D. Antoine, E. Leymarie, A. Morel, B. D. Antoine, E. Leymarie, A. Morel, B. Gentili Gentili Laboratoire d'Océanographie de Villefranche, France Laboratoire d'Océanographie de Villefranche, France J.P. Buis, N. Buis, S. Victori, S. J.P. Buis, N. Buis, S. Victori, S. Meunier, M Canini Meunier, M Canini CIMEL Electronique, Paris CIMEL Electronique, Paris B. Fougnie, P. Henry B. Fougnie, P. Henry CNES, Toulouse center, France CNES, Toulouse center, France Anisotropy of the underwater Anisotropy of the underwater light field: development of a light field: development of a “radiance camera” “radiance camera”
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D. Antoine, E. Leymarie, A. Morel, B. Gentili Laboratoire d'Océanographie de Villefranche, France J.P. Buis, N. Buis, S. Victori, S. Meunier, M Canini.
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D. Antoine, E. Leymarie, A. Morel, B. GentiliD. Antoine, E. Leymarie, A. Morel, B. Gentili
Laboratoire d'Océanographie de Villefranche, FranceLaboratoire d'Océanographie de Villefranche, France
J.P. Buis, N. Buis, S. Victori, S. Meunier, M CaniniJ.P. Buis, N. Buis, S. Victori, S. Meunier, M Canini
CIMEL Electronique, ParisCIMEL Electronique, Paris
B. Fougnie, P. HenryB. Fougnie, P. Henry
CNES, Toulouse center, FranceCNES, Toulouse center, France
Anisotropy of the underwater light field: Anisotropy of the underwater light field: development of a “radiance camera”development of a “radiance camera”
http://www.obs-vlfr.fr/Boussole
About 140001-minute acquisition sequences taken at 6Hz, of Es, Ed, Eu, and nadir Lu, at z=4 & 9 meters
Along with wave height, wave period, IOPs and AOPs.
Paper submitted to JGR … waiting for Editor decision
A data set that might be of interest to you in the frame of Radyo
Anisotropy of the underwater light fieldAnisotropy of the underwater light field•Characterized by the “Q factor”:Characterized by the “Q factor”:
)IOPs,,,,(L
)IOPs,,(E)IOPs,,,,(Q
svu
susv
Q is rhe ratio between the upwelling irradiance (EQ is rhe ratio between the upwelling irradiance (Euu) and the upwelling ) and the upwelling
radiance (Lradiance (Luu) measured in a given direction. Q depends on :) measured in a given direction. Q depends on :
The sun positionThe sun position The observation directionThe observation direction
The wavelengthThe wavelength Water optical properties (IOPs)Water optical properties (IOPs)
Knowledge of this “Q factor” is important to Knowledge of this “Q factor” is important to accurately derive the marine reflectance from accurately derive the marine reflectance from the satellite remote sensing measurement at the satellite remote sensing measurement at the top of the atmospherethe top of the atmosphere
Anisotropy of the underwater light fieldAnisotropy of the underwater light field•Q can be derived from RT Simulations (Morel & Gentili, Q can be derived from RT Simulations (Morel & Gentili,
1991, 1993, 1996; Morel et al 2002)1991, 1993, 1996; Morel et al 2002)
The accuracy of such simulations mostly derives from The accuracy of such simulations mostly derives from that of the VSFthat of the VSF
These simulations are partly validated in open ocean These simulations are partly validated in open ocean “Case I waters”“Case I waters”
Still no measurements in coastal “Case II waters”Still no measurements in coastal “Case II waters”
nearly nothing for the downwelling hemispherenearly nothing for the downwelling hemisphere
- Develop our own instrumentDevelop our own instrument
- Tentatively improve some parts of the design as compared to Tentatively improve some parts of the design as compared to existing instrumentationexisting instrumentation
- Further describe the distribution of the upwelling radiance just Further describe the distribution of the upwelling radiance just beneath the sea surface (bio-optical state, sea state, atmospheric beneath the sea surface (bio-optical state, sea state, atmospheric conditions)conditions)
- Extend the description to various depths within the lit layersExtend the description to various depths within the lit layers
- Extend the description to Case 2 watersExtend the description to Case 2 waters
- Simultaneously measure the upwelling and downwelling Simultaneously measure the upwelling and downwelling hemisphereshemispheres
- Invert the full radiance distribution in terms of the VSF ?Invert the full radiance distribution in terms of the VSF ?
II.II. The Radiance CameraThe Radiance Camera
Partnership and project historyPartnership and project history
Mid 2002 : First discussion between LOV, CNES and CIMEL. Mid 2002 : First discussion between LOV, CNES and CIMEL.
Definition of specificationsDefinition of specifications
2003 : 2003 : Project funded by a CNES “Research & Technology” Project funded by a CNES “Research & Technology” actionaction
CIMELCIMEL : Conception (optic, electronic) and realization of the : Conception (optic, electronic) and realization of the cameracamera
LOVLOV : Science background, system specifications, : Science background, system specifications, characterization and validation of the prototype, characterization and validation of the prototype, deployment at seadeployment at sea
2006 : 2006 : Additional funding from CNESAdditional funding from CNES
2008 : 2008 : Test of the first prototypeTest of the first prototype
Specifications of the cameraSpecifications of the camera
Radiometric : Radiometric : - sensitivity better than 10- sensitivity better than 10-5-5 Wm Wm-2-2nmnm-1-1srsr-1-1
- accuracy better than 5%- accuracy better than 5%
- measurement range : 10- measurement range : 10-5-5 to 1 Wm to 1 Wm-2-2nmnm-1-1srsr-1-1
- dynamic over 1 image : 3 decades- dynamic over 1 image : 3 decades
- Multi-spectral in the visible range- Multi-spectral in the visible range
Geometric : Geometric : - Hemispheric field of view (a bit larger actually)- Hemispheric field of view (a bit larger actually)
Specific : Specific : - integration time < 100 ms (movement caused by - integration time < 100 ms (movement caused by waves)waves)
- Longer integration times as well (very dim light) - Longer integration times as well (very dim light)
- compact design to minimize self-shading- compact design to minimize self-shading
- highly resistant to blooming effect (image of the sun)- highly resistant to blooming effect (image of the sun)
II.II. The Radiance CameraThe Radiance Camera
Schematic descriptionSchematic description
Fish eye optic
Bandpass filters (on a filter wheel)
CMOS
CMOS matrix
Aux
Auxiliary sensors
Com
Data transfer & commands
200m depth container
200m electrical/optical cable
II.II. The Radiance CameraThe Radiance Camera
Full descriptionFull description
CMOS
Aux
Com
•The Fish Eye Optic :The Fish Eye Optic : Telecentric, non achromaticTelecentric, non achromatic Developed specifically for this Developed specifically for this
applicationapplication Patented by CIMELPatented by CIMEL
II.II. The Radiance CameraThe Radiance Camera
Full descriptionFull description
CMOS
Aux
Com
•Filters :Filters : The telecentric optic allows a small The telecentric optic allows a small
incidence angle on the filtersincidence angle on the filters Filters used in the camera (Semrock Filters used in the camera (Semrock
®):®):λλ (nm) (nm) ΔΔλλ (nm) (nm)
406406 1515
438438 2424
494494 2020
510510 2020
560560 2525
628628 4040
II.II. The Radiance CameraThe Radiance Camera
Full descriptionFull description
•Sensor :Sensor :The choice of the sensor to have : dynamic, The choice of the sensor to have : dynamic,
sensitivity and no blooming is a key point for sensitivity and no blooming is a key point for this projectthis project
CDD : Best sensitivity, subject to bloomingCDD : Best sensitivity, subject to bloomingCMOS : less sensitive, more linear, no CMOS : less sensitive, more linear, no
blooming blooming
Our Choice :Our Choice :
a “commercial” CMOS, monochrome, 12 bit a “commercial” CMOS, monochrome, 12 bit digitization, digitization,
HD format (1920 x 1080), pixel size 5 HD format (1920 x 1080), pixel size 5 mm
CMOS
Aux
Com
Main difficulty: trade off between Main difficulty: trade off between specs, cost, availability specs, cost, availability
II.II. The Radiance CameraThe Radiance Camera
Full descriptionFull description
•Auxiliary sensors :Auxiliary sensors : CompassCompass depth sensordepth sensor tilt sensortilt sensor Internal temperature and humidityInternal temperature and humidity
CMOS
Aux
Com
II.II. The Radiance CameraThe Radiance Camera
Full descriptionFull description
•Data transferData transfer optical connection (CameraLink®)optical connection (CameraLink®) transfer rate : 15 frames/s (max)transfer rate : 15 frames/s (max) file : 2.3 Mo / frame, Tiff format file : 2.3 Mo / frame, Tiff format
•Instrument commandsInstrument commands RS232 through CameraLink®RS232 through CameraLink®
CMOS
Aux
Com
II.II. The Radiance CameraThe Radiance Camera
The first prototype of the LOV-CIMEL Radiance The first prototype of the LOV-CIMEL Radiance CameraCamera
Camera delivered at the end of 2007 :Camera delivered at the end of 2007 :Size (mm): Ø96 * 260Size (mm): Ø96 * 260
weight : 2.4 kgweight : 2.4 kg
II.II. The Radiance CameraThe Radiance Camera
Test of the deployment system, 14/03/08 Test of the deployment system, 14/03/08 Test in air Test in air
The first prototype of the LOV-CIMEL Radiance The first prototype of the LOV-CIMEL Radiance CameraCamera
IV.IV. Preliminary field resultsPreliminary field results
Q Measurement:Q Measurement:Cruise : “SORTIE”Cruise : “SORTIE”Date : 17 oct 2008 – Date : 17 oct 2008 – 13h30 UT13h30 UTLocation: BOUSSOLELocation: BOUSSOLESun Zenith : 61.2° - Blue Sun Zenith : 61.2° - Blue SkySky560nm, integration time 560nm, integration time : 90ms: 90ms
““SORTIE” cruise: PI C. SORTIE” cruise: PI C. Trees, 2 weeks in Trees, 2 weeks in October 2008 in the October 2008 in the Mediterranean SeaMediterranean Sea
15
30
45
60
90
0 50 100 150 200 250 300
05
01
00
15
02
00
25
0
15
30
45
60
90
0 1 2 3 4 5
wave 560 - tilt: 1.5 H: 133056 - Qn: 3.31 1.5
Q
Q nadir comparisonQ nadir comparison
IV.IV. Preliminary field resultsPreliminary field results
Q comparison:Q comparison:Cruise : NATOCruise : NATODate : 26 oct 2008 Date : 26 oct 2008 – 13h30 UT– 13h30 UTPlace : SW PisaPlace : SW PisaSun Zenith : 61° - Sun Zenith : 61° - Blue SkyBlue Sky
““SORTIE” cruise: SORTIE” cruise: PI C. Trees, 2 PI C. Trees, 2 weeks in October weeks in October 2008 in the 2008 in the Mediterranean Mediterranean SeaSea
Q nadir Comparison 2008-10-26 Arno Plume
4
4.5
5
5.5
6
6.5
7
350 400 450 500 550 600 650 700
Wavelength (nm)
Q f
ac
tor
(sr)
SAtlantic hyper
SAtlantic hyper
JRC SAtlantic Multi
JRC SAtlantic Multi
LOV Camera S28
Qnadir comparisons between the camera and SAtlantic’s free fall profilersQnadir comparisons between the camera and SAtlantic’s free fall profilers
Q factor comparisonQ factor comparison
IV.IV. Preliminary field resultsPreliminary field results
Q comparison:Q comparison:Cruise : Optic-MedCruise : Optic-MedDate : 5,7 and 8 Mai Date : 5,7 and 8 Mai 2008 2008 Place : Mediterranean Place : Mediterranean seaseaBlue Sky, coastal blue Blue Sky, coastal blue waterswaters[Chla] : 0.116-1.24 [Chla] : 0.116-1.24 mg.mmg.m-3-3
““Optic-Med” cruise: 2 Optic-Med” cruise: 2 weeks in April 2008, in weeks in April 2008, in the Mediterranean Seathe Mediterranean Sea
3.0 3.5 4.0 4.5 5.0 5.5 6.0
3.0
3.5
4.0
4.5
5.0
5.5
6.0
Q nadir mod
Q n
ad
ir m
ea
s
ooooo
406 nm438 nm494 nm560 nm628 nm
Qnadir comparisons between the camera and the Morel&Gentili ModelQnadir comparisons between the camera and the Morel&Gentili Model
1:1
Thank you for your attentionThank you for your attention
Measurements of the in-water radiance fieldMeasurements of the in-water radiance field•History : Univ. Miami, RSMASHistory : Univ. Miami, RSMAS
Ken Voss 1988 –> present : Fish Eye camera coupled with a Ken Voss 1988 –> present : Fish Eye camera coupled with a CID (then a CCD) matrix and spectral filtersCID (then a CCD) matrix and spectral filters
Voss et al, 2007, BiogeosciencesVoss et al, 2007, Biogeosciences
Measurements of the in-water radiance fieldMeasurements of the in-water radiance field•History :History :
K. Voss 1988 – present : Fish Eye camera with CID (then CCD) K. Voss 1988 – present : Fish Eye camera with CID (then CCD) matrix and wavelength bandpass filtersmatrix and wavelength bandpass filters