Quantifying the effects of background concentrations of crude oil pollution on sea ice albedo

The albedo response of three different types of bare sea ice (melting, first-year, and multi-year sea ice) are calculated at increasing mass ratios (0–1000ng g−1) of crude oil by using a coupled atmosphere–sea ice radiative-transfer model (TUV-snow) over the optical wavelengths 400–700 nm. The diffe...

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Main Authors: Redmond Roche, B., King, M.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017558
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5017558 2023-08-27T04:11:52+02:00 Quantifying the effects of background concentrations of crude oil pollution on sea ice albedo Redmond Roche, B. King, M. 2023 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017558 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-1981 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017558 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-1981 2023-08-06T23:41:22Z The albedo response of three different types of bare sea ice (melting, first-year, and multi-year sea ice) are calculated at increasing mass ratios (0–1000ng g−1) of crude oil by using a coupled atmosphere–sea ice radiative-transfer model (TUV-snow) over the optical wavelengths 400–700 nm. The different types of quasi-infinite-thickness sea ice exhibit different albedo responses to oil pollution, with a 1000ng g−1 mass ratio of oil causing a decrease to 70.9% in multi-year sea ice, 47.2% in first-year sea ice, and 22.1% in melting sea ice relative to the unpolluted albedo at a wavelength of 400 nm. The thickness of the sea ice is also an important factor, with realistic-thickness sea ices exhibiting similar results, albeit with a weaker albedo response. The type of oil also significantly affects the response of sea ice albedo, with a relatively opaque and heavy crude oil (Romashkino oil) causing a significantly larger decrease in sea ice albedo than a relatively transparent light crude oil (Petrobaltic oil). The size of the oil droplets polluting the ice also plays a minor role in the albedo response, with weathered submicrometre droplets (0.05–0.5µm radius) of Romashkino oil being the most absorbing across the optical wavelengths considered. Therefore, this study demonstrates that low background concentrations of small submicrometre- to micrometre-sized oil droplets have a significant effect on the albedo of bare sea ice. All three types of sea ice are sensitive to oil pollution; however, first-year sea ice and particularly melting sea ice are very sensitive to oil pollution. Conference Object Sea ice GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description The albedo response of three different types of bare sea ice (melting, first-year, and multi-year sea ice) are calculated at increasing mass ratios (0–1000ng g−1) of crude oil by using a coupled atmosphere–sea ice radiative-transfer model (TUV-snow) over the optical wavelengths 400–700 nm. The different types of quasi-infinite-thickness sea ice exhibit different albedo responses to oil pollution, with a 1000ng g−1 mass ratio of oil causing a decrease to 70.9% in multi-year sea ice, 47.2% in first-year sea ice, and 22.1% in melting sea ice relative to the unpolluted albedo at a wavelength of 400 nm. The thickness of the sea ice is also an important factor, with realistic-thickness sea ices exhibiting similar results, albeit with a weaker albedo response. The type of oil also significantly affects the response of sea ice albedo, with a relatively opaque and heavy crude oil (Romashkino oil) causing a significantly larger decrease in sea ice albedo than a relatively transparent light crude oil (Petrobaltic oil). The size of the oil droplets polluting the ice also plays a minor role in the albedo response, with weathered submicrometre droplets (0.05–0.5µm radius) of Romashkino oil being the most absorbing across the optical wavelengths considered. Therefore, this study demonstrates that low background concentrations of small submicrometre- to micrometre-sized oil droplets have a significant effect on the albedo of bare sea ice. All three types of sea ice are sensitive to oil pollution; however, first-year sea ice and particularly melting sea ice are very sensitive to oil pollution.
format Conference Object
author Redmond Roche, B.
King, M.
spellingShingle Redmond Roche, B.
King, M.
Quantifying the effects of background concentrations of crude oil pollution on sea ice albedo
author_facet Redmond Roche, B.
King, M.
author_sort Redmond Roche, B.
title Quantifying the effects of background concentrations of crude oil pollution on sea ice albedo
title_short Quantifying the effects of background concentrations of crude oil pollution on sea ice albedo
title_full Quantifying the effects of background concentrations of crude oil pollution on sea ice albedo
title_fullStr Quantifying the effects of background concentrations of crude oil pollution on sea ice albedo
title_full_unstemmed Quantifying the effects of background concentrations of crude oil pollution on sea ice albedo
title_sort quantifying the effects of background concentrations of crude oil pollution on sea ice albedo
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017558
genre Sea ice
genre_facet Sea ice
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-1981
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017558
op_doi https://doi.org/10.57757/IUGG23-1981
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