Update on the VIIRS Sensor - NASA€¦ · 5 NPP Sensors • The Visible Infrared Imaging...

51
1 Update on the VIIRS Sensor Presented to the MODIS Science Team July 22, 2002 Dr. Robert E Murphy NPP Project Scientist Code 920 NASA GSFC

Transcript of Update on the VIIRS Sensor - NASA€¦ · 5 NPP Sensors • The Visible Infrared Imaging...

Page 1: Update on the VIIRS Sensor - NASA€¦ · 5 NPP Sensors • The Visible Infrared Imaging Spectroradiometer Suite (VIIRS) extends measurement series initiated by MODIS on EOS Terra

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Update on the VIIRS Sensor

Presented to the MODIS Science Team

July 22, 2002

Dr. Robert E MurphyNPP Project Scientist

Code 920NASA GSFC

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What is NPP?

• NPP is a “bridging mission” that provides for the continuation ofmeasurement series initiated with EOS Terra & Aqua for NASA’sglobal change research

– Climate change

– Global carbon cycle

– Global water cycle

• NPP provides risk reduction for the National Polar-OrbitingOperational Environmental Satellite System (NPOESS) which willcontinue these measurements into the indefinite future

• NPP is a joint program of NASA and the Integrated Program Office(IPO), the tri-agency activity that is responsible for NPOESS

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What is the NPOES Mission?

Mission

Provide a national, operational, polar-orbiting environmental capability

Achieve National Performance Reviewsavings by converging DoD and NOAApolar satellite programs

Incorporate new technologies fromNASA and others

Incorporate, where appropriate,International Cooperation (EUMETSAT)

Local Equatorial CrossingTime

0530

13300930

METOP

NPOESS

METOP

NPOESS

NPOESS

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CY 99 00 11 12 13 14 15 16 17 1803 08 09 1001 02 0704 05 06

Earliest AvailabilityS/CDeliveries

0530

1330

DMSP

0730 -1030

NPOESSC3

POES

EOS-Aqua

NPOESSC2 or C1N’

Earliest Need to back-up launch

F20

NPOESSDMSP

POES

NPPEOS-Terra

METOP

NPOESSC1 or C2

F16

N

MF17 F19F15

F18

L (16)

WindSat/Coriolis

Satellite Transition Schedule(9 March 2001)

Slopes indicate 10-90% need (NPOESS GAP 5b)

Projected End of Life based on 50% Need

Loca

l Eq

uat

ori

al C

ross

ing

Tim

e

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NPP Sensors

• The Visible Infrared Imaging Spectroradiometer Suite (VIIRS) extendsmeasurement series initiated by MODIS on EOS Terra & Aqua

– Design is evolutionary from MODIS

• The Cross-track Infrared Sounder (CrIS) continues measurementseries initiated by AIRS on EOS Aqua

– Utilizes a Michelson interferometer in contrast to AIRS, which is aspectrometer

• The Advanced Technology Microwave Sounder (ATMS) continues themeasurement series initiated by the AMSU on NOAA-15

– MMIC Technology used to reduce mass, power & volume

• An Instrument of Opportunity is under consideration– Aerosol Polarimeter Sensor– CERES– OMPS– SAGE III– Code S payload– Decision August 2002

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NPP & NPOESS Orbits

• NPP has 824 km Sun synchronous orbit– 10:30 AM descending node– 98.74° inclination– Mimics Terra ground track repeat

> 16 day ground-track repeat

– Swath width 0f 3,000 Km (±56.06°)

• NPOESS has 833 km Sun synchronous orbits– All 3 satellites will carry a VIIRS

> 09:30 descending node> 13:30 ascending node> 17:30 ascending node

– Swath width of 3,000 km (±56.06°)

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Operational & Research Data Products

• The operational system (NPOESS) will produceEnvironmental Data Records (EDR’s) of geophysicalproducts in less than 90 minutes from acquisition– Timeliness requirement limits accuracy & consistency that can

be obtained

– Yesterday’s weather is of limited use

• NASA’s program requires maximum accuracy andconsistency over many years– Timeliness is not an issue

• NASA will produce similar geophysical products in the formof Climate Data Records (CDR’s)

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Visible Infrared Imaging Radiometer Suite (VIIRS)

• Purpose: Global observationsof land, ocean, & atmosphereparameters at high temporalresolution (~ daily)

• Predecessor Instruments:AVHRR, OLS, MODIS, SeaWiFS

• Management: IntegratedProgram Office

• Status:Phase C/D (Raytheon)

• Approach: Multi-spectralscanning radiometer (22 bandsbetween 0.4 µm and 12 µm)12-bit quantization

• Swath width: 3000 km

• Changes to specifics of banddynamic ranges, bandpasses& band centers negotiated

• Consideration of adding 6.7micrometer water vapor bandto FM3 & later models

• CDR Completed March 2002

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Visible Infrared Imaging Spectroradiometer (VIIRS)

Cryoradiator

4-Mirror AnastigmatAll Reflective

Aft Optics Imager

3-Mirror AnastigmatAll reflective

Rotating telescope

FPIE

Solar Diffuser

Blackbody

Half-angle Mirror

Separately Mounted Electronics Module

Cold FPADewar Assembly

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VIIRS Spectral Bands

• 22 Bands– Subset of MODIS bands plus day-night panchromatic band

• Two spatial resolutions– Imagery resolution bands: 370 m at nadir

– Moderate resolution bands: 740 m at nadir

• Features– 8 (Moderate) or 16 (Imagery) detectors per scan

– Bands spatially nested

– Some bands have dual gain> Maximize dynamic range without precision penalties

• Constrained pixel growth with scan angle

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VIIRS Optimized Bandset Supports All EDRs

Band name DNB M1 M2 M3 M4 I1 M5 M6 M7 I2 M8 M9 M10 I3 M11 M12 I4 M13 M14 M15 I5 M16Band position 700 412 445 488 555 645 672 751 865 865 1.2 1.4 1.6 1.6 2.3 3.7 3.7 4.1 8.6 10.8 11.5 12.0Band width 400 20 18 20 20 50 20 15 39 39 0.02 0.015 0.06 0.06 0.05 0.18 0.38 0.16 0.30 1.00 1.90 0.95

ImagerySea Surface Temp.Soil MoistureCloud Cover/LayersCloud Partical SizeCloud Thickness Cloud Top HeightCloud Top PressureCloud Top Temp. Land Surface Temp.FireVegetation IndexSnow Cover (Binary)Snow Cover (Fraction)Vegetation/TypeAlbedoFresh Water IceIce Surface Temp.Littoral TransportNet Heat FluxOcean Color/Chloro.Sea Ice age/motionMass (turbidity)Aer Opt Thick (Ocean)Aer Opt Thick (Land)Aer Part Size (Ocean)Aer Part Size (Land)Suspended Matter Total Prec. WaterCloud Mask

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0

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1

0.4 0.48 0.56 0.64 0.72 0.8 0.88 0.96

8 9 10 11MODIS: 12 13/14 15 16

MODIS Ocean Bands in the Vis/NIR

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0

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8 9 10 11MODIS: 12 13/14 15 16

Ocean Bands: MODIS - VIIRS TransitionR-1 R-2 R-3VIIRS: R-4 R-5 R-6 R-7

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0

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R-1 R-2 R-3VIIRS: R-4 R-5 R-6 R-7

VIIRS Ocean Bands in the Vis/NIR

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0

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5MODIS: 6 7

Deciduous

MODIS Land Bands in the NIR

Sand

Dark Soil

Snow

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1 1.2 1.4 1.6 1.8 2 2.2 2.4 2.6

5MODIS: 6 7

Deciduous

MODIS & VIIRS Land Bands in the NIR

Sand

Dark Soil

Snow

R-8 R-10/I-3VIIRS: R-11

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0

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1 1.2 1.4 1.6 1.8 2 2.2 2.4 2.6

Deciduous

VIIRS Land Bands in the NIR

Sand

Dark Soil

Snow

R-8 R-10/I-3VIIRS: R-11

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0

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6 8 10 12 14

MODIS:

MODIS Atmospheric Bands in the LWIR

27 28 29 34 363530 31 32 33

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0

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1

8 8.8 9.6 10.4 11.2 12 12.8 13.6

MODIS:

MODIS Atmospheric Bands in the LWIR

29 31 32

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8 8.8 9.6 10.4 11.2 12 12.8 13.6

MODIS:

MODIS & VIIRS Atmospheric Bands in the LWIR

29 31 32R-14VIIRS: R-15 I-5 R-16

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0

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VIIRS Atmospheric Bands in the LWIR

R-14VIIRS: R-15 I-5 R-16

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Detector Aggregation Reduces Pixel Growth

742 m 1104 m 1600 m

630 m

1260 m1600 m

262 m

786 m

Nadir 1700 km 3000 km• aggregate 3 samples• SNR increases by sqrt(3)

• no aggregation• aggregate 2 samples• SNR increases by sqrt(2)

Radiometric (“Moderate-Resolution”) Bands

371 m 552 m 800 m

315 m

630 m800 m

131 m

393 m

Nadir 1700 km 3000 km

• aggregate 3 samples• SNR increases by sqrt(3)

• no aggregation• aggregate 2 samples• SNR increases by sqrt(2)

Imaging (“High-Resolution”) Bands

Moderate and Imaging bands nest 2x2

To ~

To ~

VIIRSReducesPixel Size

AlongScan:

MuchBetter

HSR, SNRTowardNadir

AVHRR& MODIS“1 km”Bands:~2x6kmAt Edge

Vs.

VIIRS1.6x1.6 km

At Edge

HorizontalSamplingInterval

HorizontalSamplingInterval

to 1060km

to 1060km

To

To

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Reduced Pixel Growth Along Scan

Scan HSI as a Function of Scan Angle

for Unit Raw GSD at Nadir

0123456789

10111213141516171819

0 8 16 24 32 40 48 56

Scan Angle (degrees)

Raw GSD (No Agg)

Agg 2 in Scan

Agg 3 in Scan

VIIRS HSI

HSI Returns to Nadirsize at the two transition

points (31.71o and 47.87

o)

Rati

o o

f O

ff-n

ad

ir p

ixel to

nad

ir p

ixel

~1500 km

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Calibration

• Stray light much better than MODIS– Driven by needs of the day-night (DNB)– Rotating telescope, extensive baffling reduces scattered light

• V-grove blackbody similar to MODIS– Baffled to avoid Earth illumination– Emissivity of 0.9998– Controlled to 290K by pulsed voltage– Heat to 315K

• Solar Diffuser (SD) evolutionary from MODIS– 1 time door– New design eliminates “ripples”

• Solar Diffuser Stability Monitor (SDSM) evolutionary from MODIS– 7 bands– Views 70% of SD area

• Planning to use 2nd order polynomial for all bands• Characterization plan similar to MODIS• Lunar views possible

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Some Issues

• Dynamic range for fire is inadequate– Similar issue faced on MODIS– “Imagery” & SST are the two highest priority EDRs for the IPO– “MODIS compromise” not acceptable– Multi-band algorithmic solution may be possible

• 645 nm band (I-1) dynamic range increased to avoid saturatedpixels for imagery

– Spectral requirements changed from center wavelength of 645nm (50nm wide) to 640nm (80nm wide)

– Modest compromise to VI work

• 751 nm band (M-6) center wavelength changed from 751nm to746nm

• NASA geolocation requirement (200 m 3 σ) not an IPO requirement– Margin is eroding to achieve this accuracy

• Consideration being given to adding 6.7 micrometer band for FM3& beyond

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Fine Scale WV Depiction MODIS 1 km resolution reveals mountain waves

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Imagery Energy Budget/Spectral Adapted Y2466

SST 4-Channel Skin--ATSR, MODIS Adapted (ATSR, Brown, Emery) Y2386Air-mass classificationCirrus, aerosol mitigation

Soil Moisture CMIS/VIIRS Data Fusion Adapted (Carlson) Y2387

Aerosol Optical Dark Pixel Method Adapted (Kaufman, Tanre, Vermote) Y2388Thickness, Particle Developed radius (Vermote)Size, Effective Radius

Suspended Matter Multiple Indices & Adapted Y2390Dominant Type

Cloud Base Height Cloud Property LUT Adapted (Hutchison, Wilheit) Y2391

Cloud Cover/Layers Clustering based on cloud properties Adapted Y2392

Cloud Effective UCLA Ice & Water Adapted (Ou, Liou) Y2393Particle Size

Cloud Top Height, UCLA Ice & Water IR Adapted (Ou, Liou) Y2395Temp., Pressure

Algorithm Development Status (1 of 3)and Delivery of the V5 ATBDs

EDR Final Baseline Adopted/Adapted/Developed ATBD#

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Albedo, Surface Bright surfaces: Linear regression Adapted (Liang) Y2398Dark surfaces: MODIS kernel-driven Adapted (Strahler, Lucht, Schaaf)

Land Sfc. Temp 4-Channel Land Cover Adapted Y2399

Vegetation Index NDVI, EVI Adapted (Tarpley, Deering, Huete) Y2400FPAR, LAI, NPP, PSN Adapted (Running, Knyazikhin, Myneni)

Snow Cover/Depth Spectral Mixture Adapted (Hall, Dozier) Y2401

and MODISthreshold

Surface Type Decision Tree Adapted (Townshend, DeFries) Y2402

Fresh Water Ice Energy Budget/Spect. Mix. Adapted Y2404

Ice Surface Temp. Split Window Adapted Y2405

Algorithm Development Status (2 of 3)

EDR/SDR Final Baseline Adopted/Adapted/Developed ATBD#

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Net Heat Flux Regression/Neural/Bulk Adapted (Ruprecht, Liu) Y2407

OC/Chlorophyll Carder/MODIS Case 2 Adapted (Carder) Y2408Regionally tuneable

Ocean Atmos. Corr. Improved SeaWiFS Adapted (Gordon, Wang, Liu) Y2411

With full residual (IP)polarization handling

Sea Ice Age/Edge Maximum Cross-Correlation Adapted (Emery) Y2409

Land Atmos. Corr. Radiative Transfer LUT (MODIS) Adapted (Vermote) Y2411(Surface Reflectance) (IP)

Cloud Mask Thresholding/Phase Adapted (MODIS/CLAVR, Stowe) Y2412

Precipitable Water Five-band TIR Adapted (Huang) Y3251

Active Fires Raytheon HSS/MODIS Adapted (HSS, Giglio/Justice/Kaufman) Y3252

(ARR)

Algorithm Development Status (3 of 3)

EDR Final Baseline Adopted/Adapted/Developed ATBD#

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NRA Status

• An NRA for an initial science team for NPP is nearingrelease

• The team will assist NASA in preparing to use theoperational system for long term climate research– Which EDRs can be used as CDRs?

– What steps need to be taken to assure climate quality data?

– Use simulations based on real and synthetic data sets

– Provide insight into sensor characterization

• A second science team selection will be made closer to thelaunch of NPP

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Summary

• MODIS quality measurements will be continued in theoperational system (NPOESS)

• VIIRS draws heavily on its MODIS heritage

• Some research capabilities (e.g. fluorescence, CO2 slicingbands) are not continued

• Overall similar radiometric quality

• Improved geometric resolution

• Continued commitment to characterization and calibration

• NASA science team to be competed soon

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Back-Up Charts

• Land Vis-NIR Bands

• Ocean SWIR Bands

• Atmosphere Vis-NIR Bands

• Atmosphere SWIR Bands

• Atmosphere MWIR Bands

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0

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3MODIS: 4 1 2

Snow

Sand

Deciduous

Dark Soil

MODIS Land Bands in the Vis-NIR

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3MODIS: 4 1 2

Snow

Sand

Deciduous

Dark Soil

MODIS & VIIRS Land Bands in the Vis-NIRR-1 R-3VIIRS: R-4 R-5 R-7/I-2I-1

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Snow

Sand

Deciduous

Dark Soil

VIIRS Land Bands in the Vis-NIR

R-1 R-3VIIRS: R-4 R-5 R-7/I-2I-1

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Back-Up Charts

• Land Vis-NIR Bands

• Ocean SWIR Bands

• Atmosphere Vis-NIR Bands

• Atmosphere SWIR Bands

• Atmosphere MWIR Bands

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0

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3.2 3.4 3.6 3.8 4 4.2

MODIS: 20 2321-22

MODIS Ocean Bands in the SWIR

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0

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MODIS: 20 2321-22

MODIS & VIIRS Ocean Bands in the SWIRVIIRS: R-12 R-13

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Back-Up Charts

• Land Vis-NIR Bands

• Ocean SWIR Bands

• Atmosphere Vis-NIR Bands

• Atmosphere SWIR Bands

• Atmosphere MWIR Bands

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0

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3MODIS: 4 1 2 17 18/19

Deciduous

MODIS Atmospheric Bands in the Vis-NIR

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0

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0.4 0.48 0.56 0.64 0.72 0.8 0.88 0.96

3MODIS: 4 1 2 17 18/19

Deciduous

MODIS & VIIRS Atmospheric Bands in the Vis-NIRR-1 R-3VIIRS: R-4 R-5 R-7/I-2I-1

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0

0.2

0.4

0.6

0.8

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0.4 0.48 0.56 0.64 0.72 0.8 0.88 0.96

Deciduous

VIIRS Atmospheric Bands in the Vis-NIR

R-1 R-3VIIRS: R-4 R-5 R-7/I-2I-1

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Back-Up Charts

• Land Vis-NIR Bands

• Ocean SWIR Bands

• Atmosphere Vis-NIR Bands

• Atmosphere SWIR Bands

• Atmosphere MWIR Bands

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0

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1 1.2 1.4 1.6 1.8 2 2.2 2.4 2.6

5MODIS: 26 6 7

Deciduous

MODIS Atmospheric Bands in the NIR

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5MODIS: 26 6 7

Deciduous

MODIS & VIIRS Atmospheric Bands in the NIRR-8 R-9 R-10/I-3VIIRS: R-11

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0

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0.6

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1 1.2 1.4 1.6 1.8 2 2.2 2.4 2.6

Deciduous

VIIRS Atmospheric Bands in the NIR

R-8 R-9 R-10/I-3VIIRS: R-11

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Back-Up Charts

• Land Vis-NIR Bands

• Ocean SWIR Bands

• Atmosphere Vis-NIR Bands

• Atmosphere SWIR Bands

• Atmosphere MWIR Bands

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MODIS & VIIRS Atmospheric Bands in the MWIRVIIRS: R-12 R-13I-4

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VIIRS: R-12 R-13I-4