Physical processes driving phytoplankton production around Southampton Island, Nunavut in late summer 2018 and 2019

Climate change impacts have brought up the need for a better understanding of the rapidly changing ecosystem of the Arctic. Arctic marine ecosystems, such as around Southampton Island in Hudson Bay, are supported by phytoplankton production. In turn, phytoplankton production, which is influenced by...

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Bibliographic Details
Main Author: Kitching, Elizabeth
Other Authors: Mundy, C.J., Michel, Christine, Higgins, Scott (Environment and Geography), Kuzyk, Zou Zou (Earth Sciences)
Format: Master Thesis
Language:English
Published: 2022
Subjects:
Online Access:http://hdl.handle.net/1993/36865
id ftunivmanitoba:oai:mspace.lib.umanitoba.ca:1993/36865
record_format openpolar
spelling ftunivmanitoba:oai:mspace.lib.umanitoba.ca:1993/36865 2023-06-18T03:39:01+02:00 Physical processes driving phytoplankton production around Southampton Island, Nunavut in late summer 2018 and 2019 Kitching, Elizabeth Mundy, C.J. Michel, Christine Higgins, Scott (Environment and Geography) Kuzyk, Zou Zou (Earth Sciences) 2022-08-01T02:11:33Z application/pdf http://hdl.handle.net/1993/36865 eng eng http://hdl.handle.net/1993/36865 open access Southampton Island Phytoplankton production phytoplankton bloom Hudson Bay P-E curve master thesis 2022 ftunivmanitoba 2023-06-04T17:43:57Z Climate change impacts have brought up the need for a better understanding of the rapidly changing ecosystem of the Arctic. Arctic marine ecosystems, such as around Southampton Island in Hudson Bay, are supported by phytoplankton production. In turn, phytoplankton production, which is influenced by environmental conditions and processes, can impact pelagic and benthic food webs. The goal of this thesis was to determine the physical processes driving phytoplankton production around Southampton Island, Nunavut during summer. Three subgroups of differing physical characteristics of the water column were distinguished: the Northwest Narrows group (well-mixed water connecting Roes Welcome Sound and Frozen Strait), the Hudson Bay group (warmer stratified waters to the south of Southampton Island), and the Foxe group (colder stratified northeastern waters in Foxe Basin and Foxe Channel). The different physical characteristics resulted in contrasting phytoplankton production and phytoplankton bloom stages around the island. In particular, a highly productive phytoplankton bloom supported by mixing and high nutrient availability, was observed in the Northwest Narrows group. Phytoplankton production estimates in the Northwest Narrows group were higher than estimates for Hudson Bay and Foxe Basin, and comparable to those in Hudson Strait. The substantial variability phytoplankton production around Southampton Island highlights the importance of local processes for primary production in the Arctic. This also calls to the necessity for future work to identify similar regions that have the potential to support high phytoplankton production in the Arctic. October 2022 Master Thesis Arctic Climate change Foxe Basin Foxe Channel Frozen Strait Hudson Bay Hudson Strait Nunavut Phytoplankton Roes Welcome Sound Southampton Island MSpace at the University of Manitoba Arctic Foxe Basin ENVELOPE(-77.918,-77.918,65.931,65.931) Foxe Channel ENVELOPE(-79.999,-79.999,65.001,65.001) Frozen Strait ENVELOPE(-84.332,-84.332,65.751,65.751) Hudson Hudson Bay Hudson Strait ENVELOPE(-70.000,-70.000,62.000,62.000) Nunavut Roes Welcome Sound ENVELOPE(-86.666,-86.666,65.018,65.018) Southampton Island ENVELOPE(-84.501,-84.501,64.463,64.463)
institution Open Polar
collection MSpace at the University of Manitoba
op_collection_id ftunivmanitoba
language English
topic Southampton Island
Phytoplankton production
phytoplankton bloom
Hudson Bay
P-E curve
spellingShingle Southampton Island
Phytoplankton production
phytoplankton bloom
Hudson Bay
P-E curve
Kitching, Elizabeth
Physical processes driving phytoplankton production around Southampton Island, Nunavut in late summer 2018 and 2019
topic_facet Southampton Island
Phytoplankton production
phytoplankton bloom
Hudson Bay
P-E curve
description Climate change impacts have brought up the need for a better understanding of the rapidly changing ecosystem of the Arctic. Arctic marine ecosystems, such as around Southampton Island in Hudson Bay, are supported by phytoplankton production. In turn, phytoplankton production, which is influenced by environmental conditions and processes, can impact pelagic and benthic food webs. The goal of this thesis was to determine the physical processes driving phytoplankton production around Southampton Island, Nunavut during summer. Three subgroups of differing physical characteristics of the water column were distinguished: the Northwest Narrows group (well-mixed water connecting Roes Welcome Sound and Frozen Strait), the Hudson Bay group (warmer stratified waters to the south of Southampton Island), and the Foxe group (colder stratified northeastern waters in Foxe Basin and Foxe Channel). The different physical characteristics resulted in contrasting phytoplankton production and phytoplankton bloom stages around the island. In particular, a highly productive phytoplankton bloom supported by mixing and high nutrient availability, was observed in the Northwest Narrows group. Phytoplankton production estimates in the Northwest Narrows group were higher than estimates for Hudson Bay and Foxe Basin, and comparable to those in Hudson Strait. The substantial variability phytoplankton production around Southampton Island highlights the importance of local processes for primary production in the Arctic. This also calls to the necessity for future work to identify similar regions that have the potential to support high phytoplankton production in the Arctic. October 2022
author2 Mundy, C.J.
Michel, Christine
Higgins, Scott (Environment and Geography)
Kuzyk, Zou Zou (Earth Sciences)
format Master Thesis
author Kitching, Elizabeth
author_facet Kitching, Elizabeth
author_sort Kitching, Elizabeth
title Physical processes driving phytoplankton production around Southampton Island, Nunavut in late summer 2018 and 2019
title_short Physical processes driving phytoplankton production around Southampton Island, Nunavut in late summer 2018 and 2019
title_full Physical processes driving phytoplankton production around Southampton Island, Nunavut in late summer 2018 and 2019
title_fullStr Physical processes driving phytoplankton production around Southampton Island, Nunavut in late summer 2018 and 2019
title_full_unstemmed Physical processes driving phytoplankton production around Southampton Island, Nunavut in late summer 2018 and 2019
title_sort physical processes driving phytoplankton production around southampton island, nunavut in late summer 2018 and 2019
publishDate 2022
url http://hdl.handle.net/1993/36865
long_lat ENVELOPE(-77.918,-77.918,65.931,65.931)
ENVELOPE(-79.999,-79.999,65.001,65.001)
ENVELOPE(-84.332,-84.332,65.751,65.751)
ENVELOPE(-70.000,-70.000,62.000,62.000)
ENVELOPE(-86.666,-86.666,65.018,65.018)
ENVELOPE(-84.501,-84.501,64.463,64.463)
geographic Arctic
Foxe Basin
Foxe Channel
Frozen Strait
Hudson
Hudson Bay
Hudson Strait
Nunavut
Roes Welcome Sound
Southampton Island
geographic_facet Arctic
Foxe Basin
Foxe Channel
Frozen Strait
Hudson
Hudson Bay
Hudson Strait
Nunavut
Roes Welcome Sound
Southampton Island
genre Arctic
Climate change
Foxe Basin
Foxe Channel
Frozen Strait
Hudson Bay
Hudson Strait
Nunavut
Phytoplankton
Roes Welcome Sound
Southampton Island
genre_facet Arctic
Climate change
Foxe Basin
Foxe Channel
Frozen Strait
Hudson Bay
Hudson Strait
Nunavut
Phytoplankton
Roes Welcome Sound
Southampton Island
op_relation http://hdl.handle.net/1993/36865
op_rights open access
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