DEMOSS - European Space Agencyearth.esa.int/seasar2008/participants/301/pres_301... · 2018. 5....

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DEMOSS Title: Development of Marine Oil Spills/slicks Satellite monitoring System elements for the Black Sea, Caspian Sea and /Kara/Barents Seas INTAS Thematic Call on Earth Sciences and Environment in co- operation with with ESA, 2006 by Stein Sandven 1 , Vladimir Kudriavtsev 2 and Vladimir Malinovsky 3 1 NERSC, Bergen, Norway 2 NIERSC, St. Petersburg, Russia 3 MHI, Sevastopol, Ukraine With contribution form the other DEMOSSS partners

Transcript of DEMOSS - European Space Agencyearth.esa.int/seasar2008/participants/301/pres_301... · 2018. 5....

  • DEMOSSTitle: Development of Marine Oil Spills/slicks Satellite monitoring System elements for the Black Sea, Caspian Sea and /Kara/Barents Seas

    INTAS Thematic Call on Earth Sciences and Environment in co-operation with with ESA, 2006

    byStein Sandven1, Vladimir Kudriavtsev2 and Vladimir Malinovsky3

    1NERSC, Bergen, Norway2NIERSC, St. Petersburg, Russia

    3MHI, Sevastopol, UkraineWith contribution form the other DEMOSSS partners

  • Partners1. Nansen Environmental and Remote Sensing Center (NERSC),

    Norway2. BOOST Technologies, Brest, France3. University of Hamburg, Hamburg, Germany4. Nansen International Environmental and Remote Sensing Center

    (NIERSC), St.Petersburg, Russia5. Institute of Applied Physics Russian Academy of Sciences (IAP),

    Nizhny Novgorod, Russia6. Marine Hydrophysical Institute of the Ukrainian National Academy

    of Sciences, Sevastopol, Ukraine7. Arctic and Antarctic Research Institute (AARI), St.Petersburg,

    Russia8. Research Center for Earth Operative Monitoring (NTs OMZ),

    Moscow, Russia

  • Project Objectives

    • To develop and demonstrate components of a marine oil spill detection and prediction system based on satellite SAR and other space data in combination with models for oil slick/spill monitoring and prediction

  • Overview of Tasks

    Satellite monitoring of selected areas:* Barents/Kara Sea, NIERSC* Black Sea, MHI* Caspian Sea, NTsOMZand validation of oil slick detection, BOOST

    Task 4

    Radar Imaging Model Development, NIERSCTask 2Algorithm for detection & quantification of oil spills and look-alikes, NIERSC

    Task 3

    Task 5

    Task 1

    Oil spill modelling and drift forecasting, AARI

    Field experiment with oil slicks in the Black Sea, IAP/MHI

  • SAR acquisition of the study areas1 2

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    The Barents Sea (1) and Kara Sea (2) are relatively clean areas with little ship traffic and offshore exploration has just started. The areas are expected to become much more exposed to oil pollution in the future.

    The Black Sea (3) and the Caspian Sea (4) have already significant tanker traffic and offshore exploitation has started from several platforms

    WSM: 38APM: 1IMM: 52

    91Caspian

    WSM: 58APM: 38IMM: 86

    182Black

    WSM: 276APM: 3IMM: 168

    447Kara

    WSM: 131APM: 12IMM: 240

    383Barents

    DetailsTotal*Region

    * Number of image obtained from ESA rolling archive from May to December 2007. In addition, archived data from earlier years are available for the studies.

  • Radar scattering modelling

    DEMOSSS develops an improved model of radar scattering from a sea surface covered by oil and biogenic films to be used in detection and classification of surface film in SAR images

    Flow diagram of the radar scatter model for simulation of a given surface condition

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    u10=6m/sOLEE=0.022

    OmniDirectional Up−Wind Direction

    Wind Waves Spectrum and Effect of Thin OLE Film

    Oleic adic (OLE): monomolecular film

  • Backscatter from clean and film-covered water in tank experiments (inc. angle 30°)

    • Blue dots: observed backscatter from clean water• Blue circles: observed backscatter from oil films (also triangles and crosses)• Blue line: modelled backscatter from clean surface• Green line: modelled backscatter from surface film

    (Ref. Gade at el.,JGR 1998, Kudriavtsev et al, JGR, 2005)

  • Spectral Contrasts for different surface films: Comparison of models with data

    Wavenumber k, rad/cm

    Data from tank experiments (Ermakov et al.)

    OLE

    Vegetable oil

    Crude oil

    Diesel oil

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    OLE E=0.022

    VO E=0.012

    CO E=0.004

    Contrast between wind wave spectrum for clean water and different surface films

    Model simulations

  • Effective Oil Film ViscosityExperimental estimates by Ermakov et al. vs. Jacobs and Jenkins (1997) model

    Wave damping coefficients as function of film thickness

    Oil thickness in mm Oil thickness in mm

    15 Hz waves 25 Hz waves

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    C−bandθ=200u

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    X−bandθ=200u

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    C−bandθ=200u

    10=10m/s

    X−bandθ=200u

    10=10m/s

    Up-wind Radar contrasts vs. oil film thicknessat C- and X-band

  • Analysis of oil spill signatures in SAR images

    NRCS

    Incidence angle

    direction

    Wind speed

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    ontr

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    Comparison of observed (from SAR archive) and modelled C-band backscatter contrasts in oil spill signatures

  • Simulated NRCS field (in dB) for an eddy current field in presence of surfactants. Wind speed (a) 5 m/s and (b) 15 m/s. Radar geometry is for ERS SAR.

    Modelled backscatter of surfactants in an eddy

  • Field experiment from an offshore tower in the Black Sea

    Optical system to measure short wave spectrum and surface mean slope

    Video system to measure wave breaking characteristics

  • Optical Spectrum Analyzer

    X-band radar

    Ka-band radar

  • OLO (11:55)Periodic Natural slicks

    250º2 - 4 m/s?70º06.10.07, 10:02

    VO (12:22)Natural slick (12:30)

    OLO (12:44) DA (13:00)VO (13:39) VO (15:39)VO (15:50) DA (16:09)

    OLO (16:23) VO (16:23)

    270º2-4 m/s?0º - 5º05.10.07, 10:28

    Natural slick (17:17)330º1-3 m/s150º04.10.07, 15:46

    Natural slick (12:37)300º0-2 m/s120º04.10.07, 10:34

    Natural slick (15:50)Natural slick (16:03)

    OLO (16:09)Natural slick (16:14)

    280º1-2 m/s110º03.10.07, 15:46

    Natural slick (12:00)Natural slick (12:42)Natural slick (12:54)

    Natural slick (12:59) + VONatural slick (13:13)

    OLO (13:43)

    270º0 m/s1-2 m/s2 -3 m/s

    No wind107º

    (11:43)90º

    (12:28)

    03.10.07, 10:27

    Natural slick (17:12)DF (17:14)

    270º2.5m/s?90º (E)02.10.07, 16:47

    VO (13:03)VO (14:15)

    OLO (15:07)

    260º0 m/s

  • Contrasts in slicks observed on 05 Oct 2007

    Dodecyl alcohol slick (film elasticity E=50-70 mN/m)

    Vegetable oil slick (film elasticity E=12-15 mN/m)

    Wind velocity 2-4 m/s

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  • SAR observation of experimental oil spills

  • NRCS profile across a slick observed in ASAR APP data

    Results from SAR analysis of AP images form 2003:

    The largest slick has a contrast of about 15 dB compared to the surrounding clean water

  • Subset of ENVISAT ASAR AP image on 23 August 2003 off Novorossisk coast:

    (a) VV-pol

    (b) HH-pol

    (c) Pol ratio (PR)

    For clean seas PR is defined by contribution of bragg scattering and wave breaking, with typical value of 5 for this inc angle. In slicks bragg waves disappear and PR becomes close to 1

    Another slick observation in SAR APP image

  • Distribution of oil spills in the Black Sea derived from 68 SAR images

    SAR images from ERS-2 and ENVISAT were analyzed for a period of three years (2001 - 2004), resulting in 68 images with 424 likely oil spill events.

    The distribution of the spills are concentrated along the main shipping lanes and in the offshore drilling area in the western Black Sea

  • Example from the Caspian Sea

    • The ASAR Wideswath image from 04 July 2007 covers most of the Caspian Sea (left figure). A subset of the image (above) was analyzed for the area off Baku (red circle) where a spill event could be detected. The SARTool provided by BOOST Technologies was used to detect and quantify the oil spill area.

  • Oil spill event Kerch Strait 11 November 2007

    C-band: RADARSAT X-band: TerraSAR L-band: ALOS PALSAR

    Images obtained 16 November - > case study for model comparison

    Courtesy: Scanex Courtesy: DLR

  • Comparison with previous SIR-C/X SAR dataand field experiments

  • Oil drift modellingoil spill locationoil spill volume and spill rateoil propertiesfractional composition of the oil

    Oil spill input

    currentswindwind wavesthermohaline structurebathymetryice conditions

    advectionturbulent diffusionevaporationemulsificationdispersionphoto-oxidationbio-oxidation

    Oil slick spatial distributionOil mass balance

    spreading of the spillets

    advectionevaporation

    Oil spill simulation

    Oil spill output

    Sea state input

    AARI is developing an oil drift model, OilMARS, based on the components shown in the diagram. The model has been tested in the Barents and Kara Seas.

  • Oil spill modelling in Kara Sea: open water• AARI uses its oil

    spill model OilMARS to simulate oil drift in the Kara Sea. The figures show the spreading of a spill over a period of 20 days. The red area indicate where oil reached the coast and caused pollution at the beach.

  • Oil spill modelling in Kara Sea: sea ice waters• AARI uses its oil spill

    model Oilmars to simulate oil drift in the Kara Sea. The figures show the spreading of a spill over a period of 20 days in winter when the sea ice ice-covered. Black indicates oil spill in open water, blue indicate oil spill on top of th eice and red is oil spill under the ice.

  • Summary and further work• Radar scattering modelling tools is ready for use• Field experiments with artificial oil spills at the tower in the Black Sea were

    performed in 2007, more experiments are planned in 2008• Lab experiments with radar observation of wave damping by various oil

    types have been conducted• Build-up of SAR data base for the study regions have started, primarily

    with ASAR data. Will be supplemented by other SAR data (X- and L-band)• Analysis of SAR data for slick and other ocean surface features, including

    comparison with models has started• Verify hypothesis that PR can be used to identify oil and natural slicks and

    discriminate them from look-alikes• Establish monitoring scheme using satellite data in combination with

    models and in situ data for validation

  • Acknowledgement

    • The SAR data for the study is provided ESA through AOBE-2780)

    • The research is supported by INTAS (contract no. 06-1000025-9264), EU

    FP6 (contract no. 031001- MONRUK), and national projects