MODELING THE DISTRIBUTION OF FISH SCHOOLS IN THE BERING SEA: MORPHOLOGICAL SCHOOL IDENTIFICATION
In this paper we demonstrate how fish schools can be automatically identified from acoustic backscatter data using a simple morphological and threshold algorithm. The algorithm includes: 1) seabed identification and removal; 2) bubble layer removal; 3) choosing a threshold for fish backscatter and s...
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crwiley:10.1111/j.1939-7445.1994.tb00180.x 2023-12-03T10:20:22+01:00 MODELING THE DISTRIBUTION OF FISH SCHOOLS IN THE BERING SEA: MORPHOLOGICAL SCHOOL IDENTIFICATION Swartzman, Gordon Stuetzle, Werner Kulman, Kristin Wen, Nuan 1994 http://dx.doi.org/10.1111/j.1939-7445.1994.tb00180.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1939-7445.1994.tb00180.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1939-7445.1994.tb00180.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Natural Resource Modeling volume 8, issue 2, page 177-194 ISSN 0890-8575 1939-7445 Environmental Science (miscellaneous) Modeling and Simulation journal-article 1994 crwiley https://doi.org/10.1111/j.1939-7445.1994.tb00180.x 2023-11-09T14:14:58Z In this paper we demonstrate how fish schools can be automatically identified from acoustic backscatter data using a simple morphological and threshold algorithm. The algorithm includes: 1) seabed identification and removal; 2) bubble layer removal; 3) choosing a threshold for fish backscatter and setting all pixels below it to 0; and 4) identifying the school boundaries and smoothing the images by using morphological operations. We compared the school sizes and boundaries found by using our algorithms with those found by experts to evaluate our choice of threshold, structuring element and morphological operations. Results showed two classes of images. The algorithm performed well for images having distinct, well defined fish schools. Images having more amorphous aggregations showed significant disparity between the algorithm and experts' choice. Differences appear to involve separating higher intensity aggregations from surrounding lower intensity aggregations. In these cases, the algorithm provides a more consistent and arguably more accurate estimate than the experts. The shoal image data is translated, via a connected‐surface‐identifier algorithm into a table of information about shoal size, shape and location that allows further analysis of the shoal information with a much smaller data set than the original acoustic images. Such analysis can lead to observing patterns in fish shoal distribution and its relationship to environmental factors and to point‐process tests for randomness at different spatial scales which, in turn, allows stochastic modeling of the schooling process. These topics will be presented in subsequent papers. Article in Journal/Newspaper Bering Sea Wiley Online Library (via Crossref) Bering Sea Natural Resource Modeling 8 2 177 194 |
institution |
Open Polar |
collection |
Wiley Online Library (via Crossref) |
op_collection_id |
crwiley |
language |
English |
topic |
Environmental Science (miscellaneous) Modeling and Simulation |
spellingShingle |
Environmental Science (miscellaneous) Modeling and Simulation Swartzman, Gordon Stuetzle, Werner Kulman, Kristin Wen, Nuan MODELING THE DISTRIBUTION OF FISH SCHOOLS IN THE BERING SEA: MORPHOLOGICAL SCHOOL IDENTIFICATION |
topic_facet |
Environmental Science (miscellaneous) Modeling and Simulation |
description |
In this paper we demonstrate how fish schools can be automatically identified from acoustic backscatter data using a simple morphological and threshold algorithm. The algorithm includes: 1) seabed identification and removal; 2) bubble layer removal; 3) choosing a threshold for fish backscatter and setting all pixels below it to 0; and 4) identifying the school boundaries and smoothing the images by using morphological operations. We compared the school sizes and boundaries found by using our algorithms with those found by experts to evaluate our choice of threshold, structuring element and morphological operations. Results showed two classes of images. The algorithm performed well for images having distinct, well defined fish schools. Images having more amorphous aggregations showed significant disparity between the algorithm and experts' choice. Differences appear to involve separating higher intensity aggregations from surrounding lower intensity aggregations. In these cases, the algorithm provides a more consistent and arguably more accurate estimate than the experts. The shoal image data is translated, via a connected‐surface‐identifier algorithm into a table of information about shoal size, shape and location that allows further analysis of the shoal information with a much smaller data set than the original acoustic images. Such analysis can lead to observing patterns in fish shoal distribution and its relationship to environmental factors and to point‐process tests for randomness at different spatial scales which, in turn, allows stochastic modeling of the schooling process. These topics will be presented in subsequent papers. |
format |
Article in Journal/Newspaper |
author |
Swartzman, Gordon Stuetzle, Werner Kulman, Kristin Wen, Nuan |
author_facet |
Swartzman, Gordon Stuetzle, Werner Kulman, Kristin Wen, Nuan |
author_sort |
Swartzman, Gordon |
title |
MODELING THE DISTRIBUTION OF FISH SCHOOLS IN THE BERING SEA: MORPHOLOGICAL SCHOOL IDENTIFICATION |
title_short |
MODELING THE DISTRIBUTION OF FISH SCHOOLS IN THE BERING SEA: MORPHOLOGICAL SCHOOL IDENTIFICATION |
title_full |
MODELING THE DISTRIBUTION OF FISH SCHOOLS IN THE BERING SEA: MORPHOLOGICAL SCHOOL IDENTIFICATION |
title_fullStr |
MODELING THE DISTRIBUTION OF FISH SCHOOLS IN THE BERING SEA: MORPHOLOGICAL SCHOOL IDENTIFICATION |
title_full_unstemmed |
MODELING THE DISTRIBUTION OF FISH SCHOOLS IN THE BERING SEA: MORPHOLOGICAL SCHOOL IDENTIFICATION |
title_sort |
modeling the distribution of fish schools in the bering sea: morphological school identification |
publisher |
Wiley |
publishDate |
1994 |
url |
http://dx.doi.org/10.1111/j.1939-7445.1994.tb00180.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1939-7445.1994.tb00180.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1939-7445.1994.tb00180.x |
geographic |
Bering Sea |
geographic_facet |
Bering Sea |
genre |
Bering Sea |
genre_facet |
Bering Sea |
op_source |
Natural Resource Modeling volume 8, issue 2, page 177-194 ISSN 0890-8575 1939-7445 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/j.1939-7445.1994.tb00180.x |
container_title |
Natural Resource Modeling |
container_volume |
8 |
container_issue |
2 |
container_start_page |
177 |
op_container_end_page |
194 |
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1784267796357578752 |