Arctic warming interrupts the Transpolar Drift and affects long-range transport of sea ice and ice-rafted matter
Sea ice is an important transport vehicle for gaseous, dissolved and particulate matter in the Arctic Ocean. Due to the recently observed acceleration in sea ice drift, it has been assumed that more matter is advected by the Transpolar Drift from shallow shelf waters to the central Arctic Ocean and...
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| Published in | Scientific reports Vol. 9; no. 1; p. 5459 |
|---|---|
| Main Authors | , , , , , , , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
London
Nature Publishing Group UK
02.04.2019
Nature Publishing Group |
| Subjects | |
| Online Access | Get full text |
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| Abstract | Sea ice is an important transport vehicle for gaseous, dissolved and particulate matter in the Arctic Ocean. Due to the recently observed acceleration in sea ice drift, it has been assumed that more matter is advected by the Transpolar Drift from shallow shelf waters to the central Arctic Ocean and beyond. However, this study provides first evidence that intensified melt in the marginal zones of the Arctic Ocean interrupts the transarctic conveyor belt and has led to a reduction of the survival rates of sea ice exported from the shallow Siberian shelves (−15% per decade). As a consequence, less and less ice formed in shallow water areas (<30 m) has reached Fram Strait (−17% per decade), and more ice and ice-rafted material is released in the northern Laptev Sea and central Arctic Ocean. Decreasing survival rates of first-year ice are visible all along the Russian shelves, but significant only in the Kara Sea, East Siberian Sea and western Laptev Sea. Identified changes affect biogeochemical fluxes and ecological processes in the central Arctic: A reduced long-range transport of sea ice alters transport and redistribution of climate relevant gases, and increases accumulation of sediments and contaminates in the central Arctic Ocean, with consequences for primary production, and the biodiversity of the Arctic Ocean. |
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| AbstractList | Sea ice is an important transport vehicle for gaseous, dissolved and particulate matter in the Arctic Ocean. Due to the recently observed acceleration in sea ice drift, it has been assumed that more matter is advected by the Transpolar Drift from shallow shelf waters to the central Arctic Ocean and beyond. However, this study provides first evidence that intensified melt in the marginal zones of the Arctic Ocean interrupts the transarctic conveyor belt and has led to a reduction of the survival rates of sea ice exported from the shallow Siberian shelves (−15% per decade). As a consequence, less and less ice formed in shallow water areas (<30 m) has reached Fram Strait (−17% per decade), and more ice and ice-rafted material is released in the northern Laptev Sea and central Arctic Ocean. Decreasing survival rates of first-year ice are visible all along the Russian shelves, but significant only in the Kara Sea, East Siberian Sea and western Laptev Sea. Identified changes affect biogeochemical fluxes and ecological processes in the central Arctic: A reduced long-range transport of sea ice alters transport and redistribution of climate relevant gases, and increases accumulation of sediments and contaminates in the central Arctic Ocean, with consequences for primary production, and the biodiversity of the Arctic Ocean. Sea ice is an important transport vehicle for gaseous, dissolved and particulate matter in the Arctic Ocean. Due to the recently observed acceleration in sea ice drift, it has been assumed that more matter is advected by the Transpolar Drift from shallow shelf waters to the central Arctic Ocean and beyond. However, this study provides first evidence that intensified melt in the marginal zones of the Arctic Ocean interrupts the transarctic conveyor belt and has led to a reduction of the survival rates of sea ice exported from the shallow Siberian shelves (-15% per decade). As a consequence, less and less ice formed in shallow water areas (<30 m) has reached Fram Strait (-17% per decade), and more ice and ice-rafted material is released in the northern Laptev Sea and central Arctic Ocean. Decreasing survival rates of first-year ice are visible all along the Russian shelves, but significant only in the Kara Sea, East Siberian Sea and western Laptev Sea. Identified changes affect biogeochemical fluxes and ecological processes in the central Arctic: A reduced long-range transport of sea ice alters transport and redistribution of climate relevant gases, and increases accumulation of sediments and contaminates in the central Arctic Ocean, with consequences for primary production, and the biodiversity of the Arctic Ocean. Sea ice is an important transport vehicle for gaseous, dissolved and particulate matter in the Arctic Ocean. Due to the recently observed acceleration in sea ice drift, it has been assumed that more matter is advected by the Transpolar Drift from shallow shelf waters to the central Arctic Ocean and beyond. However, this study provides first evidence that intensified melt in the marginal zones of the Arctic Ocean interrupts the transarctic conveyor belt and has led to a reduction of the survival rates of sea ice exported from the shallow Siberian shelves (-15% per decade). As a consequence, less and less ice formed in shallow water areas (<30 m) has reached Fram Strait (-17% per decade), and more ice and ice-rafted material is released in the northern Laptev Sea and central Arctic Ocean. Decreasing survival rates of first-year ice are visible all along the Russian shelves, but significant only in the Kara Sea, East Siberian Sea and western Laptev Sea. Identified changes affect biogeochemical fluxes and ecological processes in the central Arctic: A reduced long-range transport of sea ice alters transport and redistribution of climate relevant gases, and increases accumulation of sediments and contaminates in the central Arctic Ocean, with consequences for primary production, and the biodiversity of the Arctic Ocean.Sea ice is an important transport vehicle for gaseous, dissolved and particulate matter in the Arctic Ocean. Due to the recently observed acceleration in sea ice drift, it has been assumed that more matter is advected by the Transpolar Drift from shallow shelf waters to the central Arctic Ocean and beyond. However, this study provides first evidence that intensified melt in the marginal zones of the Arctic Ocean interrupts the transarctic conveyor belt and has led to a reduction of the survival rates of sea ice exported from the shallow Siberian shelves (-15% per decade). As a consequence, less and less ice formed in shallow water areas (<30 m) has reached Fram Strait (-17% per decade), and more ice and ice-rafted material is released in the northern Laptev Sea and central Arctic Ocean. Decreasing survival rates of first-year ice are visible all along the Russian shelves, but significant only in the Kara Sea, East Siberian Sea and western Laptev Sea. Identified changes affect biogeochemical fluxes and ecological processes in the central Arctic: A reduced long-range transport of sea ice alters transport and redistribution of climate relevant gases, and increases accumulation of sediments and contaminates in the central Arctic Ocean, with consequences for primary production, and the biodiversity of the Arctic Ocean. |
| ArticleNumber | 5459 |
| Author | Peeken, Ilka Stein, Rüdiger Krumpen, Thomas Nicolaus, Marcel Boetius, Antje Ricker, Robert Hendricks, Stefan Haas, Christian Paul, Stephan Damm, Ellen Belter, H. Jakob Nöthig, Eva-Maria |
| Author_xml | – sequence: 1 givenname: Thomas orcidid: 0000-0001-6234-8756 surname: Krumpen fullname: Krumpen, Thomas email: Thomas.krumpen@awi.de organization: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research – sequence: 2 givenname: H. Jakob orcidid: 0000-0001-9383-911X surname: Belter fullname: Belter, H. Jakob organization: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research – sequence: 3 givenname: Antje surname: Boetius fullname: Boetius, Antje organization: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research – sequence: 4 givenname: Ellen orcidid: 0000-0002-1487-1283 surname: Damm fullname: Damm, Ellen organization: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research – sequence: 5 givenname: Christian surname: Haas fullname: Haas, Christian organization: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research – sequence: 6 givenname: Stefan surname: Hendricks fullname: Hendricks, Stefan organization: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research – sequence: 7 givenname: Marcel surname: Nicolaus fullname: Nicolaus, Marcel organization: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research – sequence: 8 givenname: Eva-Maria orcidid: 0000-0002-7527-7827 surname: Nöthig fullname: Nöthig, Eva-Maria organization: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research – sequence: 9 givenname: Stephan surname: Paul fullname: Paul, Stephan organization: Ludwig Maximilians University, Department of Geography – sequence: 10 givenname: Ilka orcidid: 0000-0003-1531-1664 surname: Peeken fullname: Peeken, Ilka organization: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research – sequence: 11 givenname: Robert surname: Ricker fullname: Ricker, Robert organization: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research – sequence: 12 givenname: Rüdiger orcidid: 0000-0002-4453-9564 surname: Stein fullname: Stein, Rüdiger organization: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research |
| BackLink | https://www.ncbi.nlm.nih.gov/pubmed/30940829$$D View this record in MEDLINE/PubMed |
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| Snippet | Sea ice is an important transport vehicle for gaseous, dissolved and particulate matter in the Arctic Ocean. Due to the recently observed acceleration in sea... |
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| SubjectTerms | 704/106/125 704/106/694 704/47 Biodiversity Drift Gases Humanities and Social Sciences Ice Ice drift Marine pollution multidisciplinary Particulate matter Primary production Science Science (multidisciplinary) Sea ice Sediments Shallow water Survival Temperature |
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| Title | Arctic warming interrupts the Transpolar Drift and affects long-range transport of sea ice and ice-rafted matter |
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