Impact of tidal dynamics on diel vertical migration of zooplankton in Hudson Bay

Hudson Bay is a large, seasonally-ice covered Canadian inland sea, connected to the Arctic Ocean and North Atlantic through Foxe Basin and Hudson Strait. This study investigates zooplankton distribution, dynamics and factors controlling them during open water and ice cover periods (from September 20...

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Main Authors: Petrusevich, Vladislav Y., Dmitrenko, Igor A., Niemi, Andrea, Kirillov, Sergey A., Kamula, Christina Michelle, Kuzyk, Zou Zou A., Barber, David G., Ehn, Jens K.
Format: Text
Language:English
Published: 2019
Subjects:
Online Access:https://doi.org/10.5194/os-2019-107
https://www.ocean-sci-discuss.net/os-2019-107/
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spelling ftcopernicus:oai:publications.copernicus.org:osd80486 2023-05-15T15:06:00+02:00 Impact of tidal dynamics on diel vertical migration of zooplankton in Hudson Bay Petrusevich, Vladislav Y. Dmitrenko, Igor A. Niemi, Andrea Kirillov, Sergey A. Kamula, Christina Michelle Kuzyk, Zou Zou A. Barber, David G. Ehn, Jens K. 2019-10-07 application/pdf https://doi.org/10.5194/os-2019-107 https://www.ocean-sci-discuss.net/os-2019-107/ eng eng doi:10.5194/os-2019-107 https://www.ocean-sci-discuss.net/os-2019-107/ eISSN: 1812-0792 Text 2019 ftcopernicus https://doi.org/10.5194/os-2019-107 2019-12-24T09:48:25Z Hudson Bay is a large, seasonally-ice covered Canadian inland sea, connected to the Arctic Ocean and North Atlantic through Foxe Basin and Hudson Strait. This study investigates zooplankton distribution, dynamics and factors controlling them during open water and ice cover periods (from September 2016 to October 2017) in Hudson Bay. A mooring equipped with two Acoustic Doppler Current Profilers (ADCP) and a sediment trap was deployed in September 2016 in Hudson Bay ~ 190 km north-east from the port of Churchill. The backscatter intensity and vertical velocity time series showed a pattern typical for the zooplankton diel vertical migration (DVM). Zooplankton collected by the sediment trap allowed for the identification of migrating scatters during the study period. From the acquired acoustic data we observed the interaction of DVM with multiple factors including lunar light, tides, as well as water and sea ice dynamics. Solar illuminance was the major factor determining migration pattern, but unlike at some other polar and sub-polar regions, moonlight had a little effect on DVM, while tidal dynamics is important. The presented data constitutes a first-ever observed presence of DVM in Hudson Bay during winter as well as its interaction with the tidal dynamics. Text Arctic Arctic Ocean Foxe Basin Hudson Bay Hudson Strait North Atlantic Sea ice Zooplankton Copernicus Publications: E-Journals Arctic Arctic Ocean Foxe Basin ENVELOPE(-77.918,-77.918,65.931,65.931) Hudson Hudson Bay Hudson Strait ENVELOPE(-70.000,-70.000,62.000,62.000)
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Hudson Bay is a large, seasonally-ice covered Canadian inland sea, connected to the Arctic Ocean and North Atlantic through Foxe Basin and Hudson Strait. This study investigates zooplankton distribution, dynamics and factors controlling them during open water and ice cover periods (from September 2016 to October 2017) in Hudson Bay. A mooring equipped with two Acoustic Doppler Current Profilers (ADCP) and a sediment trap was deployed in September 2016 in Hudson Bay ~ 190 km north-east from the port of Churchill. The backscatter intensity and vertical velocity time series showed a pattern typical for the zooplankton diel vertical migration (DVM). Zooplankton collected by the sediment trap allowed for the identification of migrating scatters during the study period. From the acquired acoustic data we observed the interaction of DVM with multiple factors including lunar light, tides, as well as water and sea ice dynamics. Solar illuminance was the major factor determining migration pattern, but unlike at some other polar and sub-polar regions, moonlight had a little effect on DVM, while tidal dynamics is important. The presented data constitutes a first-ever observed presence of DVM in Hudson Bay during winter as well as its interaction with the tidal dynamics.
format Text
author Petrusevich, Vladislav Y.
Dmitrenko, Igor A.
Niemi, Andrea
Kirillov, Sergey A.
Kamula, Christina Michelle
Kuzyk, Zou Zou A.
Barber, David G.
Ehn, Jens K.
spellingShingle Petrusevich, Vladislav Y.
Dmitrenko, Igor A.
Niemi, Andrea
Kirillov, Sergey A.
Kamula, Christina Michelle
Kuzyk, Zou Zou A.
Barber, David G.
Ehn, Jens K.
Impact of tidal dynamics on diel vertical migration of zooplankton in Hudson Bay
author_facet Petrusevich, Vladislav Y.
Dmitrenko, Igor A.
Niemi, Andrea
Kirillov, Sergey A.
Kamula, Christina Michelle
Kuzyk, Zou Zou A.
Barber, David G.
Ehn, Jens K.
author_sort Petrusevich, Vladislav Y.
title Impact of tidal dynamics on diel vertical migration of zooplankton in Hudson Bay
title_short Impact of tidal dynamics on diel vertical migration of zooplankton in Hudson Bay
title_full Impact of tidal dynamics on diel vertical migration of zooplankton in Hudson Bay
title_fullStr Impact of tidal dynamics on diel vertical migration of zooplankton in Hudson Bay
title_full_unstemmed Impact of tidal dynamics on diel vertical migration of zooplankton in Hudson Bay
title_sort impact of tidal dynamics on diel vertical migration of zooplankton in hudson bay
publishDate 2019
url https://doi.org/10.5194/os-2019-107
https://www.ocean-sci-discuss.net/os-2019-107/
long_lat ENVELOPE(-77.918,-77.918,65.931,65.931)
ENVELOPE(-70.000,-70.000,62.000,62.000)
geographic Arctic
Arctic Ocean
Foxe Basin
Hudson
Hudson Bay
Hudson Strait
geographic_facet Arctic
Arctic Ocean
Foxe Basin
Hudson
Hudson Bay
Hudson Strait
genre Arctic
Arctic Ocean
Foxe Basin
Hudson Bay
Hudson Strait
North Atlantic
Sea ice
Zooplankton
genre_facet Arctic
Arctic Ocean
Foxe Basin
Hudson Bay
Hudson Strait
North Atlantic
Sea ice
Zooplankton
op_source eISSN: 1812-0792
op_relation doi:10.5194/os-2019-107
https://www.ocean-sci-discuss.net/os-2019-107/
op_doi https://doi.org/10.5194/os-2019-107
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