Bottom melting of Arctic Sea Ice in the Nansen Basin due to Atlantic Water influence

The hydrographic situation for a region north of Svalbard is investigated using observations from the Norwegian Young Sea Ice Cruise (N-ICE2015). Observations from January to June 2015 are compared to historical observations with a particular focus on the warm and salty Atlantic Water (AW) entering...

Full description

Bibliographic Details
Main Author: Muilwijk, Morven Korneel
Format: Master Thesis
Language:English
Published: The University of Bergen 2016
Subjects:
CTD
PHC
Online Access:https://hdl.handle.net/1956/12661
id ftunivbergen:oai:bora.uib.no:1956/12661
record_format openpolar
spelling ftunivbergen:oai:bora.uib.no:1956/12661 2023-05-15T14:51:54+02:00 Bottom melting of Arctic Sea Ice in the Nansen Basin due to Atlantic Water influence Muilwijk, Morven Korneel 2016-05-24 13773691 bytes application/pdf https://hdl.handle.net/1956/12661 eng eng The University of Bergen https://hdl.handle.net/1956/12661 Copyright the Author. All rights reserved Atlantic water Oceanography Nansen Basin Arctic Sea Ice Lance Global warming Climate change Svalbard Hydrography ADCP CTD Mixed Layer N-ICE2015 Fram Bottom Melting PHC World Ocean Atlas AOTIM Circulation NorESM Model Ocean Nautilus Tides TEOS-10 Freshwater 756213 Master thesis 2016 ftunivbergen 2023-03-14T17:38:52Z The hydrographic situation for a region north of Svalbard is investigated using observations from the Norwegian Young Sea Ice Cruise (N-ICE2015). Observations from January to June 2015 are compared to historical observations with a particular focus on the warm and salty Atlantic Water (AW) entering the Arctic Ocean through the Fram Strait. Here we discuss how the AW has changed over time, what governs its characteristics, and how it might influence the sea ice cover. We find that AW characteristics north of Svalbard are mainly controlled by the distance along the inflow path, and by changes in inflowing AW temperature in the Fram Strait. AW characteristics north of Svalbard are also largely affected by local processes such as sea ice growth, melting and tidal induced mixing. Furthermore, one dimensional model results and observations show that AW has a direct impact on the sea ice cover north of Svalbard. Shallow and warm AW efficiently reduces sea ice growth and results in bottom melting throughout the whole year. The historical observations and outcome from a fully coupled earth system model show a warming trend of AW core temperature over the last few decades. We believe that the AW warming trend in the Arctic Ocean may be part of long term multi-decadal variability, which is influenced by anthropogenic forcing. Simulations suggest that approximately 30 % of the recent warming may be attributed to global warming. Master i Meteorologi og oseanografi MAMN-GEOF GEOF399 Master Thesis Arctic Arctic Ocean Climate change Fram Strait Global warming Nansen Basin Sea ice Svalbard University of Bergen: Bergen Open Research Archive (BORA-UiB) Arctic Arctic Ocean Nautilus ENVELOPE(-67.167,-67.167,-67.650,-67.650) Svalbard
institution Open Polar
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
op_collection_id ftunivbergen
language English
topic Atlantic water
Oceanography
Nansen Basin
Arctic Sea Ice
Lance
Global warming
Climate change
Svalbard
Hydrography
ADCP
CTD
Mixed Layer
N-ICE2015
Fram
Bottom Melting
PHC
World Ocean Atlas
AOTIM
Circulation
NorESM
Model Ocean
Nautilus
Tides
TEOS-10
Freshwater
756213
spellingShingle Atlantic water
Oceanography
Nansen Basin
Arctic Sea Ice
Lance
Global warming
Climate change
Svalbard
Hydrography
ADCP
CTD
Mixed Layer
N-ICE2015
Fram
Bottom Melting
PHC
World Ocean Atlas
AOTIM
Circulation
NorESM
Model Ocean
Nautilus
Tides
TEOS-10
Freshwater
756213
Muilwijk, Morven Korneel
Bottom melting of Arctic Sea Ice in the Nansen Basin due to Atlantic Water influence
topic_facet Atlantic water
Oceanography
Nansen Basin
Arctic Sea Ice
Lance
Global warming
Climate change
Svalbard
Hydrography
ADCP
CTD
Mixed Layer
N-ICE2015
Fram
Bottom Melting
PHC
World Ocean Atlas
AOTIM
Circulation
NorESM
Model Ocean
Nautilus
Tides
TEOS-10
Freshwater
756213
description The hydrographic situation for a region north of Svalbard is investigated using observations from the Norwegian Young Sea Ice Cruise (N-ICE2015). Observations from January to June 2015 are compared to historical observations with a particular focus on the warm and salty Atlantic Water (AW) entering the Arctic Ocean through the Fram Strait. Here we discuss how the AW has changed over time, what governs its characteristics, and how it might influence the sea ice cover. We find that AW characteristics north of Svalbard are mainly controlled by the distance along the inflow path, and by changes in inflowing AW temperature in the Fram Strait. AW characteristics north of Svalbard are also largely affected by local processes such as sea ice growth, melting and tidal induced mixing. Furthermore, one dimensional model results and observations show that AW has a direct impact on the sea ice cover north of Svalbard. Shallow and warm AW efficiently reduces sea ice growth and results in bottom melting throughout the whole year. The historical observations and outcome from a fully coupled earth system model show a warming trend of AW core temperature over the last few decades. We believe that the AW warming trend in the Arctic Ocean may be part of long term multi-decadal variability, which is influenced by anthropogenic forcing. Simulations suggest that approximately 30 % of the recent warming may be attributed to global warming. Master i Meteorologi og oseanografi MAMN-GEOF GEOF399
format Master Thesis
author Muilwijk, Morven Korneel
author_facet Muilwijk, Morven Korneel
author_sort Muilwijk, Morven Korneel
title Bottom melting of Arctic Sea Ice in the Nansen Basin due to Atlantic Water influence
title_short Bottom melting of Arctic Sea Ice in the Nansen Basin due to Atlantic Water influence
title_full Bottom melting of Arctic Sea Ice in the Nansen Basin due to Atlantic Water influence
title_fullStr Bottom melting of Arctic Sea Ice in the Nansen Basin due to Atlantic Water influence
title_full_unstemmed Bottom melting of Arctic Sea Ice in the Nansen Basin due to Atlantic Water influence
title_sort bottom melting of arctic sea ice in the nansen basin due to atlantic water influence
publisher The University of Bergen
publishDate 2016
url https://hdl.handle.net/1956/12661
long_lat ENVELOPE(-67.167,-67.167,-67.650,-67.650)
geographic Arctic
Arctic Ocean
Nautilus
Svalbard
geographic_facet Arctic
Arctic Ocean
Nautilus
Svalbard
genre Arctic
Arctic Ocean
Climate change
Fram Strait
Global warming
Nansen Basin
Sea ice
Svalbard
genre_facet Arctic
Arctic Ocean
Climate change
Fram Strait
Global warming
Nansen Basin
Sea ice
Svalbard
op_relation https://hdl.handle.net/1956/12661
op_rights Copyright the Author. All rights reserved
_version_ 1766323047110803456