Ice and brine production in Hornsund

The Hornsund fjord system has been studied using observations of the atmosphere, ocean and sea ice, and two different types of models. The study documents significant year to year variability in sea ice formation and brine release in the fjord over the period 1978 - 2014, production of brine enriche...

Full description

Bibliographic Details
Main Author: Arntsen, Martin
Format: Master Thesis
Language:English
Published: The University of Bergen 2015
Subjects:
Online Access:https://hdl.handle.net/1956/10419
id ftunivbergen:oai:bora.uib.no:1956/10419
record_format openpolar
spelling ftunivbergen:oai:bora.uib.no:1956/10419 2023-05-15T16:34:56+02:00 Ice and brine production in Hornsund Arntsen, Martin 2015-06-02 14165974 bytes application/pdf https://hdl.handle.net/1956/10419 eng eng The University of Bergen https://hdl.handle.net/1956/10419 Copyright the Author. All rights reserved 756213 Master thesis 2015 ftunivbergen 2023-03-14T17:42:18Z The Hornsund fjord system has been studied using observations of the atmosphere, ocean and sea ice, and two different types of models. The study documents significant year to year variability in sea ice formation and brine release in the fjord over the period 1978 - 2014, production of brine enriched winter water, and inflow of warmer Atlantic water in recent years. Salt production through brine release was investigated for the winter period between 1978 and 2014 using a simple one-dimensional polynya model forced with observed wind and air temperatures. Results show that easterly winds dominate in winter, often accom- panied by cold air temperature. This favour high ice production as open water is often exposed to the cold air due to the development of a polynya in the fjord. The yearly ac- cumulated heat exchange over open water is the main driver of the year to year variations in ice production. The effect of a fast ice cover restricting the polynya activity is included for the years 2006 - 2014, and results show that this reduces the magnitude in the year to year dif- ferences in salt production. This is a result of higher fast ice coverage in years of high polynya activity. In later years (2012-2014) indications of a warmer inflow is seen in the hydrographic observations, and in 2013 came into contact with the Brine enriched winter water that is trapped at depth behind the sill. The warm water will likely contribute to melting of the tide water glaciers in the fjord. Simulations using the Regional Ocean Model System (ROMS) are presented and evalu- ated towards observed hydrography and satellite observations of the ice cover. Simulations cover the period 2005- 2010 and show that inflow events generally warm the lower layer in the inner parts of the fjord before the onset of freezing. Master i Meteorologi og oseanografi MAMN-GEOF GEOF399 Master Thesis Hornsund Sea ice University of Bergen: Bergen Open Research Archive (BORA-UiB) Hornsund ENVELOPE(15.865,15.865,76.979,76.979)
institution Open Polar
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
op_collection_id ftunivbergen
language English
topic 756213
spellingShingle 756213
Arntsen, Martin
Ice and brine production in Hornsund
topic_facet 756213
description The Hornsund fjord system has been studied using observations of the atmosphere, ocean and sea ice, and two different types of models. The study documents significant year to year variability in sea ice formation and brine release in the fjord over the period 1978 - 2014, production of brine enriched winter water, and inflow of warmer Atlantic water in recent years. Salt production through brine release was investigated for the winter period between 1978 and 2014 using a simple one-dimensional polynya model forced with observed wind and air temperatures. Results show that easterly winds dominate in winter, often accom- panied by cold air temperature. This favour high ice production as open water is often exposed to the cold air due to the development of a polynya in the fjord. The yearly ac- cumulated heat exchange over open water is the main driver of the year to year variations in ice production. The effect of a fast ice cover restricting the polynya activity is included for the years 2006 - 2014, and results show that this reduces the magnitude in the year to year dif- ferences in salt production. This is a result of higher fast ice coverage in years of high polynya activity. In later years (2012-2014) indications of a warmer inflow is seen in the hydrographic observations, and in 2013 came into contact with the Brine enriched winter water that is trapped at depth behind the sill. The warm water will likely contribute to melting of the tide water glaciers in the fjord. Simulations using the Regional Ocean Model System (ROMS) are presented and evalu- ated towards observed hydrography and satellite observations of the ice cover. Simulations cover the period 2005- 2010 and show that inflow events generally warm the lower layer in the inner parts of the fjord before the onset of freezing. Master i Meteorologi og oseanografi MAMN-GEOF GEOF399
format Master Thesis
author Arntsen, Martin
author_facet Arntsen, Martin
author_sort Arntsen, Martin
title Ice and brine production in Hornsund
title_short Ice and brine production in Hornsund
title_full Ice and brine production in Hornsund
title_fullStr Ice and brine production in Hornsund
title_full_unstemmed Ice and brine production in Hornsund
title_sort ice and brine production in hornsund
publisher The University of Bergen
publishDate 2015
url https://hdl.handle.net/1956/10419
long_lat ENVELOPE(15.865,15.865,76.979,76.979)
geographic Hornsund
geographic_facet Hornsund
genre Hornsund
Sea ice
genre_facet Hornsund
Sea ice
op_relation https://hdl.handle.net/1956/10419
op_rights Copyright the Author. All rights reserved
_version_ 1766025047133126656