goes-r coastal waters imaging and the coast risk reduction activities

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GOES-R Coastal Waters Imaging and the COAST Risk Reduction ActivitiesGOES-R Coastal Waters Imaging and the COAST Risk Reduction Activities

Curtiss O. DavisCollege of Oceanic and Atmospheric Sciences

Oregon State University, Corvallis, Oregon 97331

[email protected]

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Presentation OutlinePresentation Outline

• Hyperspectral Environmental Suite-Coastal Water Imaging capability (HES-CW) is planned for GOES-R.

• First ocean color measurements from geostationary orbit to provide frequent imaging of coastal waters to– Resolve coastal dynamics and tides– Provide cloud clearing

• Why HES-CW given VIIRS on NPOESS?• Example Products• The Coastal Ocean Applications and Science Team (COAST)

and planned Risk Reduction Activities• Summary

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Visible Infrared Imaging Radiometer Suite (VIIRS)

Visible Infrared Imaging Radiometer Suite (VIIRS)

• Being built by Raytheon SBRS

– SeaWiFS and MODIS heritage

• First flight on NPOESS Preparatory Project (NPP) in 2008 then NPOESS satellites starting in 2011

• Seven ocean color channels and 2 SST channels

ChannelName

channel Center

Channel Width

Ltypical ocean

Required SNR/NET

VIIRS SNR/NET

M1 412 nm 20 nm 44.9 352 670 M2 445 nm 18 nm 40 380 506 M3 488 nm 20 nm 32 415 515

M4 555 nm 20 nm 21 361 446

M5 672 nm 20 nm 10 242 ~ 400

M6 751 nm 15 nm 9.6 199 ~ 400

M7 865 nm 39 nm 6.4 215 314

M15 10.8 m 1.0 m 300K .070 .041

M16 12.0 m 1.0 m 300K .072 .041 M

•Approximately 1 km GSD ocean color–742 m GSD and Nadir, 1092 m at +/- 850 km, 1597m at End of Scan (+/- 1500 km)–Designed to meet global ocean imaging requirements at 1 km GSD –Maximum revisit frequency of twice a day at 1030 and 1530

•Approximately 1 km GSD ocean color–742 m GSD and Nadir, 1092 m at +/- 850 km, 1597m at End of Scan (+/- 1500 km)–Designed to meet global ocean imaging requirements at 1 km GSD –Maximum revisit frequency of twice a day at 1030 and 1530

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Why HES-CW given VIIRS?Why HES-CW given VIIRS?

• Tides, diel winds (such as the land/sea breeze), river runoff, upwelling and storm winds drive coastal currents that can reach several knots. Furthermore, currents driven by diurnal and semi-diurnal tides reverse approximately every 6 hours.

• VIIRS daily sampling at the same time cannot resolve tides, diurnal winds, etc.

• HES-CW Can resolve tides from a geostationary platform and will provide the management and science community with a unique capability to observe the dynamic coastal ocean environment.

• HES-CW will provide higher spatial resolution (300 m vs. 1000 m)

• HES-CW will provide additional channels to measure solar stimulated fluorescence, suspended sediments, CDOM and improved atmospheric correction. Example tidal cycle from

Charleston, OR. Black arrows VIIRS sampling, red arrows HES-CW sampling.

Example tidal cycle from Charleston, OR. Black arrows VIIRS sampling, red arrows HES-CW sampling.

These improvements are critical for the analyses of coastal waters.

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MODIS1 km water clarity

Modeled HES-CW (250 m)

HES-CW higher spatial resolution critical to monitor complex coastal waters

HES-CW higher spatial resolution critical to monitor complex coastal waters

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HES-CW Products and ApplicationsHES-CW Products and Applications

Products: • Spectral water leaving radiances• Chlorophyll• Chlorophyll fluorescence• Turbidity• Spectral absorption and scattering

Applications: • Water quality monitoring• Coastal hazard assessment• Navigation safety• Human and ecosystem health awareness (Harmful Algal Blooms)• Natural resource management in coastal and estuarine areas• Climate variability prediction (e.g., role of the coastal ocean in the

carbon cycle)• Nowcast and Forecast models of the coastal ocean

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Chlorophyll and chlorophyll fluorescence of optically-complex coastal waters

Chlorophyll and chlorophyll fluorescence of optically-complex coastal waters

MODIS Terra scene from 3 October 2001.

• The ratio of Fluorescence Line

Height (FLH) to chlorophyll is a good indicator of the health of the

phytoplankton population.

• FLH separates chlorophyll from

suspended sediments in the

Columbia River Plume.

Fluorescence line height not available from VIIRS.

MODIS Terra scene from 3 October 2001.

• The ratio of Fluorescence Line

Height (FLH) to chlorophyll is a good indicator of the health of the

phytoplankton population.

• FLH separates chlorophyll from

suspended sediments in the

Columbia River Plume.

Fluorescence line height not available from VIIRS.

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Monterey Bay Harmful Algal BloomMonterey Bay Harmful Algal Bloom

Harmful Algal Bloom in Monterey Bay threatens

beach areas.

• Bloom near coast and on the order of 2 x 5 km would not be

resolved in 1 km VIIRS data.

• Additional channels on HES-CW aid bloom identification.

Harmful Algal Bloom in Monterey Bay threatens

beach areas.

• Bloom near coast and on the order of 2 x 5 km would not be

resolved in 1 km VIIRS data.

• Additional channels on HES-CW aid bloom identification.

PHILLS-2 airborne hyperspectral data from

Paul Bissett, Florida Environmental Research Institute. (October 2002 Ceratium spp. bloom)

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HES-Will support the higher temporal and spatial resolution required for coastal models

HES-Will support the higher temporal and spatial resolution required for coastal models

July 31 SeaWiFS Chlor-a (mg/m3)

.5

2

3

4

5

39:30N

39:00N

Node A

UCSB

Small diatoms

Large diatoms

Satellite Measured

ECOSIM run for July 31, 2001 with ROMS Physical model 15 minute time step and

300 m spatial resolution(Paul Bissett, Florida Environmental Research

Institute)

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COAST and Risk Reduction ActivitiesCOAST and Risk Reduction Activities

• The Coastal Ocean Applications and Science Team (COAST) was created in August 2004 to support NOAA to develop coastal ocean applications for HES-CW:– Mark Abbott, Dean of the College of Oceanic and Atmospheric Sciences

(COAS) at Oregon State University is the COAST team leader,– COAST activities are managed through the Cooperative Institute for

Oceanographic Satellite Studies (CIOSS) a part of COAS, Ted Strub, Director

– Curtiss Davis, Senior Research Professor at COAS, is the Executive Director of COAST.

• Initial activity to evaluate HES-CW requirements and suggest improvements• Paul Menzel Presented GOES-R Risk Reduction Program at the first COAST

meeting in September 2004 and invited COAST to participate.– Curt Davis and Mark Abbott presented proposed activities in Feb. 2005. – CIOSS/COAST invited to become part of GOES-R Risk Reduction Activity

beginning in FY 2006.– Proposal Submitted to NOAA Sept 6, 2005.– Activities to begin in May, 2006.

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Risk Reduction Activities:Principal Roles of Co-Investigators

Risk Reduction Activities:Principal Roles of Co-Investigators

• Curtiss Davis, program management, calibration, atmospheric correction• Mark Abbott, COAST Team Leader• Ricardo Letelier, phytoplankton productivity and chlorophyll fluorescence,

data management • Peter Strutton, coastal carbon cycle, Harmful Algal Blooms (HABs)• Ted Strub, CIOSS Director, coastal dynamics, links to IOOSCOAST Participants:• Bob Arnone, NRL, optical products, calibration, atmospheric correction,

data management• Paul Bissett, FERI, optical products, data management• Heidi Dierssen, U. Conn., benthic productivity• Raphael Kudela, UCSC, HABs, IOOS• Steve Lohrenz, USM, suspended sediments, HABs• Oscar Schofield, Rutgers U., product validation, IOOS, coastal models• Heidi Sosik, WHOI, productivity and optics• Ken Voss, U. Miami, calibration, atmospheric correction, opticsNOAA/STAR • Menghua Wang, atmospheric correction• Mike Ondrusek, calibration, MOBY

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HES-CW Data flow and Risk Reduction Activities

HES-CW Data flow and Risk Reduction Activities

Raw sensor data

Calibrated radiances

at the sensor

Water Leaving

Radiances

In-Water Optical

Properties

Applications and products

Users

CalibrationCalibration Atmospheric Correction

Atmospheric Correction

Optical properties Algorithms

Optical properties Algorithms

Product models and algorithms

Product models and algorithms

now-cast and forecast models Data

assimilation into models

Data assimilation into models

Education and outreach

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Approach to Algorithm DevelopmentApproach to Algorithm Development

• Directly involve the ocean color community which has extensive algorithm development experience with SeaWiFS and MODIS– NASA funded science teams developed, tested and validated calibration,

atmospheric correction and product algorithms– Additional product development and testing funded by U. S. Navy– Documented in Technical reports, publications and Algorithm

Theoretical Basis Documents (ATBDs)– Algorithms are continuously evaluated and updated; SeaWiFS and

MODIS data routinely reprocessed to provide Climate Data Records with latest algorithms.

• Design program to assure compatibility of HES-CW products with VIIRS– VIIRS algorithms based on MODIS ATBDs– Similar calibration and atmospheric correction approaches– Use the same ocean calibration sites for vicarious calibration

• Initial plans and algorithms based on SeaWiFS and MODIS experience modified to fit HES-CW in geostationary orbit.

• Advanced algorithms tested and implemented when available.• Early tests planned using airborne hyperspectral data.

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Proposed Experiments to Collect Simulated HES-CW data

Proposed Experiments to Collect Simulated HES-CW data

• There are no existing data sets that include all the key attributes of HES-CW data:– Spectral coverage (.4 – 1.0 m)– High signal-to-noise ratio (>300:1 prefer 900:1, for ocean radiances)– High spatial resolution (<150 m, bin to 300 m) – Hourly or better revisit

• Propose field experiments in FY2006-2008 to develop the required data sets for HES-CW algorithm and model development.

• Airborne system:– Hyperspectral imager that can be binned to the HES-CW bands– Flown at high altitude for 20 km x 20 km scenes every 30 min– Endurance to collect repeat flight lines every half hour for up to 6 hours– Spectroscopy Aerial Mapping System with On-Board Navigation

(SAMSON) Hyperspectral Imager (Florida Environmental Research Inst.)• Propose three experimental sites:– 2006 Monterey Bay (September 3-16, 2006, coastal upwelling, HABs)– 2007 New York/Mid Atlantic Bight (August, river input, urban aerosols)– 2008 Mississippi River Plume (Sediment input, HABs)

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SummarySummary

• HES-CW will provide an excellent new tool for the characterization and management of the coastal ocean.

• Risk Reduction activities focus on calibration and algorithm development;– Initially provide SeaWiFS and MODIS heritage calibration and algorithms;– 2006-2008 field experiments to develop example HES-CW data for

- algorithm development and testing,- Coordination with IOOS for in-situ data and coastal ocean models,- Demonstrate terabyte web-based data system.

– Major focus on developing advanced algorithms that take advantage of HES-CW unique characteristics.

• Efforts coordinated with NOAA ORA, NMFS and NOS with a focus on meeting their operational needs.

Special thanks to Ted Strub, Amy Vandehey and the COAST for their hard work getting this program started.

Thanks to NOAA for funding and particularly to Stan Wilson, John Pereira, Eric Bayler and Paul Menzel for their support and guidance.

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BACKUPBACKUP

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COAST proposed new HES-CW Channel Specifications


Nominal Threshold

Channel Center

Nominal Threshold Resolution

Nominal Threshold

Signal to Noise

Nominal GOAL Channel Center

Wavelength (um)

Nominal GOAL

Resolution

Nominal Goal Signal to Noise

0.412 0.02 0.345 0.02

0.443 0.02 0.38 0.020.49 0.02 0.407 through 0.987 0.010.51 0.02 0.57 0.010.53 0.02 0.72 0.020.55 0.02 1.24 0.040.58 0.02 1.38 0.03

0.61 0.02 1.61 0.06

0.645 0.01 2.26 0.05

0.667 0.01 11.2 (2 km) 0.8

0.678 0.01 12.3 (2 km) 1

0.709 0.02

Nominal Threshold

Horiz. Resolution

Nominal Goal Horiz.

Resolution

0.75

COAST Proposed HES-CW Channel Specifications

375-meters (at Equator)


except for LW IR channels.865 0.02

300 to 1 all channels


0.02

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Nominal Threshold

Channel Center

Nominal Threshold Resolution

Nominal Threshold

Signal to Noise

Nominal GOAL Channel Center

Wavelength (um)

Nominal GOAL

Resolution

Nominal Goal Signal to Noise

0.412 0.02 0.345 0.02

0.443 0.02 0.38 0.020.49 0.02 0.407 through 0.987 0.010.51 0.02 0.57 0.010.53 0.02 0.72 0.020.55 0.02 1.24 0.040.58 0.02 1.38 0.03

0.61 0.02 1.61 0.06

0.645 0.01 2.26 0.05

0.667 0.01 11.2 (2 km) 0.8

0.678 0.01 12.3 (2 km) 1

0.75 0.02

Nominal Threshold

Horiz. Resolution

Nominal Goal Horiz.

Resolution

0.865

COAST Proposed HES-CW Channel Specifications



except for LW IR channels

1.000 (0.72 backup)

0.04 (0.02)



0.02

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Frequency of Sampling and Prioritizing Goal Requirements

Frequency of Sampling and Prioritizing Goal Requirements

• COAST top priority goals are:– Higher frequency of sampling– Goal channels for atmospheric correction– Hyperspectral instead of multispectral

• Threshold requirement is to sample all Hawaii and Continental U. S. coastal waters once every three hours during daylight– Plus additional hourly sampling of

selected areas• Goal requirement is hourly sampling of all

U.S. coastal waters is strongly recommended, for cloud clearing and to better resolve coastal ocean dynamics.

• Goal requirements compete with each other, e.g. higher spatial resolution makes it harder to increase sampling frequency or SNR.

• Threshold requirement is to sample all Hawaii and Continental U. S. coastal waters once every three hours during daylight– Plus additional hourly sampling of

selected areas• Goal requirement is hourly sampling of all

U.S. coastal waters is strongly recommended, for cloud clearing and to better resolve coastal ocean dynamics.

• Goal requirements compete with each other, e.g. higher spatial resolution makes it harder to increase sampling frequency or SNR.

HES-CW built to the threshold requirements will be a dramatic improvement over present capabilities for coastal imaging.

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Risk Reduction ActivitiesRisk Reduction Activities

• Approach to Algorithm Development– Experience with SeaWiFS and MODIS– Field Experiments to collect prototype HES-CW data

• Planned Risk Reduction activities:– Calibration and vicarious calibration– Atmospheric correction– Optical properties– Phytoplankton chlorophyll, chlorophyll fluorescence and productivity– Benthic productivity– Coastal carbon budget– Harmful algal blooms– Data access and visualization– Education and public outreach

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Proposed Experiments to collect simulated HES-CW data (2 of 2)

Proposed Experiments to collect simulated HES-CW data (2 of 2)

• Experimental Design– Choose sites with IOOS or other long term monitoring and modeling

activities– Intensive effort for 2 weeks to assure that all essential parameters are

measured:- Supplement standard measurements at the site with shipboard or

mooring measurements of water-leaving radiance, optical properties and products expected from HES-CW algorithms,- Additional atmospheric measurements as needed to validate

atmospheric correction parameters,- As needed, enhance modeling efforts to include bio-optical models

that will utilize HES-CW data.– Aircraft overflights for at least four clear days and one partially cloudy

day (to evaluate cloud clearing) during the two week period. - High altitude to include 90% or more of the atmosphere- 30 min repeat flight lines for up to 6 hours to provide a time series for

models and to evaluate changes with time of day (illumination, phytoplankton physiology, etc.)

• All data to be processed and then distributed over the Web for all users to test and evaluate algorithms and models.