Coastal erosion dynamics on the permafrost-dominated Bykovsky Peninsula, north Siberia, 1951–2006
This study investigates the rate of erosion during the 1951–2006 period on the Bykovsky Peninsula, located north-east of the harbour town of Tiksi, north Siberia. Its coastline, which is characterized by the presence of ice-rich sediment (Ice Complex) and the vicinity of the Lena River Delta, retrea...
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Norwegian Polar Institute
2011
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Online Access: | https://doi.org/10.3402/polar.v30i0.7341 https://doaj.org/article/e7e7973a31c54bb58f218b9c33816a8e |
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fttriple:oai:gotriple.eu:oai:doaj.org/article:e7e7973a31c54bb58f218b9c33816a8e 2023-05-15T15:09:30+02:00 Coastal erosion dynamics on the permafrost-dominated Bykovsky Peninsula, north Siberia, 1951–2006 Hugues Lantuit David Atkinson Pier Paul Overduin Mikhail Grigoriev Volker Rachold Guido Grosse Hans-Wolfgang Hubberten 2011-09-01 https://doi.org/10.3402/polar.v30i0.7341 https://doaj.org/article/e7e7973a31c54bb58f218b9c33816a8e en eng Norwegian Polar Institute doi:10.3402/polar.v30i0.7341 0800-0395 1751-8369 https://doaj.org/article/e7e7973a31c54bb58f218b9c33816a8e undefined Polar Research, Vol 30, Iss 0, Pp 1-21 (2011) Coastal erosion permafrost Arctic climate change Russia geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2011 fttriple https://doi.org/10.3402/polar.v30i0.7341 2023-01-22T19:23:44Z This study investigates the rate of erosion during the 1951–2006 period on the Bykovsky Peninsula, located north-east of the harbour town of Tiksi, north Siberia. Its coastline, which is characterized by the presence of ice-rich sediment (Ice Complex) and the vicinity of the Lena River Delta, retreated at a mean rate of 0.59 m/yr between 1951 and 2006. Total erosion ranged from 434 m of erosion to 92 m of accretion during these 56 years and exhibited large variability (σ = 45.4). Ninety-seven percent of the rates observed were less than 2 m/yr and 81.6% were less than 1 m/yr. No significant trend in erosion could be recorded despite the study of five temporal subperiods within 1951–2006. Erosion modes and rates actually appear to be strongly dependant on the nature of the backshore material, erosion being stronger along low-lying coastal stretches affected by past or current thermokarst activity. The juxtaposition of wind records monitored at the town of Tiksi and erosion records yielded no significant relationship despite strong record amplitude for both data sets. We explain this poor relationship by the only rough incorporation of sea-ice cover in our storm extraction algorithm, the use of land-based wind records vs. offshore winds, the proximity of the peninsula to the Lena River Delta freshwater and sediment plume and the local topographical constraints on wave development. Article in Journal/Newspaper Arctic Climate change Ice lena river permafrost Polar Research Sea ice Thermokarst Tiksi Siberia Unknown Arctic Tiksi ENVELOPE(128.867,128.867,71.633,71.633) Polar Research 30 1 7341 |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
fttriple |
language |
English |
topic |
Coastal erosion permafrost Arctic climate change Russia geo envir |
spellingShingle |
Coastal erosion permafrost Arctic climate change Russia geo envir Hugues Lantuit David Atkinson Pier Paul Overduin Mikhail Grigoriev Volker Rachold Guido Grosse Hans-Wolfgang Hubberten Coastal erosion dynamics on the permafrost-dominated Bykovsky Peninsula, north Siberia, 1951–2006 |
topic_facet |
Coastal erosion permafrost Arctic climate change Russia geo envir |
description |
This study investigates the rate of erosion during the 1951–2006 period on the Bykovsky Peninsula, located north-east of the harbour town of Tiksi, north Siberia. Its coastline, which is characterized by the presence of ice-rich sediment (Ice Complex) and the vicinity of the Lena River Delta, retreated at a mean rate of 0.59 m/yr between 1951 and 2006. Total erosion ranged from 434 m of erosion to 92 m of accretion during these 56 years and exhibited large variability (σ = 45.4). Ninety-seven percent of the rates observed were less than 2 m/yr and 81.6% were less than 1 m/yr. No significant trend in erosion could be recorded despite the study of five temporal subperiods within 1951–2006. Erosion modes and rates actually appear to be strongly dependant on the nature of the backshore material, erosion being stronger along low-lying coastal stretches affected by past or current thermokarst activity. The juxtaposition of wind records monitored at the town of Tiksi and erosion records yielded no significant relationship despite strong record amplitude for both data sets. We explain this poor relationship by the only rough incorporation of sea-ice cover in our storm extraction algorithm, the use of land-based wind records vs. offshore winds, the proximity of the peninsula to the Lena River Delta freshwater and sediment plume and the local topographical constraints on wave development. |
format |
Article in Journal/Newspaper |
author |
Hugues Lantuit David Atkinson Pier Paul Overduin Mikhail Grigoriev Volker Rachold Guido Grosse Hans-Wolfgang Hubberten |
author_facet |
Hugues Lantuit David Atkinson Pier Paul Overduin Mikhail Grigoriev Volker Rachold Guido Grosse Hans-Wolfgang Hubberten |
author_sort |
Hugues Lantuit |
title |
Coastal erosion dynamics on the permafrost-dominated Bykovsky Peninsula, north Siberia, 1951–2006 |
title_short |
Coastal erosion dynamics on the permafrost-dominated Bykovsky Peninsula, north Siberia, 1951–2006 |
title_full |
Coastal erosion dynamics on the permafrost-dominated Bykovsky Peninsula, north Siberia, 1951–2006 |
title_fullStr |
Coastal erosion dynamics on the permafrost-dominated Bykovsky Peninsula, north Siberia, 1951–2006 |
title_full_unstemmed |
Coastal erosion dynamics on the permafrost-dominated Bykovsky Peninsula, north Siberia, 1951–2006 |
title_sort |
coastal erosion dynamics on the permafrost-dominated bykovsky peninsula, north siberia, 1951–2006 |
publisher |
Norwegian Polar Institute |
publishDate |
2011 |
url |
https://doi.org/10.3402/polar.v30i0.7341 https://doaj.org/article/e7e7973a31c54bb58f218b9c33816a8e |
long_lat |
ENVELOPE(128.867,128.867,71.633,71.633) |
geographic |
Arctic Tiksi |
geographic_facet |
Arctic Tiksi |
genre |
Arctic Climate change Ice lena river permafrost Polar Research Sea ice Thermokarst Tiksi Siberia |
genre_facet |
Arctic Climate change Ice lena river permafrost Polar Research Sea ice Thermokarst Tiksi Siberia |
op_source |
Polar Research, Vol 30, Iss 0, Pp 1-21 (2011) |
op_relation |
doi:10.3402/polar.v30i0.7341 0800-0395 1751-8369 https://doaj.org/article/e7e7973a31c54bb58f218b9c33816a8e |
op_rights |
undefined |
op_doi |
https://doi.org/10.3402/polar.v30i0.7341 |
container_title |
Polar Research |
container_volume |
30 |
container_issue |
1 |
container_start_page |
7341 |
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1766340683191287808 |