Probing the fine structure of ocean sound‐scattering layers with ROVERSE technology
A 420‐kHz, dual‐beam SONAR system, deployed on a remotely operated vehicle (ROV), was used to examine the fine structure of sound‐scattering layers (SSLs) in Puget Sound and the Arctic Ocean. The Puget Sound SSL, initially detected with a shipboard, 200‐kHz SONAR system, was correlated with a high b...
Published in: | Limnology and Oceanography |
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crwiley:10.4319/lo.1991.36.1.0193 2023-12-03T10:16:25+01:00 Probing the fine structure of ocean sound‐scattering layers with ROVERSE technology Greene, Charles H. Wiebe, Peter H. Miyamoto, Robert T. Burczynski, Janusz 1991 http://dx.doi.org/10.4319/lo.1991.36.1.0193 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.1991.36.1.0193 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.1991.36.1.0193 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Limnology and Oceanography volume 36, issue 1, page 193-204 ISSN 0024-3590 1939-5590 Aquatic Science Oceanography journal-article 1991 crwiley https://doi.org/10.4319/lo.1991.36.1.0193 2023-11-09T14:04:11Z A 420‐kHz, dual‐beam SONAR system, deployed on a remotely operated vehicle (ROV), was used to examine the fine structure of sound‐scattering layers (SSLs) in Puget Sound and the Arctic Ocean. The Puget Sound SSL, initially detected with a shipboard, 200‐kHz SONAR system, was correlated with a high biomass of sound scatterers in the size range of macrozooplankton and micronekton. Its vertical position appeared unrelated to profiles of temperature, salinity, or chlorophyll fluorescence. The Arctic Ocean SSL was composed of similar‐sized sound scatterers, although its volume backscattering intensity was 10–100 times lower than that observed for the Puget Sound SSL. The vertical position of the Arctic SSL was closely associated with the thermocline separating Arctic Water from North Atlantic Water. The fine‐scale, horizontal variability of water‐column volume backscattering was examined at both study sites. The highest variability observed was associated with the Puget Sound SSL where the mean intensity of volume backscattering was also the highest. These findings are consistent with the common observation that, whatever methods are used to measure zooplankton and micronekton abundance, sampling variance nearly always increases with the mean. Article in Journal/Newspaper Arctic Arctic Ocean North Atlantic Zooplankton Wiley Online Library (via Crossref) Arctic Arctic Ocean Limnology and Oceanography 36 1 193 204 |
institution |
Open Polar |
collection |
Wiley Online Library (via Crossref) |
op_collection_id |
crwiley |
language |
English |
topic |
Aquatic Science Oceanography |
spellingShingle |
Aquatic Science Oceanography Greene, Charles H. Wiebe, Peter H. Miyamoto, Robert T. Burczynski, Janusz Probing the fine structure of ocean sound‐scattering layers with ROVERSE technology |
topic_facet |
Aquatic Science Oceanography |
description |
A 420‐kHz, dual‐beam SONAR system, deployed on a remotely operated vehicle (ROV), was used to examine the fine structure of sound‐scattering layers (SSLs) in Puget Sound and the Arctic Ocean. The Puget Sound SSL, initially detected with a shipboard, 200‐kHz SONAR system, was correlated with a high biomass of sound scatterers in the size range of macrozooplankton and micronekton. Its vertical position appeared unrelated to profiles of temperature, salinity, or chlorophyll fluorescence. The Arctic Ocean SSL was composed of similar‐sized sound scatterers, although its volume backscattering intensity was 10–100 times lower than that observed for the Puget Sound SSL. The vertical position of the Arctic SSL was closely associated with the thermocline separating Arctic Water from North Atlantic Water. The fine‐scale, horizontal variability of water‐column volume backscattering was examined at both study sites. The highest variability observed was associated with the Puget Sound SSL where the mean intensity of volume backscattering was also the highest. These findings are consistent with the common observation that, whatever methods are used to measure zooplankton and micronekton abundance, sampling variance nearly always increases with the mean. |
format |
Article in Journal/Newspaper |
author |
Greene, Charles H. Wiebe, Peter H. Miyamoto, Robert T. Burczynski, Janusz |
author_facet |
Greene, Charles H. Wiebe, Peter H. Miyamoto, Robert T. Burczynski, Janusz |
author_sort |
Greene, Charles H. |
title |
Probing the fine structure of ocean sound‐scattering layers with ROVERSE technology |
title_short |
Probing the fine structure of ocean sound‐scattering layers with ROVERSE technology |
title_full |
Probing the fine structure of ocean sound‐scattering layers with ROVERSE technology |
title_fullStr |
Probing the fine structure of ocean sound‐scattering layers with ROVERSE technology |
title_full_unstemmed |
Probing the fine structure of ocean sound‐scattering layers with ROVERSE technology |
title_sort |
probing the fine structure of ocean sound‐scattering layers with roverse technology |
publisher |
Wiley |
publishDate |
1991 |
url |
http://dx.doi.org/10.4319/lo.1991.36.1.0193 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.1991.36.1.0193 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.1991.36.1.0193 |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean North Atlantic Zooplankton |
genre_facet |
Arctic Arctic Ocean North Atlantic Zooplankton |
op_source |
Limnology and Oceanography volume 36, issue 1, page 193-204 ISSN 0024-3590 1939-5590 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.4319/lo.1991.36.1.0193 |
container_title |
Limnology and Oceanography |
container_volume |
36 |
container_issue |
1 |
container_start_page |
193 |
op_container_end_page |
204 |
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1784263320912527360 |