open water season and the increasing open water area are likely to induce greater erosion and threaten community and industry infrastructure as well as dramatically change nutrient pathways in the near-shore zone. The shallow, mediterranean Arctic Ocean is likely to be strongly affected by changes in currently poorly observed arctic coastal dynamics. We present a geomorphological classification scheme for the arctic coast, with 101,447 km of coastline in 1,315 segments. The average rate of erosion for the arctic coast is 0.5 m year⁻¹ with high local and regional variability. Highest rates are observed in the Laptev, East Siberian, and Beaufort Seas. Strong spatial variability in associated database bluff height, ground carbon and ice content, and coastline movement highlights the need to estimate the relative importance of shifting coastal fluxes to the Arctic Ocean at multiple spatial scales.</description><subject>Beaches</subject><subject>Carbon cycle</subject><subject>Climate change</subject><subject>Coastal Sciences</subject><subject>Coastal zone management</subject><subject>Coasts</subject><subject>Datasets</subject><subject>Earth and Environmental Science</subject><subject>Ecology</subject><subject>Environment</subject><subject>Environmental Management</subject><subject>Erosion</subject><subject>Erosion rates</subject><subject>Estuaries</subject><subject>Freshwater & Marine Ecology</subject><subject>Ice</subject><subject>Marine</subject><subject>Permafrost</subject><subject>Seas</subject><subject>Sediments</subject><subject>Soil organic carbon</subject><subject>SPECIAL SECTION: THE ARCTIC OCEAN 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The lengthening open water season and the increasing open water area are likely to induce greater erosion and threaten community and industry infrastructure as well as dramatically change nutrient pathways in the near-shore zone. The shallow, mediterranean Arctic Ocean is likely to be strongly affected by changes in currently poorly observed arctic coastal dynamics. We present a geomorphological classification scheme for the arctic coast, with 101,447 km of coastline in 1,315 segments. The average rate of erosion for the arctic coast is 0.5 m year⁻¹ with high local and regional variability. Highest rates are observed in the Laptev, East Siberian, and Beaufort Seas. 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subjects | Beaches Carbon cycle Climate change Coastal Sciences Coastal zone management Coasts Datasets Earth and Environmental Science Ecology Environment Environmental Management Erosion Erosion rates Estuaries Freshwater & Marine Ecology Ice Marine Permafrost Seas Sediments Soil organic carbon SPECIAL SECTION: THE ARCTIC OCEAN ESTUARY Water and Health |
title | The Arctic Coastal Dynamics Database: A New Classification Scheme and Statistics on Arctic Permafrost Coastlines |
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