Simulating the Oceanic Migration of Silver Japanese Eels.

The oceanic migration of silver Japanese eels starts from their continental growth habitats in East Asia and ends at the spawning area near the West Mariana Ridge seamount chain. However, the actual migration routes remain unknown. In this study, we examined the possible oceanic migration routes and...

Full description

Bibliographic Details
Main Authors: Yu-Lin Chang, Yasumasa Miyazawa, Mélanie Béguer-Pon
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2016-01-01
Series:PLoS ONE
Online Access:http://europepmc.org/articles/PMC4794164?pdf=render
_version_ 1819017641909551104
author Yu-Lin Chang
Yasumasa Miyazawa
Mélanie Béguer-Pon
author_facet Yu-Lin Chang
Yasumasa Miyazawa
Mélanie Béguer-Pon
author_sort Yu-Lin Chang
collection DOAJ
description The oceanic migration of silver Japanese eels starts from their continental growth habitats in East Asia and ends at the spawning area near the West Mariana Ridge seamount chain. However, the actual migration routes remain unknown. In this study, we examined the possible oceanic migration routes and strategies of silver Japanese eels using a particle tracking method in which virtual eels (v-eels) were programmed to move vertically and horizontally in an ocean circulation model (Japan Coastal Ocean Predictability Experiment 2, JCOPE2). Four horizontal swimming strategies were tested: random heading, true navigation (readjusted heading), orientation toward the spawning area (fixed heading), and swimming against the Kuroshio. We found that all strategies, except random swimming, allowed v-eels swimming at 0.65 m s-1 to reach the spawning area within eight months after their departure from the south coast of Japan (end of the spawning season). The estimated minimum swimming speed required to reach the area spawning within eight months was 0.1 m s-1 for true navigation, 0.12 m s-1 for constant compass heading, and 0.35 m s-1 for swimming against the Kuroshio. The lowest swimming speed estimated from tracked Japanese eels at sea was 0.03 m.s-1, which would not allow them to reach the spawning area within eight months, through any of the tested orientation strategies. Our numerical experiments also showed that ocean circulation significantly affected the migration of Japanese v-eels. A strong Kuroshio could advect v-eels further eastward. In addition, western Pacific ocean currents accelerated the migration of navigating v-eels. The migration duration was shortened in years with a stronger southward flow, contributed by a stronger recirculation south of Japan, an enhanced subtropical gyre, or a higher southward Kuroshio velocity.
first_indexed 2024-12-21T03:06:46Z
format Article
id doaj.art-bc86f076c8ad43e09c30232716872db8
institution Directory Open Access Journal
issn 1932-6203
language English
last_indexed 2024-12-21T03:06:46Z
publishDate 2016-01-01
publisher Public Library of Science (PLoS)
record_format Article
series PLoS ONE
spelling doaj.art-bc86f076c8ad43e09c30232716872db82022-12-21T19:18:05ZengPublic Library of Science (PLoS)PLoS ONE1932-62032016-01-01113e015018710.1371/journal.pone.0150187Simulating the Oceanic Migration of Silver Japanese Eels.Yu-Lin ChangYasumasa MiyazawaMélanie Béguer-PonThe oceanic migration of silver Japanese eels starts from their continental growth habitats in East Asia and ends at the spawning area near the West Mariana Ridge seamount chain. However, the actual migration routes remain unknown. In this study, we examined the possible oceanic migration routes and strategies of silver Japanese eels using a particle tracking method in which virtual eels (v-eels) were programmed to move vertically and horizontally in an ocean circulation model (Japan Coastal Ocean Predictability Experiment 2, JCOPE2). Four horizontal swimming strategies were tested: random heading, true navigation (readjusted heading), orientation toward the spawning area (fixed heading), and swimming against the Kuroshio. We found that all strategies, except random swimming, allowed v-eels swimming at 0.65 m s-1 to reach the spawning area within eight months after their departure from the south coast of Japan (end of the spawning season). The estimated minimum swimming speed required to reach the area spawning within eight months was 0.1 m s-1 for true navigation, 0.12 m s-1 for constant compass heading, and 0.35 m s-1 for swimming against the Kuroshio. The lowest swimming speed estimated from tracked Japanese eels at sea was 0.03 m.s-1, which would not allow them to reach the spawning area within eight months, through any of the tested orientation strategies. Our numerical experiments also showed that ocean circulation significantly affected the migration of Japanese v-eels. A strong Kuroshio could advect v-eels further eastward. In addition, western Pacific ocean currents accelerated the migration of navigating v-eels. The migration duration was shortened in years with a stronger southward flow, contributed by a stronger recirculation south of Japan, an enhanced subtropical gyre, or a higher southward Kuroshio velocity.http://europepmc.org/articles/PMC4794164?pdf=render
spellingShingle Yu-Lin Chang
Yasumasa Miyazawa
Mélanie Béguer-Pon
Simulating the Oceanic Migration of Silver Japanese Eels.
PLoS ONE
title Simulating the Oceanic Migration of Silver Japanese Eels.
title_full Simulating the Oceanic Migration of Silver Japanese Eels.
title_fullStr Simulating the Oceanic Migration of Silver Japanese Eels.
title_full_unstemmed Simulating the Oceanic Migration of Silver Japanese Eels.
title_short Simulating the Oceanic Migration of Silver Japanese Eels.
title_sort simulating the oceanic migration of silver japanese eels
url http://europepmc.org/articles/PMC4794164?pdf=render
work_keys_str_mv AT yulinchang simulatingtheoceanicmigrationofsilverjapaneseeels
AT yasumasamiyazawa simulatingtheoceanicmigrationofsilverjapaneseeels
AT melaniebeguerpon simulatingtheoceanicmigrationofsilverjapaneseeels