MERIS for Case 2 Waters
|
|
- Lily Harrington
- 5 years ago
- Views:
Transcription
1 MERIS for Case 2 Waters Roland Doerffer &Helmut Schiller GKSS Forschungszentrum Institute for Coastal Research doerffer@gkss.de
2 Case 2 water reflectance spectra North Sea
3 Dissolved and suspended matter in coastal water water molecules hydrocarbons, aminoacids humic acids clay-humic-metal -complexes viruses colloid range bacteria terrigenous sm eroded mud and sand fly-ash fecal pellets phytoplankton desert-dust macroflocs zooplankton colonies 0.1 nm 1 nm 10 nm 100 nm 1 µm 10 µm 100 µm 1 mm 1 cm dissolved 0.45 µm suspended
4 Case 2 Water Algorithm COASTLOOC COLORS MAPP MAPP Bio-optical measurements a(λ), a(λ), b (λ), (λ), Pig, Pig, TSM, TSM, C, C, Y Lu/Ed(λ,z), RLw RLw Bio-optical Model Model Incl. Incl. variability Set Set up up radiance transfer model model Monte Monte Carlo, Carlo, Hydrolight fann, fann, bann bann MERIS MERIS Processor 3 angles 8 RLw ann Simulation of of RLw(λ,θ v,θ v,θ s,φ s,φ vs vs > Spectra Training and and Test Test of of ann ann TSM Pig Gelb Conf. Flag MERIS MERIS Product
5 Scheme of a bio-optical model: optical components for MERIS Water sample In situ AC-9 BB-4 particle particle scattering scattering backscattering backscattering TSM Gelbstoff yellow substance particle total absorption Absorption Absorption of of Total Total --bleached bleached fraction fraction = phytoplankton phytoplankton absorption absorption Absorption Absorption of of bleached bleached fraction Absorption fraction Absorption of of = spm spmabsorption bleached bleached Fraction Fraction + gelbstoff gelbstoff gelbstoff gelbstoff absorption absorptionspectrum = spectrum total total gelbstoff gelbstoff spectral spectralexponent exponent Optical properties at 442 nm Chlor Gelb
6 COLORS Helgoland Gelbstoff absorption all stations 1.2 COLORS Helgoland Gelbstoff absorption all stations absorption a (m -1 ) wavelength (nm)
7 Pigment absorption spectra H187, Norway different locations Norway all stations a (m -1 )) norm a (m -1 )) norm wavelength (nm) wavelength (nm)
8 Bio-optical model Based on: MAVT North Sea / German Bight (GKSS), Norwegian waters (NIVA, Uni Oslo, NERSC), Baltic Sea (IOW), Recommendation by M. Babin Gelbstoff absorption exponent: Bleached particle absorption exponent: Particle scattering exponent: White particles scattering exponent: 0.0 Phytoplankton pigment absorption: > 200 spectra from different areas and seasons Gelbstoff absorption ays(443): m-1 Particle scattering bp(443): m-1 White particle scattering: m-1 Phytoplankton pigment abs. apig(443): m-1 Minimum particle scattering bp(443): 0.25*a_pig(443) Bleached particle absorption abp(443): 0.1*bp(443)+ran_gauss*0.03*bp(443)
9 The actual MERIS case II water algorithm r, r log of reflectances c log of concentrations g geometry information q quality indicator NN input NN output r r invnn q q g g c forwnn r c c If RLw < , RLw = Flag q true if sum (r(i) / r (i)) > 4.0
10 NN sensitivity test, all cases 10 2 case 2 water chlorophyll retrieval with NN nn-derived µg/l model chlorophyll µg/l
11 NN sensitivity, typical North Sea water 10 2 Pigment in North Sea Water (gelb < 0.2 m-1, MSM < 5 mg/l) nn µg/l model µg/l
12 Pigment absorption Chl. a, H Heincke187 a443 pigment n=95 chlorophyll a [mg/l] a(443) (m -1 )) Conversions: Chl. a [mg m-3] = 21 * a_pig_442 ^1.04 TSM [ g m-3] = 1.72 * b_tsm_442
13 MEGS 7.2 algal_1 / algal_2=21*a_pig^1.04 Red dots indicate pixels localized in the map (next pages), these dots have been selected by hand, because they form a second cloud in the scatter plot. As seen in the map they belong mainly to case 2 water. The regression line was also determined by hand only for the upper data cloud (case 1 water) Algal_2=21*a_pig^1.04
14 MEGS 7.2 relationship, log ref. input Red line: alg1=21*apig^1.04 MEGS 7.3 coefficients
15 World map of MERIS data of MEGS 7.2 processing, red dots indicate data which form a second cloud in the scatter plot Algal_2 computed
16 MERIS algal_2,
17 MERIS, TSM,
18 MERIS, Gelbstoff,
19 Red Tide German Bight , MERIS FR
20 North Sea Red Tide of Myrionecta rubra
21 Chlorophyll Distribution Northsea March 2003 (MERIS) Chlorophyll] mg/m³ L3-Product: Monthly Median MERIS-Algal2 March 2003, 37 scenes, GKSS-ESA-Algorithm
22 comparison transect Cuxhaven -> Helgoland ca. 60 km from highly turbid waters to average North-Sea water
23 comparison concentrations Meris <-> in-situ along track Cuxhaven-Helgoland match-up
24 comparison concentrations Meris <-> in-situ along track Cuxhaven-Helgoland match-up
25 Algal 1 and 2 Mean algal_1_mean algal_2_mean 1.E+02 1.E+01 1.E+00 mg/m³ 1.E-01 1.E-02 1.E product id
26 MEGS 7.3, lin refl. Input Histogram 8000 Histogram log(alg2) MEGS7.3 (linnn) Histogram log(alg1) MEGS7.3 (linnn) logn(algal_1) logn(algal_2)
27 MERIS Case 2 algorithm test against IOCCG simulated data set 10 1 a_tot sun TSM scatter a_tot_442 NN GKSS [m -1 ] b_tot_442 NN GKSS [m -1 ] a_tot_442 test_case [m -1 ] bb_tot_442 test_case [m -1 ] Total absorption at 442 nm Total scattering at 442 nm
28 High suspended matter concentrations in the German Bight MERIS FR Helgoland Bight Section 160 km
29 Strange Spectra producing negative reflectances MERIS FR RL_toa RL_tosa RL_path RLw_bread 0.04 RL [sr -1 ] wavelength [nm]
30 SPM distribution Helgoland Bay MERIS FR North Sea Elbe estuary mg/l
31 Summary and Conclusions Primary output of MERIS Case 2 water algorithm are the inherent optical properties: (1) scattering b of all particles, (2) absorption a_y of dissolved gelbstoff + absorption of bleached particles, (3) absorption of phytoplankton pigments, all at MERIS band 2 (442 nm) Variability of bio-optical variables as well as expected errors are included in the training of the NN Using a combination of a backward and forward NN the input reflectance spectrum (i.e. after atmospheric correction) is tested if this spectrum is within the range of the training data set, a flag is set if deviation is too high Accuracy of results may change pixel by pixel, depends on concentration mixture and scope of the bio-optical model MERIS Case 2 water algorithm as implemented in MEGS 7.4 for reprocessing is more robust than pre-launch version: Improved bio-optical model based on more data Using cut-off reflectance more robust against error in atmospheric correction Further test are needed world wide
32 Algal 1 and 2 Stdev algal_1_stddev algal_2_stddev 1.E+02 1.E+01 1.E+00 mg/m³ 1.E-01 1.E-02 1.E product id
33 MEGS 7.3, lin reflectance input mean values of scenes 10 2 Mean of algal_2, YS, TSM with LinNN algal_2 ys tsm 10 1 mean concentration product id
MERIS Reprocessing Neural Net Algorithm. Roland Doerffer, Carsten Brockmann,
MERIS Reprocessing Neural Net Algorithm Roland Doerffer, doerffer@gkss.de Carsten Brockmann, brockmann@brockmann-consult.de MERIS: Aufnahme der Helgoländer Bucht MERIS FR 16.4.2003 Helgoland Bight Section
More informationIntroduction into Ocean Coulour Remote Sensing using MERIS data
ESA Training Course Oceanography from Space Hamburg, September 25-29 2006 Introduction into Ocean Coulour Remote Sensing using MERIS data Roland Doerffer GKSS Research Center Institute for Coastal Research
More informationAtmospheric Correction
NOWPAP / PICES / WESTPAC Joint Training Course on Remote Sensing Data Analysis Introduction and recent progress in ocean color remote sensing part II: Correction of the influence of the atmosphere in Ocean
More informationMapping water constituents in Lake Constance using CHRIS/Proba
S. Miksa, T. Heege, V. Kisselev and P. Gege Mapping water constituents in Lake Constance using CHRIS/Proba 3rd ESA CHRIS/Proba Workshop Frascati,, 21-23 23 March 2005 Overview - Test site and in-situ data
More informationOcean Colour Remote Sensing in Turbid Waters. Lecture 2: Introduction to computer exercise #1 The Colour of Water.
Ocean Colour Remote Sensing in Turbid Waters Lecture 2: Introduction to computer exercise #1 The Colour of Water by Kevin Ruddick Overview of this lecture Objective: introduce the HYPERTEACH ocean colour
More informationEVOLUTION OF THE C2RCC NEURAL NETWORK FOR SENTINEL 2 AND 3 FOR THE RETRIEVAL OF OCEAN COLOUR PRODUCTS IN NORMAL AND EXTREME OPTICALLY COMPLEX WATERS
EVOLUTION OF THE C2RCC NEURAL NETWORK FOR SENTINEL 2 AND 3 FOR THE RETRIEVAL OF OCEAN COLOUR PRODUCTS IN NORMAL AND EXTREME OPTICALLY COMPLEX WATERS Brockmann, Carsten (1), Doerffer, Roland (1), Peters,
More informationSentinel 2 Pre-processing Requirements for coastal and inland waters
Sentinel 2 Pre-processing Requirements for coastal and inland waters K A I S Ø R E NSEN NIVA CARSTEN B R O CKMANN Ecological and chemical classification of water bodies in Norway Water quality - products
More informationOcean Colour Remote Sensing in Turbid Waters. Lecture 2: Introduction to computer exercise #1 The Colour of Water
[1/17] Kevin Ruddick, /RBINS 2012 Ocean Colour Remote Sensing in Turbid Waters Lecture 2: Introduction to computer exercise #1 The Colour of Water by Kevin Ruddick [2/17] Kevin Ruddick, /RBINS 2012 Overview
More informationC M E M S O c e a n C o l o u r S a t e l l i t e P r o d u c t s
Implemented by C M E M S O c e a n C o l o u r S a t e l l i t e P r o d u c t s This slideshow gives an overview of the CMEMS Ocean Colour Satellite Products Marine LEVEL1 For Beginners- Slides have been
More informationMERMAID: Chl and IOPs
MERMAID: Chl and IOPs Kathryn Barker 1, C. Mazeran 2, C. Lerebourg 2 1 ARGANS Ltd, UK. 2 ACRI-ST, France MERMAID catalogue Chla and IOP definitions have been fixed; Other parameters also. MERMAID columns
More information5.5. Coastal and inland waters
5.5. Coastal and inland waters 5. Atmospheric Correction SeaWiFS and MODIS Experiences Show: High quality ocean color products for the global open oceans (Case-1 waters). Significant efforts are needed
More informationChlorophyll-a, Phycocyanin and Phytoplankton type products
Chlorophyll-a, Phycocyanin and Phytoplankton type products Mariano Bresciani, Monica Pinardi, Claudia Giardino CNR IREA bresciani.m@irea.cnr.it Aims Implementation of algorithms dedicated to phytoplankton's
More informationAbsorption properties. Scattering properties
Absorption properties Scattering properties ocean (water) color light within water medium Lu(ϴ,ϕ) (Voss et al 2007) (Kirk 1994) They are modulated by water constituents! Sensor measures E d L w [Chl] [CDOM]
More informationThe low water-leaving radiances phenomena around the Yangtze River Estuary
The low water-leaving radiances phenomena around the Yangtze River Estuary He Xianqiang* a, Bai Yan a, Mao Zhihua a, Chen Jianyu a a State Key Laboratory of Satellite Ocean Environment Dynamics, Second
More informationMarine Reflectance in the Short Wave Infrared ( nm, esp nm) For extremely turbid waters
Marine Reflectance in the Short Wave Infrared (1000-3000nm, esp. 1000-1150nm) For extremely turbid waters Belcolour MICAS heritage Knaeps, E., Raymaekers, D., Sterckx, S, Ruddick, K., Dogliotti, A.I..
More informationPLEASE SCROLL DOWN FOR ARTICLE
This article was downloaded by:[csiro Library Network] On: 19 November 2007 Access Details: [subscription number 778652903] Publisher: Taylor & Francis Informa Ltd Registered in England and Wales Registered
More informationAbsorption properties. Scattering properties
Absorption properties Scattering properties ocean (water) color light within water medium Lu(ϴ,ϕ) (Voss et al 2007) (Kirk 1994) They are modulated by water constituents! Sensor measures E d L w [Chl] [CDOM]
More informationZhongPing Lee, University of Massachusetts Boston
ZhongPing Lee, University of Massachusetts Boston Absorption properties Scattering properties ocean (water) color light within water medium Lu(ϴ,ϕ) (Voss et al 2007) (Kirk 1994) They are modulated by water
More information10 Absorption and scattering of light in natural waters
10 Absorption and scattering of light in natural waters Vladimir I. Haltrin 10.1 Introduction In this chapter we restrict ourselves to the problems of absorptionabsorption [1 13], elastic [1, 4, 5, 10,
More informationModeling of elastic and inelastic scattering effects in oceanic optics
22-25 October 996, Halifax, Nova Scotia, Canada, SPI Volume 2963, Bellingham, WA, USA, 96 pp., 997 Modeling of elastic and inelastic scattering effects in oceanic optics Vladimir I. Haltrin, eorge W. Kattawar,
More informationProceedings of EARSeL-SIG-Workshop LIDAR, Dresden/FRG, June 16 17, 2000
MEASUREMENT AND SIMULATION OF SUBSTANCE SPECIFIC CONTRIBUTIONS OF PHYTOPLANKTON, GELBSTOFF, AND MINERAL PARTICLES TO THE UNDERWATER LIGHT FIELD IN COASTAL WATERS Hans Barth, Rainer Reuter & Marc Schröder
More information1-2 Aerosol models We obtain the aerosol reflectance for 678nm and 865nm bands including the interaction part as follows,
OTSK1 tmospheric Correction for Ocean Color. lgorithm Outline (1) lgorithm name: tmospheric Correction for Ocean Color (2) Product Code: NWLR (3) PI names: G-0065 Hajime Fukushima (4) Overview of the algorithm
More informationBAYESIAN METHODOLOGY FOR ATMOSPHERIC CORRECTION OF PACE OCEAN-COLOR IMAGERY
BAYESIAN METHODOLOGY FOR ATMOSPHERIC CORRECTION OF PACE OCEAN-COLOR IMAGERY Robert Frouin, SIO/UCSD Topics 1. Estimating phytoplankton fluorescence and ocean Raman scattering from OCI super sampling in
More informationVariations of Estuarine Turbid Plumes and Mudflats in Response to Human Activities and Climate Change Dragon-3 project id
Variations of Estuarine Turbid Plumes and Mudflats in Response to Human Activities and Climate Change Dragon-3 project id. 1555 Chinese PI(s) Prof. SHEN Fang( 沈芳 ) Prof. ZHOU Yunxuan( 周云轩 ) European PI(s)
More informationHICO OSU Website and Data Products
HICO OSU Website and Data Products Curtiss O. Davis College of Earth Ocean and Atmospheric Sciences Oregon State University, Corvallis, OR, USA 97331 cdavis@coas.oregonstate.edu Oregon State Introduction
More informationBio-optical Algorithms for European Seas
Bio-optical Algorithms for European Seas Performance and Applicability of Neural-Net Inversion Schemes Davide D Alimonte 1, Giuseppe Zibordi 2, Jean-François Berthon 2, Elisabetta Canuti 2 and Tamito Kajiyama
More informationA Method for MERIS Aerosol Correction : Principles and validation. David Béal, Frédéric Baret, Cédric Bacour, Kathy Pavageau
A Method for MERIS Aerosol Correction : Principles and validation David Béal, Frédéric Baret, Cédric Bacour, Kathy Pavageau Outlook Objectives Principles Training neural networks Validation Comparison
More informationAtmospheric correction in presence of sun glint: the POLYMER Algorithm
Atmospheric correction in presence of sun glint: the POLYMER Algorithm Dominique Jolivet François Steinmetz Pierre-Yves Deschamps Jan 17, 2011 Atelier National Couleur de l'eau - GIS COOC c 2011 Atmospheric
More informationBio-optical modeling of IOPs (PFT approaches)
Bio-optical modeling of IOPs (PFT approaches) Collin Roesler July 28 2014 note: the pdf contains more information than will be presented today Some History It started with satellite observations of El
More informationHICO Calibration and Atmospheric Correction
HICO Calibration and Atmospheric Correction Curtiss O. Davis College of Earth Ocean and Atmospheric Sciences Oregon State University, Corvallis, OR, USA 97331 cdavis@coas.oregonstate.edu Oregon State Introduction
More informationImpacts of Atmospheric Corrections on Algal Bloom Detection Techniques
1 Impacts of Atmospheric Corrections on Algal Bloom Detection Techniques Ruhul Amin, Alex Gilerson, Jing Zhou, Barry Gross, Fred Moshary and Sam Ahmed Optical Remote Sensing Laboratory, the City College
More information9/12/2011. Training Course Remote Sensing - Basic Theory & Image Processing Methods September 2011
Training Course Remote Sensing - Basic Theory & Image Processing Methods 19 23 September 2011 Introduction to Remote Sensing Michiel Damen (September 2011) damen@itc.nl 1 Overview Electro Magnetic (EM)
More informationA Quantitative Comparison of Total Suspended Sediment Algorithms: A Case Study of the Last Decade for MODIS and Landsat-Based Sensors
remote sensing Article A Quantitative Comparison of Total Suspended Sediment Algorithms: A Case Study of the Last Decade for MODIS and Landsat-Based Sensors Passang Dorji * and Peter Fearns Remote Sensing
More informationSatellite Oceanography and Applications 1: Introduction, SST, Ocean color
Satellite Oceanography and Applications 1: Introduction, SST, Ocean color Ebenezer Nyadjro US Naval Research Lab RMU Summer Program (AUGUST 24-28, 2015) Objectives/Goals To know the basic methods of ocean
More informationCoastal Characterization Using EO-1 Hyperion Data
Coastal Characterization Using EO-1 Hyperion Data Dr. Hsiao-hua K. Burke EO-1 SVT Meeting 18-21 November 2002 Sponsor: NOAA NESDIS GOES 2002-1 Channel Positions of Various Ocean- Color Sensors, 1978-2000*
More informationAn evaluation of two semi-analytical ocean color algorithms for waters of the South China Sea
28 5 2009 9 JOURNAL OF TROPICAL OCEANOGRAPHY Vol.28 No.5 Sep. 2009 * 1 1 1 1 2 (1. ( ), 361005; 2. Northern Gulf Institute, Mississippi State University, MS 39529) : 42, QAA (Quasi- Analytical Algorithm)
More informationMethod to derive ocean absorption coefficients from remote-sensing reflectance
Method to derive ocean absorption coefficients from remote-sensing reflectance Z. P. Lee, K. L. Carder, T. G. Peacock, C. O. Davis, and J. L. Mueller A method to derive in-water absorption coefficients
More informationBio-optical properties and ocean color algorithms for coastal waters influenced by the Mississippi River during a cold front
Bio-optical properties and ocean color algorithms for coastal waters influenced by the Mississippi River during a cold front Eurico J. D Sa, Richard L. Miller, and Carlos Del Castillo During the passage
More informationSEDIMENT AND CHLOROPHYLL CONCENTRATIONS IN MAJOR CHINESE RIVERS USING MERIS IMAGERY
SEDIMENT AND CHLOROPHYLL CONCENTRATIONS IN MAJOR CHINESE RIVERS USING MERIS IMAGERY P.J. Mulhearn (1) and Ian S. F. Jones (2) (1) Ocean Technology Group J05, University of Sydney, NSW 2006 Australia; phil.mulhearn@otg.usyd.edu.au
More informationOptics and biogeochemistry, (the use & misuse of optical proxies)
Optics and biogeochemistry, (the use & misuse of optical proxies) Emmanuel Boss, UMaine. Optical measurements: measurements of EM radiation from UV->IR. Why use optics? Provides ability to observe oceans
More informationAEROSOL RETRIEVAL AND ATMOSPHERIC CORRECTION FOR MERIS DATA OVER LAKES
AEROSOL RETRIEVAL AND ATMOSPHERIC CORRECTION FOR MERIS DATA OVER LAKES Dana Floricioiu, Helmut Rott Institute of Meteorology and Geophysics, University of Innsbruck, Innrain, A-6 Innsbruck, Austria. Email:
More informationAtmospheric Correction of Ocean Color RS Observations
Atmospheric Correction of Ocean Color RS Observations Menghua Wang NOAA/NESDIS/STAR E/RA3, Room 3228, 5830 University Research Ct. College Park, MD 20740, USA IOCCG Summer Lecture Series, Villefranche-sur-Mer,
More informationChlorophyll-based model of seawater optical properties
Chlorophyll-based model of seawater optical properties Vladimir I. Haltrin A one-parameter model of the inherent optical properties of biologically stable waters is proposed. The model is based on the
More informationOCEAN COLOUR MONITOR ON-BOARD OCEANSAT-2
OCEAN COLOUR MONITOR ON-BOARD OCEANSAT-2 Rangnath R Navalgund Space Applications Centre Indian Space Research Organisation Ahmedabad-380015, INDIA OCEANSAT-2 2 MISSION OCEANSAT-2 2 is a global mission
More informationOptics of Marine Particles
Optics of Marine Particles Lecture 2 Dariusz Stramski Scripps Institution of Oceanography University of California San Diego Email: dstramski@ucsd.edu IOCCG Summer Lecture Series 22 July - 2 August 2014,
More informationGSICS UV Sub-Group Activities
GSICS UV Sub-Group Activities Rosemary Munro with contributions from NOAA, NASA and GRWG UV Subgroup Participants, in particular L. Flynn 1 CEOS Atmospheric Composition Virtual Constellation Meeting (AC-VC)
More informationVERIFICATION OF MERIS LEVEL 2 PRODUCTS: CLOUD TOP PRESSURE AND CLOUD OPTICAL THICKNESS
VERIFICATION OF MERIS LEVEL 2 PRODUCTS: CLOUD TOP PRESSURE AND CLOUD OPTICAL THICKNESS Rene Preusker, Peter Albert and Juergen Fischer 17th December 2002 Freie Universitaet Berlin Institut fuer Weltraumwissenschaften
More informationCarsten Brockmann, Ana Ruescas, Simon Pinnock CoastColour Team: BC D, HZG D, PML UK, RBINS B, LISE F, FCUL P COASTCOLOUR SPOT 4 TAKE 5
Carsten Brockmann, Ana Ruescas, Simon Pinnock CoastColour Team: BC D, HZG D, PML UK, RBINS B, LISE F, FCUL P COASTCOLOUR SPOT 4 TAKE 5 CoastColour CoastColour is providing ocean colour products for coastal
More informationEstimation of ocean contribution at the MODIS near-infrared wavelengths along the east coast of the U.S.: Two case studies
GEOPHYSICAL RESEARCH LETTERS, VOL. 32, L13606, doi:10.1029/2005gl022917, 2005 Estimation of ocean contribution at the MODIS near-infrared wavelengths along the east coast of the U.S.: Two case studies
More informationA NOVEL CONCEPT FOR MEASURING SEAWATER INHERENT OPTICAL PROPERTIES IN AND OUT OF THE WATER
A NOVEL CONCEPT FOR MEASURING SEAWATER INHERENT OPTICAL PROPERTIES IN AND OUT OF THE WATER Gainusa Bogdan, Alina 1 ; Boss, Emmanuel 1 1 School of Marine Sciences, Aubert Hall, University of Maine, Orono,
More informationThis article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and
This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution
More informationBldg., Corvallis, OR, USA USA 39529, USA. Arabia 1. INTRODUCTION ABSTRACT
Evaluating VIIRS Ocean Color Products for West Coast and Hawaiian Waters Curtiss O. Davis a, Nicholas Tufillaro a, Jasmine Nahorniak a, Burton Jones b,d and Robert Arnone c a College of Earth, Ocean and
More informationSatellite-based Red-Tide Detection/Monitoring
Satellite-based Detection/Monitoring Contents 1. Introduction - and Its Monitoring System 2. Detection Using Ocean Color Remote Sensing 3. Satellite-Based Monitoring in the Asian Coastal Seas Hiroshi KAWAMURA
More informationEstimating Shelf Seawater Composition by Inversion of AC9 Inherent Optical Property Measurements
Estimating Shelf Seawater Composition by Inversion of AC9 Inherent Optical Property Measurements Ian C. Brown, Alex Cunningham, David McKee Physics Department, University of Strathclyde, 107 Rottenrow,
More informationAbsorption spectrum of phytoplankton pigments derived from hyperspectral remote-sensing reflectance
Remote Sensing of Environment 89 (2004) 361 368 www.elsevier.com/locate/rse Absorption spectrum of phytoplankton pigments derived from hyperspectral remote-sensing reflectance ZhongPing Lee a, *, Kendall
More informationPolarization measurements in coastal waters using a hyperspectral multiangular sensor
Polarization measurements in coastal waters using a hyperspectral multiangular sensor A. Tonizzo 1, J. Zhou 1, A. Gilerson 1, T. Iijima 1, M. Twardowski 2, D. Gray 3, R. Arnone 3, B. Gross 1, F. Moshary
More informationAnalysis of the particle size distribution and optical properties in the Korean seas
Analysis of the particle size distribution and optical properties in the Korean seas Boram Lee 1,2, Young-Je Park 1, Wonkook Kim 1, Jae-Hyun Ahn 1, Kwangseok Kim 1, Jeong-Eon Moon 1 and Sang-Wan Kim 2
More informationBACKSCATTERING BY NON-SPHERICAL NATURAL PARTICLES: INSTRUMENT DEVELOPMENT, IOP S, AND IMPLICATIONS FOR RADIATIVE TRANSFER
BACKSCATTERING BY NON-SPHERICAL NATURAL PARTICLES: INSTRUMENT DEVELOPMENT, IOP S, AND IMPLICATIONS FOR RADIATIVE TRANSFER Emmanuel Boss School of Marine Sciences 5741 Libby Hall University Of Maine Orono,
More informationUsing Satellite Data to Monitor Sediment Fluxes, Water Properties and Particles Distribution in the Black Sea-Danube Interaction Zone
Using Satellite Data to Monitor Sediment Fluxes, Water Properties and Particles Distribution in the Black Sea-Danube Interaction Zone Adriana M. Constantinescu 1,2, Andrew N. Tyler 2, Peter D. Hunter 2,
More informationComparison of chlorophyll concentration in the Bay of Bengal and the Arabian Sea using IRS-P4 OCM and MODIS Aqua
Indian Journal of Marine Sciences Vol. 39(3), September 2010, pp. 334-340 Comparison of chlorophyll concentration in the Bay of Bengal and the Arabian Sea using IRS-P4 OCM and MODIS Aqua Ramesh P. Singh
More informationAutomated ocean color product validation for the Southern California Bight
Automated ocean color product validation for the Southern California Bight Curtiss O. Davis a, Nicholas Tufillaro a, Burt Jones b, and Robert Arnone c a College of Earth, Ocean and Atmospheric Sciences,
More informationLong-Term Time Series of Water Vapour Total Columns from GOME, SCIAMACHY and GOME-2
Graphics: ESA Graphics: ESA Graphics: ESA Long-Term Time Series of Water Vapour Total Columns from GOME, SCIAMACHY and GOME-2 S. Noël, S. Mieruch, H. Bovensmann, J. P. Burrows Institute of Environmental
More informationAtmospheric Lidar The Atmospheric Lidar (ATLID) is a high-spectral resolution lidar and will be the first of its type to be flown in space.
www.esa.int EarthCARE mission instruments ESA s EarthCARE satellite payload comprises four instruments: the Atmospheric Lidar, the Cloud Profiling Radar, the Multi-Spectral Imager and the Broad-Band Radiometer.
More informationApparent and inherent optical properties in the ocean
Apparent and inherent optical properties in the ocean Tomorrow: "Open questions in radiation transfer with a link to climate change 9:30 Gathering and Coffee 9:50 Opening Ilan Koren, Environmental Sciences
More informationOcean Color Algorithms for the Southern Ocean Constraining the Carbon cycle
Ocean Color Algorithms for the Southern Ocean Constraining the Carbon cycle Report Breakout Session No. 5 IOCS 2017 Lisbon, Portugal Maria Vernet Scripps Institution of Oceanography, USA Antarctic Fronts:
More informationSATELLITE DATA COLLECTION BY THE UPRM-TCESS SPACE INFORMATION LABORATORY
SATELLITE DATA COLLECTION BY THE UPRM-TCESS SPACE INFORMATION LABORATORY Visita a la Estación De Satélites De UPRM En el CID 16 sep. 4:30 pm Nos reuniremos al frente del CID. CID L-BAND ANTENNA Orbview
More informationParallel Measurements of Light Scattering and Characterization of Marine Particles in Water: An Evaluation of Methodology
Parallel Measurements of Light Scattering and Characterization of Marine Particles in Water: An Evaluation of Methodology Dariusz Stramski Marine Physical Laboratory Scripps Institution of Oceanography
More informationLong-term variations in primary production in a eutrophic sub-estuary. I. Seasonal and spatial patterns
The following supplement accompanies the article Long-term variations in primary production in a eutrophic sub-estuary. I. Seasonal and spatial patterns Charles L. Gallegos Smithsonian Environmental Research
More informationParting the Red Seas: The Optics of Red Tides
Parting the Red Seas: The Optics of Red Tides H.M. Dierssen 1*, Kudela, R.M. 2, Ryan, J.P. 3 1 University of Connecticut, Department of Marine Science, Groton, CT 06340. 2 University of California, Ocean
More informationProceedings, Ocean Optics XXI, Glasgow, Scotland, 8-12 October, Assessing Uncertainties in Satellite Ocean Color Bio-Optical Properties
Assessing Uncertainties in Satellite Ocean Color Bio-Optical Properties S.C. McCarthy 1. R.W. Gould, Jr. 1, J. Richman 1, E. Coelho 2, and I. Shulman 1 'Code 7331, Naval Research Laboratory, Stennis Space
More informationReference Model for MERIS Level 2 Processing. Third MERIS reprocessing: Ocean Branch
Page : i of 107 Reference Model for MERIS Level 2 Processing Third MERIS reprocessing: Ocean Branch Page : ii of 107 Doc. no: PO-TN-MEL-GS-0026-Ocean Issue: 5.0 Rev: 4.0 Date: May 2013 Function Name Company
More informationUncertainties of inherent optical properties obtained from semianalytical inversions of ocean color
Uncertainties of inherent optical properties obtained from semianalytical inversions of ocean color Peng Wang, Emmanuel S. Boss, and Collin Roesler We present a method to quantify the uncertainties in
More informationInteractive comment on River bulge evolution and dynamics in a non-tidal sea Daugava River plume in the Gulf of Riga, Baltic Sea by E. Soosaar et al.
Ocean Sci. Discuss., 12, C1547 C1555, 2016 www.ocean-sci-discuss.net/12/c1547/2016/ Author(s) 2016. This work is distributed under the Creative Commons Attribute 3.0 License. Interactive comment on River
More informationEffect of suspended particulate-size distribution on the backscattering ratio in the remote sensing of seawater
Effect of suspended particulate-size distribution on the backscattering ratio in the remote sensing of seawater Dubravko Risović Mie theory is used to study the influence of the particle-size distribution
More informationHyperspectral imaging of river systems
Hyperspectral imaging of river systems Curtiss O. Davis College of Oceanic and Atmospheric Sciences Oregon State University 104 COAS Admin. Bldg. Corvallis OR 97331-5503 U.S.A. +1 541-737-5707 cdavis@coas.oregonstate.edu
More informationNear-infrared light scattering by particles in coastal waters
Near-infrared light scattering by particles in coastal waters David Doxaran *, Marcel Babin and Edouard Leymarie Université Pierre et Marie Curie - Paris 6, Laboratoire d'océanographie de Villefranche,
More informationA new perspective on aerosol direct radiative effects in South Atlantic and Southern Africa
A new perspective on aerosol direct radiative effects in South Atlantic and Southern Africa Ian Chang and Sundar A. Christopher Department of Atmospheric Science University of Alabama in Huntsville, U.S.A.
More informationof Ocean Colour in Polar Seas Auberge Saint Pierre, Québec City, Canada (10 11 November 2011)
1st Meeting of the IOCCG Working Group on Remote Sensing of Ocean Colour in Polar Seas Auberge Saint Pierre, Québec City, Canada (10 11 November 2011) Introduction Welcoming words from Marcel Babin and
More informationApparent optical properties and radiative transfer theory*
Apparent optical properties and radiative transfer theory* Apparent optical properties. The RTE and Gershun s equation The Secchi disk (and depth, an AOP). *based in part on lectures by Roesler, Mobley,
More informationThe Coastal Ocean Imaging Spectrometer (COIS) and Coastal Ocean Remote Sensing
The Coastal Ocean Imaging Spectrometer (COIS) and Coastal Ocean Remote Sensing Curtiss O. Davis College of Oceanic and Atmospheric Sciences 104 COAS Admin, Bldg. Corvallis, OR 97331 phone: (541) 737-4432
More informationThe beam attenuation coefficient and its spectra. (also known as beam-c or extinction coefficient ). Emmanuel Boss, U. of Maine
The beam attenuation coefficient and its spectra (also known as beam-c or extinction coefficient ). Emmanuel Boss, U. of Maine Review: IOP Theory Collin s lecture 2: F o F t Incident Radiant Flux Transmitted
More informationComparison of aerosol radiative forcing over the Arabian Sea and the Bay of Bengal
Advances in Space Research 33 (2004) 1104 1108 www.elsevier.com/locate/asr Comparison of aerosol radiative forcing over the Arabian Sea and the Bay of Bengal S. Dey a, S. Sarkar b, R.P. Singh a, * a Department
More informationAnnex VI-1. Draft National Report on Ocean Remote Sensing in China. (Reviewed by the Second Meeting of NOWPAP WG4)
UNEP/NOWPAP/CEARAC/WG4 2/9 Page1 Draft National Report on Ocean Remote Sensing in China (Reviewed by the Second Meeting of NOWPAP WG4) UNEP/NOWPAP/CEARAC/WG4 2/9 Page1 1. Status of RS utilization in marine
More informationSmall-scale effects of underwater bubble clouds on ocean reflectance: 3-D modeling results
Small-scale effects of underwater bubble clouds on ocean reflectance: 3-D modeling results Jacek Piskozub, 1,* Dariusz Stramski, 2 Eric Terrill, 2 and W. Kendall Melville 2 1 Institute of Oceanology, Polish
More informationBiological Oceanography by Remote Sensing. M.A. Srokosz
Biological Oceanography by Remote Sensing M.A. Srokosz in Encyclopedia of Analytical Chemistry R.A. Meyers (Ed.) pp. 8506 8533 John Wiley & Sons Ltd, Chichester, 2000 BIOLOGICAL OCEANOGRAPHY BY REMOTE
More informationPUBLICATIONS. Journal of Geophysical Research: Oceans
PUBLICATIONS RESEARCH ARTICLE Key Points: A QA system is developed for spectral remote-sensing reflectance The system consists of a reference and a score metric It is applicable to both remotely sensed
More informationMERIS SMILE EFFECT CHARACTERISATION AND CORRECTION DOCUMENT. document title/ titre du document. prepared by/préparé par MERIS ESL
DOCUMENT document title/ titre du document MERIS SMILE EFFECT CHARACTERISATION AND CORRECTION prepared by/préparé par MERIS ESL reference/réference issue/édition 2 revision/révision 0 date of issue/date
More informationOptical Properties of Mineral Particles and Their Effect on Remote-Sensing Reflectance in Coastal Waters
Optical Properties of Mineral Particles and Their Effect on Remote-Sensing Reflectance in Coastal Waters Dariusz Stramski Marine Physical Laboratory Scripps Institution of Oceanography University of California
More informationAstrid Bracher PHYTOOPTICS group, Climate Sciences, AWI & IUP, University Bremen
Breakout session "Hyperspectral science and applications for shelf and open ocean processes" Hyperspectral ocean color imagery and applications to studies of phytoplankton ecology Astrid Bracher PHYTOOPTICS
More informationWintertime SST and Chl a off NW Iberian shelf from satellite and in situ data
Wintertime SST and Chl a off NW Iberian shelf from satellite and in situ data Paulo B. Oliveira+, Teresa Moita+, Rui Catarino+, António Jorge da Silva++ + INRB IPIMAR Instituto Nacional de Recursos Biológicos,
More informationRestoring number of suspended particles in ocean using satellite optical images and forecasting particle fields
Restoring number of suspended particles in ocean using satellite optical images and forecasting particle fields Vladimir I. Haltrin*, Robert. A. Arnone**, Peter Flynn, Brandon Casey, Alan D. Weidemann,
More informationIn-flight Spectral Calibration of MERIS/OLCI. Jürgen Fischer, Rene Preusker, Rasmus Lindstrot Institute for Space Science Free University Berlin
In-flight Spectral Calibration of MERIS/OLCI Jürgen Fischer, Rene Preusker, Rasmus Lindstrot Institute for Space Science Free University Berlin 1 MERIS Instrument 2 MERIS Instrument Concept 3 MERIS Operation
More informationESSOAr Non-exclusive First posted online: Sat, 1 Dec :39:37 This content has not been peer reviewed.
A practical method for estimating the light backscattering coefficient from the remotesensing reflectance in Baltic Sea conditions and examples of its possible application Sławomir B. Woźniak*, Mirosław
More informationFinal Report 27/06/ The. STSE-WaterRadiance. project. Final Report. (ESA Contract: AO /08/NL/CT)
7/06/1 1. Page: 1 of 77 The STSE-WaterRadiance project (ESA Contract: AO 1-5859/08/NL/CT) Authors: Rüdiger Röttgers, Carsten Brockmann, Roland Doerffer, Jürgen Fischer, Andre Hollstein, Samantha Lavender,
More informationEXTRACTION OF THE DISTRIBUTION OF YELLOW SAND DUST AND ITS OPTICAL PROPERTIES FROM ADEOS/POLDER DATA
EXTRACTION OF THE DISTRIBUTION OF YELLOW SAND DUST AND ITS OPTICAL PROPERTIES FROM ADEOS/POLDER DATA Takashi KUSAKA, Michihiro KODAMA and Hideki SHIBATA Kanazawa Institute of Technology Nonoichi-machi
More informationEvaluating Realistic Volume Scattering Functions on Underwater Imaging System Performance
Evaluating Realistic Volume Scattering Functions on Underwater Imaging System Performance Deric J Gray Ocean Optics Section Code 7333, Naval Research Laboratory Stennis Space Center, MS 39529 phone: (228)
More informationImpact of Aerosol Model Selection on Water-Leaving Radiance Retrievals from Satellite Ocean Color Imagery
Remote Sens. 2012, 4, 3638-3665; doi:10.3390/rs4123638 Article OPEN ACCESS Remote Sensing ISSN 2072-4292 www.mdpi.com/journal/remotesensing Impact of Aerosol Model Selection on Water-Leaving Radiance Retrievals
More informationRevisiting Ocean Color Algorithms for Chlorophyll a and Particulate Organic Carbon in the Southern Ocean using Biogeochemical Floats
Revisiting Ocean Color Algorithms for Chlorophyll a and Particulate Organic Carbon in the Southern Ocean using Biogeochemical Floats Haëntjens, Boss & Talley SOCCOM Profiling Floats Active floats 80 /
More informationApparent and inherent optical properties of turbid estuarine waters: measurements, empirical quantification relationships, and modeling
Apparent and inherent optical properties of turbid estuarine waters: measurements, empirical quantification relationships, and modeling David Doxaran, Nagur Cherukuru, and Samantha J. Lavender Spectral
More informationInfrared continental surface emissivity spectra and skin temperature retrieved from IASI observation
Infrared continental surface emissivity spectra and skin temperature retrieved from IASI observation Capelle V., Chédin A., Péquignot E., N. A Scott Schlüssel P., Newman S. IASI Conference 2013 Introduction
More information