Measurement of Oil Slick Transport and Evolution in the Gulf of Mexico using L-band Synthetic Aperture Radar

Source at https://www.vde-verlag.de/proceedings-en/454636104.html The transport and evolution of a mineral oil slick originating at a seep in the Gulf of Mexico approximately 16 km offshore of the mouth of the Mississippi River is measured using a series of images acquired at 40 minute intervals wit...

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Main Authors: Jones, Cathleen, Espeseth, Martine, Holt, Benjamin, Brekke, Camilla
Format: Article in Journal/Newspaper
Language:English
Published: VDE Verlag 2018
Subjects:
Online Access:https://hdl.handle.net/10037/14586
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author Jones, Cathleen
Espeseth, Martine
Holt, Benjamin
Brekke, Camilla
author_facet Jones, Cathleen
Espeseth, Martine
Holt, Benjamin
Brekke, Camilla
author_sort Jones, Cathleen
collection University of Tromsø: Munin Open Research Archive
description Source at https://www.vde-verlag.de/proceedings-en/454636104.html The transport and evolution of a mineral oil slick originating at a seep in the Gulf of Mexico approximately 16 km offshore of the mouth of the Mississippi River is measured using a series of images acquired at 40 minute intervals with the Uninhabited Aerial Vehicle Synthetic Aperture Radar (UAVSAR), an L-band, high resolution, high signal-to-noise instrument operated by the U.S. National Aeronautics and Space Agency (NASA). A series of four images acquired over a 2-hour time period is used in the study. Both VV-intensity images and the VVintensity contrast between the slick and clean water (damping ratio) are used. The intensity images show the spatial development and transport of the slick within an area extending from the source northward to near the Louisiana (USA) coast. The slick initially spreads to the northeast from the origin site, then become entrained in an along-shore current. From there, the direction of transport changes by nearly 180º, and the oil from the slick moves west along a path much closer to the Louisiana shoreline. Concentration of the oil within the slick is observed along fronts and internal waves. The oil that remains on the surface the longest shows increasing damping, which could indicate the formation of more stable emulsions that can persist in the environment.
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spelling ftunivtroemsoe:oai:munin.uit.no:10037/14586 2025-04-13T14:11:25+00:00 Measurement of Oil Slick Transport and Evolution in the Gulf of Mexico using L-band Synthetic Aperture Radar Jones, Cathleen Espeseth, Martine Holt, Benjamin Brekke, Camilla 2018-06 https://hdl.handle.net/10037/14586 eng eng VDE Verlag Electronic proceedings (EUSAR) info:eu-repo/grantAgreement/RCN/SFI/237906/Norway/Centre for Integrated Remote Sensing and Forecasting for Arctic Operations/CIRFA/ FRIDAID 1621560 https://hdl.handle.net/10037/14586 openAccess VDP::Technology: 500::Rock and petroleum disciplines: 510 VDP::Teknologi: 500::Berg‑ og petroleumsfag: 510 VDP::Mathematics and natural science: 400::Information and communication science: 420::Security and vulnerability: 424 VDP::Matematikk og Naturvitenskap: 400::Informasjons- og kommunikasjonsvitenskap: 420::Sikkerhet og sårbarhet: 424 Journal article Tidsskriftartikkel 2018 ftunivtroemsoe 2025-03-14T05:17:56Z Source at https://www.vde-verlag.de/proceedings-en/454636104.html The transport and evolution of a mineral oil slick originating at a seep in the Gulf of Mexico approximately 16 km offshore of the mouth of the Mississippi River is measured using a series of images acquired at 40 minute intervals with the Uninhabited Aerial Vehicle Synthetic Aperture Radar (UAVSAR), an L-band, high resolution, high signal-to-noise instrument operated by the U.S. National Aeronautics and Space Agency (NASA). A series of four images acquired over a 2-hour time period is used in the study. Both VV-intensity images and the VVintensity contrast between the slick and clean water (damping ratio) are used. The intensity images show the spatial development and transport of the slick within an area extending from the source northward to near the Louisiana (USA) coast. The slick initially spreads to the northeast from the origin site, then become entrained in an along-shore current. From there, the direction of transport changes by nearly 180º, and the oil from the slick moves west along a path much closer to the Louisiana shoreline. Concentration of the oil within the slick is observed along fronts and internal waves. The oil that remains on the surface the longest shows increasing damping, which could indicate the formation of more stable emulsions that can persist in the environment. Article in Journal/Newspaper Arctic University of Tromsø: Munin Open Research Archive
spellingShingle VDP::Technology: 500::Rock and petroleum disciplines: 510
VDP::Teknologi: 500::Berg‑ og petroleumsfag: 510
VDP::Mathematics and natural science: 400::Information and communication science: 420::Security and vulnerability: 424
VDP::Matematikk og Naturvitenskap: 400::Informasjons- og kommunikasjonsvitenskap: 420::Sikkerhet og sårbarhet: 424
Jones, Cathleen
Espeseth, Martine
Holt, Benjamin
Brekke, Camilla
Measurement of Oil Slick Transport and Evolution in the Gulf of Mexico using L-band Synthetic Aperture Radar
title Measurement of Oil Slick Transport and Evolution in the Gulf of Mexico using L-band Synthetic Aperture Radar
title_full Measurement of Oil Slick Transport and Evolution in the Gulf of Mexico using L-band Synthetic Aperture Radar
title_fullStr Measurement of Oil Slick Transport and Evolution in the Gulf of Mexico using L-band Synthetic Aperture Radar
title_full_unstemmed Measurement of Oil Slick Transport and Evolution in the Gulf of Mexico using L-band Synthetic Aperture Radar
title_short Measurement of Oil Slick Transport and Evolution in the Gulf of Mexico using L-band Synthetic Aperture Radar
title_sort measurement of oil slick transport and evolution in the gulf of mexico using l-band synthetic aperture radar
topic VDP::Technology: 500::Rock and petroleum disciplines: 510
VDP::Teknologi: 500::Berg‑ og petroleumsfag: 510
VDP::Mathematics and natural science: 400::Information and communication science: 420::Security and vulnerability: 424
VDP::Matematikk og Naturvitenskap: 400::Informasjons- og kommunikasjonsvitenskap: 420::Sikkerhet og sårbarhet: 424
topic_facet VDP::Technology: 500::Rock and petroleum disciplines: 510
VDP::Teknologi: 500::Berg‑ og petroleumsfag: 510
VDP::Mathematics and natural science: 400::Information and communication science: 420::Security and vulnerability: 424
VDP::Matematikk og Naturvitenskap: 400::Informasjons- og kommunikasjonsvitenskap: 420::Sikkerhet og sårbarhet: 424
url https://hdl.handle.net/10037/14586