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September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
1
Summary of Proposal Work Done at UAH to Set the Lunar Flux
ScaleWorkshop on Satellite Calibration for
Climate Change Research
David B. Pollock
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
2
Topics
Status of absolute and relative lunar flux uncertainties?
How to improve the absolute accuracy of the Lunar flux (data to develop moon as a standard to meet the requirements of the climate change research)?
• Is there a need to extend lunar observations to the infrared and what are the benefits for climate change research.
Ideas to implement solutions to use moon as a standard• What other ancillary radiometric measurements could be
made and benefits could be derived while measuring the lunar flux from above the atmosphere?
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
3
Proposal Effort Summary
• Background• Work began as a proposal to NSF in response to Solicitation 04-
522, due 2/26/04.• 5 year cost estimate $3.9 M >> $2.5 M NSF cost limit.• Proposal halted 2/18/04.• Response from relevance inquires to NSF
– Very important, but not relevant the NSF 04-522 solicitation,
– Encouraged to discuss work with Atmos. Sci. Prgm. Mgr. Dr. Moyers
• Support dollars needed to keep team together while NSF customer courted.
• A plus-up from Congress would help.• No help found.
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
4
BLAIRBalloon Lunar Absolute Irradiance Radiometer
A $4M dollar research opportunity.
4/1/2004
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
5
Goal
• Uncertainty SI < 2% will begin to eliminate the deficiency of exo-atmospheric radiometric standards, 300 to 2400 nm spectral region.
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
6
2005 - Relative and AbsoluteLunar Flux Data Uncertainty
• The ROLO lunar data is stable to better than 0.1% *
• There is a significant wavelength dependent uncertainty 5 – 15% SI.
• There is a bias ~ 6% when compared to satellite instrument measurements.
* Hugh H. Kieffer et al, On-orbit Calibration Over time and Between Spacecraft Using the Moon, SPIE 4881.
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
7
Error Budgets
Instrumentation Total Uncertainty, 2,%
NIST 0.02
(TBD)XR 0.2
SDL 1.0
ALIR 1.5
ROLO Model (RSS) 1.8
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
8
Participants - Responsibilities
• UAH (CAO and ECE) - PI, Radiometer, Pointing and ground station
• HARC - Balloon launch and recovery
• SDL - Repeated calibrations
• TBE - Payload fab, integ & qual test
• USGS - Side-by-side measurements at ROLO and data analysis
• NASA GSFC - Peer review and critique.
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
9
CostsOTAL SALARIES, WAGES & FRINGE $ 207,703 $ 241,323 $ 390,385 $ 237,227 $ 215,802 $1,292,441
OPERATING EXPENSES
Freight $ 642 $ 482 $ 2,091 $ 3,215
Subcontracts** $ 161,632 $ 577,124 $ 343,920 $ 316,624 $ 438,122 $1,837,422
Travel $ 1,132 $ 1,132 $ 3,644 $ 7,624 $ 9,582 $ 23,114
Optical Filters $ - $ 20,000 $ - $ - $ - $ 20,000
Detectors $ - $ - $ 20,000 $ - $ - $ 20,000
TOTAL OPERATING EXPENSES $ 162,764 $ 598,898 $ 367,564 $ 324,730 $ 449,795 $1,903,751
TOTAL DIRECT COSTS $ 370,467 $ 840,221 $ 757,949 $ 561,957 $ 665,597 $3,196,192
Facilities & Administrative Costs, 45.5% MTDC*** $ 121,182 $ 119,709 $ 209,996 $ 111,627 $ 112,601 $ 675,115
Ź Ź Ź Ź Ź
TOTAL ESTIMATED COST $ 491,649 $ 959,930 $ 967,945 $ 673,584 $ 778,198 $3,871,307
**Subcontracts: YR #1 YR #2 YR #3 YR #4 YR #5
1. TBE $ 105,332 $ 494,724 $ 195,720 $ 117,224 $ 96,840 $1,009,840
2. HARC $ 2,500 $ 2,500 $ 134,382 $ 139,382
3. USGS $ 48,800 $ 32,400 $ 45,700 $ 49,400 $ 61,900 $ 238,200
4. SDL $ 5,000 $ 50,000 $ 100,000 $ 150,000 $ 145,000 $ 450,000
5. NIST $ - $ - $ 100,000 $ 100,000 $ - $ 200,000
TOTAL SUBCONTRACTS $ 161,632 $ 577,124 $ 343,920 $ 316,624 $ 438,122 $1,837,422
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
10
NSF Interest SolicitationNovember 4, 2004
Dr. Jarvis L. MoyersDivision DirectorDivision of Atmospheric Sciences, 775 S
RE: Letter of inquiry dated February 18, 2004
Dear Dr. Moyers,
Thank you for your response to the letter of inquiry February 18, 2004.
Would the NSF consider an un-solicited proposal for either a high altitude balloon or aircraft program to directly tie the RObotic Lunar Observatory, ROLO, Lunar Flux Model to the International System of Units via the NIST high accuracy cryogenic radiometer, the HACR. This work is to support past as well as future radiometric calibrations for space-based observations of climate parameters. An estimated total program cost is in the $4 to $5M range.
The basic concept is build as simple and as stable a filter radiometer as technologically feasible and gather statistically
significant data sets from above most of the atmosphere, with NIST calibration immediately before and after each flight. In addition to three to five flights, there would be initial and final concurrent observations at the ROLO site. A NIST transfer device would provide the traceable path to SI units via the HACR.
Specific programs that would benefit from this work include SeaWiFS, ASTER, MODIS, ALI, MTI, Hyperion, MISR, and any NPP or NPOESS instrument that can view the Moon, e.g., VIIRS; Figure 1.
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
11
Figure 1
(Data/Model -1) %, Average of Data per Instrument.
Thomas C. Stone, USGS & Hugh H. Kieffer, Celestial Reasonings
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
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NSF ResponseProfessor Pollock,
If you have prepared your proposal in accordance with the guidelines in NSF 04 522then by all means go ahead and submit it by the published deadline. The accuracy ofatmospheric data used for atmospheric sciences research is also a matter of importance to us. You should be aware that this is likely to be a very competitivesolicitation as interest in this topic is currently very keen in the science and engineeringcommunities.
Jarvis Moyers
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
13
Notes from a conversation with Danny Ball, site manager at the National Scientific Balloon Facility on Friday, 16 April 2004.
1. A 75 kg payload carried to 25 km altitude is trivial.
2. The standard balloon sizes are 4 to 60 x 106 ft3 and anything smaller than 4 x 106
ft3 is a special.
3. Altitudes in the 25 to 30 km range are “small change”.
4. A 60 x 106 ft3 balloon will reach 45 km altitude and is 700 ft diameter.
5. A 60 x 106 ft3 balloon costs $180K and a 4 x 106 ft3 balloon costs $35K.
6. A 70 ft diameter parachute, for the smallest balloon payload, attaches directly to the balloon and is 110 ft long. There is a 65 ft cable ladder below the parachute. The payload attach point is the end of the ladder. If additional distance between the balloon and the payload is needed a second ladder can be added or a reel-down installed. The reel-down is 50 to 1000 ft in length.
7. A standard 4 x 106 ft3 balloon will carry a 200 kg payload to 33 km and the cost is $35K. A standard 4 x 106 ft3 balloon will lift up to 1500 kg.
8. A night launch out of Palestine in the June through August time period is routine.
9. There are no operational fees beyond the expendables. Expendables run about $50K per launch for a 4 x 106 ft3 balloon.
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
14
Notes Continued10. The 65 ft cable ladder provides torsional stiffness to push against for azimuth
rotation. Three arc-second pointing has been achieved hanging from a balloon.11. The atmospheric guys at JPL may have a payload frame we could borrow.12. There is a standard Consolidated Instrument Package available.
1. NSBF will track the payload.2. They will terminate the flight.3. They will recover the payload.4. The CIP will collect and record the data.5. The CIP can be used to send commands.
13. The NSBF requirements are 1. A stress analysis that shows the payload can survive 10 g vertically (parachute opening)
and 5 g @ 45° (landing),2. For a simple gondola, a hand calculation is adequate,3. An electronics compatibility test pre-launch.
14. Users outside the NASA community will be charged for expendables and a nominal user fee all payable to Wallops Island, VA.
15. The process to get on the NSBF schedule starts with a request for a Flight Request Form.
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
15
Topics
Status of absolute and relative lunar flux uncertainties? How to improve the absolute accuracy of the Lunar
flux (data to develop moon as a standard to meet the requirements of the climate change research)?
• Is there a need to extend lunar observations to the infrared and what are the benefits for climate change research.
Ideas to implement solutions to use moon as a standard• What other ancillary radiometric measurements could be
made and benefits could be derived while measuring the lunar flux from above the atmosphere?
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
16
Topics
• The problem
• Working on a solution
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
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• Operational envelope• Critical parameters and functions
• Relative spectral response, in-, out-of-band. • Absolute response• Saturation response• Dark off-set• Non-linearity of response vs temperature• Relative response over field of regard• Distortion map over field of regard• Response vs array, electronics temperature• Focus (energy on a pixel)• Pixel fill-factor• Response to out-of-field-of-view sources• Gain normalization
• Repeated observations
Total Uncertainty“Truth”
Chambers 1 ~ 2%
Stars 1.5 ~ 2.5%
Moon 6 ~ 15%
Sun 0.1 ~ 2%
Terrestrial ~ 20%
A2 = P2 + B2 + (SNR)-2 + “T” 2
B
- Taylor, B.N., Kuyatt C. E., Guidelines for Evaluating and Expressing the Uncertainty of NIST Measurement Results, NIST Technical Note 1297, 1994
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
18
Heuristic SI Traceability* Path
Reference sources
International System of Units, SIConvention of the Metre
Transfer radiometers
Remote sensors Orbital, Airborne, Terrestrial
Calibration sourcesSun, Moon, Stars, Terrestrial
National Measurement Institutes
* “Property of the result of a measurement … whereby it can be related to stated references… through an unbroken chain ofcomparisons all having stated uncertainties.” International Vocabulary of Basic and General Terms in Metrology (VIM), Estler, CALCON 2004 Workshop
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
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Current Path
• Transfer measurements in situ.– A set of measurements of Vega at 0.5556 m.*
• Data analysis, multiple observers, instruments and sites.
*Hayes, Calibration of Fundamental Stellar Quantities, Proc. IAU Symposium No. 111 (1985)
Vega
Striplamp, hundredsof meters distant
Pt or Au point cavity,inside dome, aftertelescope optics.
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
20
Planned Path
• Polychromatic to span the ROLO range, 0.34 – 2.4 m.– Combined ROLO bands.
– Individual, fixed bandpass filters.
• HACR – (TBD)XR – MIC – ALIR• Joint ROLO & ALIR observations.• Repeated ground calibrations.• Analysis
ALIR @ 12 -45 km
Moon Stars
ROLO & ALIRSDL NIST - SI Units(TBD)XR
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
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Topics
• The problem
• Working on a solution for the Lunar Irradiance
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
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Rationale
• What – Reduce the ROLO Lunar Irradiance Model uncertainty.
• Why – Remote sensors are being tasked to produce ever more accurate data.
• How – Iterative calibrations, coupled with comparative measurements in the field and laboratory.
• Who – Trained, qualified participants.• When – Needed now.
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
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ALIR
• Selectable band pass filters– Calibrated at NIST– Common to ROLO– Located near aperture stop
• High out-of-field light rejection– Hard field & aperture stops
• Internal reference source to monitor stability
Detectors
Entrance pupilField stop
Aperture stop
19 bandpass filters + BlankNear aperture stop
FOV = 0.5F No. = 10
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
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ROLO Bands, 32Lunar Spectral Irradiance, 2° / 15°
0.0
10.0
20.0
30.0
40.0
50.0
60.0
300 800 1300 1800 2300 2800
Wavelength, nm
Sp
ectr
al I
rrad
ian
ce,
nW
/cm
^2-
nm
2°
15°
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
25
ROLO Bands Combined,19Combined Bands Spectral Irradiance
0
10
20
30
40
50
60
300 800 1300 1800 2300 2800
Band center, nm
Sp
ecra
l Ir
rad
ian
ce,
nW
/cm
2 - n
m
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
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Dynamic Measurement Range Small
Lunar flux dynamic range, 2° - 15°
1.00
1.50
2.00
300 600 900 1200 1500 1800 2100 2400
Wavelength, nm
Ra
tio
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
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S/N, 1 cm Aperture, Selected - Combined ROLO Bands
1.E+00
1.E+01
1.E+02
1.E+03
1.E+04
300 600 900 1200 1500 1800 2100 2400
Wavelength, nm
S/N
Rat
io
1.0E-01
1.0E+00
1.0E+01
Co
mb
ine
d b
an
d i
rrad
ian
ce
, W
/ c
m 2
Si Phototdiode
PV HgCdTe
Comb. Bands Irr.
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
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Spurious Flux Control
1.E-20
1.E-17
1.E-14
1.E-11
1.E-08
1.E-05
1.E-02
Off-axis angle, deg
Fra
cti
on
, po
we
r
Total
Scatter
Diffraction
Field-of-view edge
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
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Az-El Gimbals
Acquisition / Track
ALIR
ECI Position Data storage and transmission
Housekeeping
Command &Control
Flight System
Aircraft
Ground station
Balloon or
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
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Estimated Parameters18-Jan-04
Part Power Part Perf.Kg lb w
Radiometer Walls 4.95 10.91 RadiometerEnd plates 1.20 2.65 Accuracy 0.10%Fittings 0.50 1.10 SensitivityInterior parts 2.00 4.41 OARLN2 (5 liter) 5.00 11.01 Spectral bands* 19
Total 13.65 30.07 0.5 Bandwidths* 8 to 58 nmOperating Temp
Electronics ResponsivityAmplifiers 1.00 2.20 Integration timesHousekeeping 1.00 2.20 Hold time at tempInterface 1.00 2.20 Detector materialsCmd / cntl 1.00 2.20 Spectral range* 320 to 2410 nmCables 1.00 2.20Communications 1.00 2.20Tracking 1.00 2.20 Gimbals
Total 7.00 15.42 10 Slew rateTrack rate
Pointing / Stabilization StabilityTrack tele. 2.00 4.41 Cage / un-cageGimbals 3.00 6.61
Total 5.00 11.01 20Track telescope
Balloon connections Field-of-viewSupport / release 5.00 11.01 OARParachute 5.00 11.01 Spectral band
Total 10.00 22.03 SensitivityAperture
Structure Track uncertaintyHardware 10.00 22.03Landing cushion 5.00 11.01
Total 15.00 33.04
PayloadTotal 50.65 111.57 30.50
Draft Requirements
Weight
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
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ScheduleAdvanced Remote Sensing with BLAIRFebruary 23, 2004
Task Year 4.50 Fractional Year for computation 4.5 4.8 5.0 5.3 5.5 5.8 6.0 6.3 6.5 6.8 7.0 7.3 7.5 7.8 8.0 8.3 8.5 8.8 9.0 9.3
2004 Year: 2000+ 4 4 5 5 5 5 6 6 6 6 7 7 7 7 8 8 8 8 9 93 Quarter 3 4 1 2 3 4 1 2 3 4 1 2 3 4 1 2 3 4 1 2
Tasks1 System Performance Analysis (UAH, USGS, TBE, SDL, NIST) x x x
1.1 SI Traceability1.2 Requirements Definitions1.3 Specifications Flow Down1.4 Experiment Planning
2 Pointing & Control (UAH, ECE, TBE) x x x x x x x x x x2.1 Design / analysis / model / fabricate2.2 Gimbals (CAO, ECE , TBE)2.3 Acqusition & Tracking (ECE, CAO, TBE)
3 Electronic Packages (ECE, TBE) x x x x x x x x x x3.1 Design / analysis / model / fabricate3.2 Communication3.3 Data 3.4 Tracking3.5 Cables3.6 Housekeeping3.7 Payload Transmitter3.8 Ground Station Receiver
4 Flight System (HARC, CAO) x4.1 Design / analysis / model / specify4.2 Balloons for flight4.3 Release system4.4 Parachute system4.5 Landing system
5 Radiometer (CAO, USGS, NIST, SDL) x x x x x x x x x x5.1 Design / analysis / model / fabricate5.2 Fabricate (Engr & Flt)5.3 Engr Model Test at UAH / TBE x5.4 Ship Engineering Model to SDL x5.5 Ship Flight Model to SDL x
6 Calibration (SDL, NIST, CAO, USGS) x x x x x x x x x x x6.1 Planning6.2 On-site calibrations at NIST x6.3 On-site calibrations at SDL, 4 times x x x x
6.4 ROLO - ARS Simultaneous Observations x x
7 Payload (TBE) x x x x x x x x x x x x x7.1 Design / analysis / model / fabricate7.2 Integration7.3 Test
8 Operations (HARC, UAH, USGS) x x x8.1 Launch & Recovery8.2 Inflation supplies8.3 Transportation8.4 Travel
1 5432
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
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Management PlanPoint Design for the Lunar Ballloon experiment Calendar
DaysSimple Schedule Who /Task Sum Cum
Specifiy mass and power for Radiometer DP 3.3 3.3Select detector type[s] 1SNR Calculations 0.5Decide how many bands 0.5Filter-wheel design 0.5
How is it driven. 0.5Decide on Optics and ApertureEstimate moment of inertia DP 0.3
last summed
Specify pointing requirements 2.5 5.8How close can GPS get? ? 0.5What is Balloon stability? BB 1What is radius of radiometer centering control? DP 0.5How well must radiometer point? DP 0.5
last summed
Moon locator [if needed] 3 8.8What layout? (Quadrent of triangles? CJ 1What detectors? DP 1What is feedback control? CJ 1
last summed
Pointing system 9 17.8will any COTS do? CJ 3
If so, specify CJ 1If not, design CJ 4
Estimate mass CJ 0.5Estimate power CJ 0.5
last summed
Electronics 2 19.8Define nominal flight plan DP 1
How much control from the ground "How much Autonomous "
Estimate data quantity DP 0.5What is stored on-board versus via telemetry " 0.2
Define Communications requirements " 0.3last summed
Payload & Structure 5 24.8Payload Power estimate DP 0.5
Estimate battery mass CJ 0.5Payload mass estimate DP 1
Ballon size required BB 3last summed
Assemble Proposal 5.5 30.3Write draft Calibration plan DP 2Decide on Engineering vrs Flight models DP,TS 0.5Write Science justification DP,HK 1
Application to spacecraft calibration HK,TS 0.5Discuss how results enter into the ROLO Irradiance model HK,TS 0.5Estimate Project Costs DP 1
last summed
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
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Trained, Qualified Participants
• SI traceable path– NIST– Space Dynamics Laboratory– USGS
• Iterative flights– Balloon, National Scientific Balloon Facility – Aircraft, SOFIA
• Payload & Operations – UAH• Data Analysis – USGS, UAH• Peer review and critique – NASA GSFC
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
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Activities• Stabilization, pointing and position.
– Alt-az gimbals w/ 1” pointing, build or borrow.– GPS and lunar ephemeris from vehicle.
• Balloon, routine– > 25 km w / a 4 x 106 ft3 volume. – 70 ft diameter by 110 ft long parachute. – Payload attached to the end of 65 ft cable ladder below the parachute.– Added distance between balloon - payload possible w / a second ladder or a
1000’ reel-down. • Aircraft SOFIA.
– 12.5 – 13.5 km– 3+ years away
• Repeated pre-, post-flight Sensor calibrations.• Concurrent observations w / ROLO telescopes in Flagstaff.• Data reduction and error analysis
– Statistically significant data set– 100 s data on 30 successive days or 100 s on 12 selected days / year
• Ingest archive data
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
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Conclusion
• A relatively small, < 5 cm aperture, well baffled, <10-11 @ 1, multi-spectral, 340 – 2,400 nm radiometer, limited dynamic range, <2, is feasible.
• Setting the ROLO Model scale < 2% is a reasonable task.
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
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Backup Charts
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
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Reducing the RObotic Lunar Observatory (ROLO) Irradiance
Model Uncertainty SI David B. Pollock1, Thomas C. Stone2, Hugh H. Kieffer3, Joe P. Rice4
1. The University of Alabama in Huntsville, 301 Sparkman Drive, OB 422, Huntsville, AL 35899
2. U.S. Geological Survey, 2255 N. Gemini Drive, Flagstaff, AZ 860013. Celestial Reasonings, 2256 Christmas Tree Lane, Carson City, NV 897034. National Institute of Standards and Technology, 100 Bureau Drive, MS 8441,
Gaithersburg, MD 20899-8441
This page and the next as well as many of the preceding pages are from the CALCON Presentation of August 26, 2004.
September 28, 2005 - NIST
Workshop - Moon as a Standard for Satellite Sensor Calibration for Climate Change
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AbstractThere is a fundamental remote sensing problem, the inability to identify and to correct biases to the
level that current sensor technology permits once a sensor becomes operational in-orbit. This paper presents a concept, retrieval and recalibration of a transfer standard, to reduce in the longer term the uncertainty of the flux from the stars, the solar flux and vicarious sources on the earth using the RObotic Lunar Observatory, ROLO, Irradiance Model as the basis for a technology demonstration. The cause of the fundamental remote sensor problem is the uncertainty of the respective fluxes traced to the International System of Units, SI. This includes the sensors relative to the U. S. Global Climate Change Research Program (U.S. GCRP), sensors for NASA, NOAA, TVA, DoD, DOE, HHS, NSF, USDA, DOI and EPA. An effort to solve this fundamental problem began about 7 years ago with the emergence of the problem at a NIST Workshop in the fall of 1997 and stated in NIST GCR 98-748, High Accuracy Space Based Remote Sensing Requirements, March 1998. Since then there has been expanding recognition and discussion of this remote sensing deficiency at National and International conferences and workshops. Remote sensor data shows that remote sensors are on the order of 4 to 5 times more stable than the uncertainty of either the spectral or total radiant flux from the moon, the stars and the sun. The consequence is data uncertainty increases because there are not adequately uncertain calibration sources available to remove the remote sensor biases that arise during operations. The concept presented by this paper when implemented would begin an effective, systematic attack on the larger problem, the stars, the sun and terrestrial, by attacking a most glaring deficiency of the recognized, accepted ROLO Lunar Irradiance model. Although the lunar data is stable to better than 0.1% there is a significant wavelength dependent uncertainty on an absolute scale thought to be on the order of 5 – 15% SI. A bias of up to 6% is found when results are compared to satellite instrument measurements. Reducing this uncertainty SI will begin to eliminate the deficiency of exo-atmospheric radiometric standards specifically for those remote sensors that can use the lunar flux over the 300 to 2300 nm spectral region for calibration.