Using thermoterrace dimensions to calculate the coastal erosion rate (in Russian)
Thermoterraces in syngenetic ice complexes are widespread along the erosion-dominated shores of the Yakutia Arctic coast. Thermoterraces progressively record quantitative information about their existence which may be used to determine the mean shore retreat rate during the time they are present. In...
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ftoceanrep:oai:oceanrep.geomar.de:27350 2023-05-15T14:59:34+02:00 Using thermoterrace dimensions to calculate the coastal erosion rate (in Russian) Are, Feliks E. Grigoriev, Mikhail N. Hubberten, Hans-Wolfgang Rachold, Volker 2004 https://oceanrep.geomar.de/id/eprint/27350/ unknown RAN Are, F. E., Grigoriev, M. N., Hubberten, H. W. and Rachold, V. (2004) Using thermoterrace dimensions to calculate the coastal erosion rate (in Russian) . Kriosfera Zemli (Earth Cryosphere, in Russian), 8 (3). pp. 52-56. Article PeerReviewed 2004 ftoceanrep 2023-04-07T15:17:18Z Thermoterraces in syngenetic ice complexes are widespread along the erosion-dominated shores of the Yakutia Arctic coast. Thermoterraces progressively record quantitative information about their existence which may be used to determine the mean shore retreat rate during the time they are present. Initial measurements of four thermoterraces were carried out by the authors on the south coast of the Dmitry Laptev Strait in 2002, and shore retreat rates were calculated. Comparison of erosion rates obtained using thermoterrace dimensions and geodetic survey results with rates determined using aerial photographs showed that the erosion rate values obtained in these two ways are approximately of the same order. Article in Journal/Newspaper Arctic laptev Yakutia OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Arctic |
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Open Polar |
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OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
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ftoceanrep |
language |
unknown |
description |
Thermoterraces in syngenetic ice complexes are widespread along the erosion-dominated shores of the Yakutia Arctic coast. Thermoterraces progressively record quantitative information about their existence which may be used to determine the mean shore retreat rate during the time they are present. Initial measurements of four thermoterraces were carried out by the authors on the south coast of the Dmitry Laptev Strait in 2002, and shore retreat rates were calculated. Comparison of erosion rates obtained using thermoterrace dimensions and geodetic survey results with rates determined using aerial photographs showed that the erosion rate values obtained in these two ways are approximately of the same order. |
format |
Article in Journal/Newspaper |
author |
Are, Feliks E. Grigoriev, Mikhail N. Hubberten, Hans-Wolfgang Rachold, Volker |
spellingShingle |
Are, Feliks E. Grigoriev, Mikhail N. Hubberten, Hans-Wolfgang Rachold, Volker Using thermoterrace dimensions to calculate the coastal erosion rate (in Russian) |
author_facet |
Are, Feliks E. Grigoriev, Mikhail N. Hubberten, Hans-Wolfgang Rachold, Volker |
author_sort |
Are, Feliks E. |
title |
Using thermoterrace dimensions to calculate the coastal erosion rate (in Russian) |
title_short |
Using thermoterrace dimensions to calculate the coastal erosion rate (in Russian) |
title_full |
Using thermoterrace dimensions to calculate the coastal erosion rate (in Russian) |
title_fullStr |
Using thermoterrace dimensions to calculate the coastal erosion rate (in Russian) |
title_full_unstemmed |
Using thermoterrace dimensions to calculate the coastal erosion rate (in Russian) |
title_sort |
using thermoterrace dimensions to calculate the coastal erosion rate (in russian) |
publisher |
RAN |
publishDate |
2004 |
url |
https://oceanrep.geomar.de/id/eprint/27350/ |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic laptev Yakutia |
genre_facet |
Arctic laptev Yakutia |
op_relation |
Are, F. E., Grigoriev, M. N., Hubberten, H. W. and Rachold, V. (2004) Using thermoterrace dimensions to calculate the coastal erosion rate (in Russian) . Kriosfera Zemli (Earth Cryosphere, in Russian), 8 (3). pp. 52-56. |
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1766331676523233280 |