Sediment Waves on the Western Slope of the Chukchi Rise (Arctic Ocean) and Their Implications for the Paleoenvironment
Based on multibeam bathymetric data and high-resolution shallow sub-bottom profiles acquired during China’s 10th Arctic Scientific Expedition Cruise in 2019, a sediment wave field was found on the western slope of the Chukchi Rise, in the Arctic Ocean. This sediment wave field developed on the lower...
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ftdoajarticles:oai:doaj.org/article:c392bc0de9274bb18eb56fb7cbfe41ee 2023-05-15T14:46:40+02:00 Sediment Waves on the Western Slope of the Chukchi Rise (Arctic Ocean) and Their Implications for the Paleoenvironment Qingfeng Hua Guanbao Li Qingjie Zhou Shujiang Li Tengfei Xu Baohua Liu Hongxia Chen 2022-10-01T00:00:00Z https://doi.org/10.3390/jmse10111586 https://doaj.org/article/c392bc0de9274bb18eb56fb7cbfe41ee EN eng MDPI AG https://www.mdpi.com/2077-1312/10/11/1586 https://doaj.org/toc/2077-1312 doi:10.3390/jmse10111586 2077-1312 https://doaj.org/article/c392bc0de9274bb18eb56fb7cbfe41ee Journal of Marine Science and Engineering, Vol 10, Iss 1586, p 1586 (2022) seafloor bedform multibeam bathymetry sub-bottom profile bottom current Naval architecture. Shipbuilding. Marine engineering VM1-989 Oceanography GC1-1581 article 2022 ftdoajarticles https://doi.org/10.3390/jmse10111586 2022-12-30T22:37:29Z Based on multibeam bathymetric data and high-resolution shallow sub-bottom profiles acquired during China’s 10th Arctic Scientific Expedition Cruise in 2019, a sediment wave field was found on the western slope of the Chukchi Rise, in the Arctic Ocean. This sediment wave field developed on the lower slope with water depths of between 1200 m and 1800 m and stretched 15 km in the downslope direction. It comprised several parallel sediment waves, with wavelengths ranging from 700 m to 3400 m and wave heights from 12 m to 70 m. In the vertical direction, well-stratified deposits, tens of meters thick, were affected by sediment waves, which exhibit asymmetric waveforms and upslope migration trends. The morphological and seismostratigraphic characteristics of the sediment waves suggested their genesis as a result of the interaction between the bottom current and seafloor morphology, which was also supported by hydrographical data adjacent to the sediment wave field. It was infered that this bottom current was related to the Arctic Circumpolar Boundary Current, which many researchers suggest flows through the study area. Article in Journal/Newspaper Arctic Arctic Ocean Chukchi Directory of Open Access Journals: DOAJ Articles Arctic Arctic Ocean Chukchi Rise ENVELOPE(-165.000,-165.000,78.000,78.000) Journal of Marine Science and Engineering 10 11 1586 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
seafloor bedform multibeam bathymetry sub-bottom profile bottom current Naval architecture. Shipbuilding. Marine engineering VM1-989 Oceanography GC1-1581 |
spellingShingle |
seafloor bedform multibeam bathymetry sub-bottom profile bottom current Naval architecture. Shipbuilding. Marine engineering VM1-989 Oceanography GC1-1581 Qingfeng Hua Guanbao Li Qingjie Zhou Shujiang Li Tengfei Xu Baohua Liu Hongxia Chen Sediment Waves on the Western Slope of the Chukchi Rise (Arctic Ocean) and Their Implications for the Paleoenvironment |
topic_facet |
seafloor bedform multibeam bathymetry sub-bottom profile bottom current Naval architecture. Shipbuilding. Marine engineering VM1-989 Oceanography GC1-1581 |
description |
Based on multibeam bathymetric data and high-resolution shallow sub-bottom profiles acquired during China’s 10th Arctic Scientific Expedition Cruise in 2019, a sediment wave field was found on the western slope of the Chukchi Rise, in the Arctic Ocean. This sediment wave field developed on the lower slope with water depths of between 1200 m and 1800 m and stretched 15 km in the downslope direction. It comprised several parallel sediment waves, with wavelengths ranging from 700 m to 3400 m and wave heights from 12 m to 70 m. In the vertical direction, well-stratified deposits, tens of meters thick, were affected by sediment waves, which exhibit asymmetric waveforms and upslope migration trends. The morphological and seismostratigraphic characteristics of the sediment waves suggested their genesis as a result of the interaction between the bottom current and seafloor morphology, which was also supported by hydrographical data adjacent to the sediment wave field. It was infered that this bottom current was related to the Arctic Circumpolar Boundary Current, which many researchers suggest flows through the study area. |
format |
Article in Journal/Newspaper |
author |
Qingfeng Hua Guanbao Li Qingjie Zhou Shujiang Li Tengfei Xu Baohua Liu Hongxia Chen |
author_facet |
Qingfeng Hua Guanbao Li Qingjie Zhou Shujiang Li Tengfei Xu Baohua Liu Hongxia Chen |
author_sort |
Qingfeng Hua |
title |
Sediment Waves on the Western Slope of the Chukchi Rise (Arctic Ocean) and Their Implications for the Paleoenvironment |
title_short |
Sediment Waves on the Western Slope of the Chukchi Rise (Arctic Ocean) and Their Implications for the Paleoenvironment |
title_full |
Sediment Waves on the Western Slope of the Chukchi Rise (Arctic Ocean) and Their Implications for the Paleoenvironment |
title_fullStr |
Sediment Waves on the Western Slope of the Chukchi Rise (Arctic Ocean) and Their Implications for the Paleoenvironment |
title_full_unstemmed |
Sediment Waves on the Western Slope of the Chukchi Rise (Arctic Ocean) and Their Implications for the Paleoenvironment |
title_sort |
sediment waves on the western slope of the chukchi rise (arctic ocean) and their implications for the paleoenvironment |
publisher |
MDPI AG |
publishDate |
2022 |
url |
https://doi.org/10.3390/jmse10111586 https://doaj.org/article/c392bc0de9274bb18eb56fb7cbfe41ee |
long_lat |
ENVELOPE(-165.000,-165.000,78.000,78.000) |
geographic |
Arctic Arctic Ocean Chukchi Rise |
geographic_facet |
Arctic Arctic Ocean Chukchi Rise |
genre |
Arctic Arctic Ocean Chukchi |
genre_facet |
Arctic Arctic Ocean Chukchi |
op_source |
Journal of Marine Science and Engineering, Vol 10, Iss 1586, p 1586 (2022) |
op_relation |
https://www.mdpi.com/2077-1312/10/11/1586 https://doaj.org/toc/2077-1312 doi:10.3390/jmse10111586 2077-1312 https://doaj.org/article/c392bc0de9274bb18eb56fb7cbfe41ee |
op_doi |
https://doi.org/10.3390/jmse10111586 |
container_title |
Journal of Marine Science and Engineering |
container_volume |
10 |
container_issue |
11 |
container_start_page |
1586 |
_version_ |
1766317862481297408 |