Evaluating and Improving Arctic Ozone Chemistry in an Atmospheric Model

The Arctic, though geographically remote, interests scientists because of the air-sea interactions that govern the composition of the atmosphere (Knepp et al. 2010). These interactions are strongly influenced by sea ice. Arctic sea ice extent is decreasing and at an accelerated rate. Between 1979 an...

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Other Authors: Confer, Kaitlyn (authoraut), Holmes, Christopher (authoraut)
Format: Bachelor Thesis
Language:English
Subjects:
Online Access:http://purl.flvc.org/fsu/fd/FSU_libsubv1_scholarship_submission_1556311545_bedb643f
http://fsu.digital.flvc.org/islandora/object/fsu%3A667651/datastream/TN/view/Evaluating%20and%20Improving%20Arctic%20Ozone%20Chemistry%20in%20an%20Atmospheric%20Model.jpg
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spelling ftfloridastunidc:oai:fsu.digital.flvc.org:fsu_667651 2023-05-15T14:40:07+02:00 Evaluating and Improving Arctic Ozone Chemistry in an Atmospheric Model Confer, Kaitlyn (authoraut) Holmes, Christopher (authoraut) 1 online resource computer application/pdf http://purl.flvc.org/fsu/fd/FSU_libsubv1_scholarship_submission_1556311545_bedb643f http://fsu.digital.flvc.org/islandora/object/fsu%3A667651/datastream/TN/view/Evaluating%20and%20Improving%20Arctic%20Ozone%20Chemistry%20in%20an%20Atmospheric%20Model.jpg English eng eng Text bachelor thesis ftfloridastunidc 2020-08-10T20:31:48Z The Arctic, though geographically remote, interests scientists because of the air-sea interactions that govern the composition of the atmosphere (Knepp et al. 2010). These interactions are strongly influenced by sea ice. Arctic sea ice extent is decreasing and at an accelerated rate. Between 1979 and 2006, it is estimated the sea ice extent at the end of the melting season decreased 9.1% per decade (Stroeve et al. 2007). These changes have large implications for global temperature, air-sea exchange fluxes, and atmospheric chemistry. Sea ice is a source of reactive halogens, particularly bromine radicals and changes to sea ice can therefore impact tropospheric ozone concentrations. We see these changes most abundantly during the springtime when reactive halogens like bromine monoxide (BrO) deplete ozone to near-zero levels. Ozone is the primary precursor to the atmospheric oxidizing agent – the hydroxyl radical (OH) – which removes harmful pollutants from the air. Thus, the loss of ozone can affect the oxidation capacity of the atmosphere. As climate changes, it is important to understand and predict the effects of changing sea ice on Arctic atmospheric chemistry. In this work, we assess the ability of a current global model, GEOS-Chem, to predict ozone and BrO concentrations over the Arctic Ocean compared to a new dataset of ozone and BrO concentrations collected over Arctic sea ice. We quantify the performance of two model versions and discuss the processes that might further improve the model. Atmospheric chemistry Bachelor Thesis Arctic Arctic Ocean Sea ice Florida State University Digital Library (FSUDL) Arctic Arctic Ocean
institution Open Polar
collection Florida State University Digital Library (FSUDL)
op_collection_id ftfloridastunidc
language English
description The Arctic, though geographically remote, interests scientists because of the air-sea interactions that govern the composition of the atmosphere (Knepp et al. 2010). These interactions are strongly influenced by sea ice. Arctic sea ice extent is decreasing and at an accelerated rate. Between 1979 and 2006, it is estimated the sea ice extent at the end of the melting season decreased 9.1% per decade (Stroeve et al. 2007). These changes have large implications for global temperature, air-sea exchange fluxes, and atmospheric chemistry. Sea ice is a source of reactive halogens, particularly bromine radicals and changes to sea ice can therefore impact tropospheric ozone concentrations. We see these changes most abundantly during the springtime when reactive halogens like bromine monoxide (BrO) deplete ozone to near-zero levels. Ozone is the primary precursor to the atmospheric oxidizing agent – the hydroxyl radical (OH) – which removes harmful pollutants from the air. Thus, the loss of ozone can affect the oxidation capacity of the atmosphere. As climate changes, it is important to understand and predict the effects of changing sea ice on Arctic atmospheric chemistry. In this work, we assess the ability of a current global model, GEOS-Chem, to predict ozone and BrO concentrations over the Arctic Ocean compared to a new dataset of ozone and BrO concentrations collected over Arctic sea ice. We quantify the performance of two model versions and discuss the processes that might further improve the model. Atmospheric chemistry
author2 Confer, Kaitlyn (authoraut)
Holmes, Christopher (authoraut)
format Bachelor Thesis
title Evaluating and Improving Arctic Ozone Chemistry in an Atmospheric Model
spellingShingle Evaluating and Improving Arctic Ozone Chemistry in an Atmospheric Model
title_short Evaluating and Improving Arctic Ozone Chemistry in an Atmospheric Model
title_full Evaluating and Improving Arctic Ozone Chemistry in an Atmospheric Model
title_fullStr Evaluating and Improving Arctic Ozone Chemistry in an Atmospheric Model
title_full_unstemmed Evaluating and Improving Arctic Ozone Chemistry in an Atmospheric Model
title_sort evaluating and improving arctic ozone chemistry in an atmospheric model
url http://purl.flvc.org/fsu/fd/FSU_libsubv1_scholarship_submission_1556311545_bedb643f
http://fsu.digital.flvc.org/islandora/object/fsu%3A667651/datastream/TN/view/Evaluating%20and%20Improving%20Arctic%20Ozone%20Chemistry%20in%20an%20Atmospheric%20Model.jpg
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Sea ice
genre_facet Arctic
Arctic Ocean
Sea ice
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