Requirement for atmospheric corrections Linear stretch images of TOA and Rayleigh/Ozone/Water Vapor...

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Requirement for atmospheric corrections Linear stretch images of TOA and Rayleigh/Ozone/Water Vapor Corrected reflectance by using the same reflectance maximum and minimum TOA reflectance Rayleigh/Ozone/Water Vapor Corrected reflectance

Transcript of Requirement for atmospheric corrections Linear stretch images of TOA and Rayleigh/Ozone/Water Vapor...

Page 1: Requirement for atmospheric corrections Linear stretch images of TOA and Rayleigh/Ozone/Water Vapor Corrected reflectance by using the same reflectance.

Requirement for atmospheric corrections

Requirement for atmospheric corrections

Linear stretch images of TOA and Rayleigh/Ozone/Water Vapor Corrected reflectance by using the same reflectance maximum and minimum

TOA reflectance Rayleigh/Ozone/Water VaporCorrected reflectance

Page 2: Requirement for atmospheric corrections Linear stretch images of TOA and Rayleigh/Ozone/Water Vapor Corrected reflectance by using the same reflectance.

Surface reflectance and Top of the atmosphere

Surface reflectance and Top of the atmosphere

Image from: http://www.profc.udec.cl/~gabriel/tutoriales/rsnote/cp9/cp9-2.htm

Page 3: Requirement for atmospheric corrections Linear stretch images of TOA and Rayleigh/Ozone/Water Vapor Corrected reflectance by using the same reflectance.

PEN EquipmentsPEN EquipmentsTKY

TGF

MSE

RHN

Mar. Apr. May Jun. Jul. Aug. Sep. Oct. Nov. Dec. Jan. Feb.

HSSR

http://www.pheno-eye.org

SP

ADFC

Page 4: Requirement for atmospheric corrections Linear stretch images of TOA and Rayleigh/Ozone/Water Vapor Corrected reflectance by using the same reflectance.

Validation (SP & MOD08)Validation (SP & MOD08)

0

0.4

0.8

1.2

1.6

2005 2006

Optical Depth Skyradiometer(400nm) MOD08(470nm)

0

0.4

0.8

1.2

1.6

2005 2006

Optical Depth Skyradiometer(400nm) MOD08(470nm)

0

0.4

0.8

1.2

1.6

2005 2006

Optical Depth Skyradiometer(500nm) MOD08(550nm)

0

0.4

0.8

1.2

1.6

2005 2006

Optical Depth Skyradiometer(500nm) MOD08(550nm)

0

0.4

0.8

1.2

1.6

2005 2006

Optical Depth Skyradiometer(675nm) MOD08(660nm)

0

0.4

0.8

1.2

1.6

2005 2006

Optical Depth Skyradiometer(675nm) MOD08(660nm)

0

0.5

1.0

1.5

2.0

2005 2006

Angstrom Exponent Skyradiometer(400-675nm) MOD08(470-660nm)

0

0.5

1.0

1.5

2.0

2005 2006

Angstrom Exponent Skyradiometer(400-675nm) MOD08(470-660nm)

Page 5: Requirement for atmospheric corrections Linear stretch images of TOA and Rayleigh/Ozone/Water Vapor Corrected reflectance by using the same reflectance.

Validation (SP & MOD04)Validation (SP & MOD04)

0

0.4

0.8

1.2

1.6

MO

D04(4

70nm

)

0 0.4 0.8 1.2 1.6Skyradiometer(400nm)

Optical Depth

TKY

0

0.4

0.8

1.2

1.6

MO

D04(4

70nm

)

0 0.4 0.8 1.2 1.6Skyradiometer(400nm)

Optical Depth

TKY

0

0.4

0.8

1.2

1.6

MO

D04(5

50nm

)

0 0.4 0.8 1.2 1.6Skyradiometer(500nm)

Optical Depth

TKY

0

0.4

0.8

1.2

1.6

MO

D04(5

50nm

)

0 0.4 0.8 1.2 1.6Skyradiometer(500nm)

Optical Depth

TKY

0

0.4

0.8

1.2

1.6

MO

D04(6

60nm

)

0 0.4 0.8 1.2 1.6Skyradiometer(675nm)

Optical Depth

TKY

0

0.4

0.8

1.2

1.6

MO

D04(6

60nm

)

0 0.4 0.8 1.2 1.6Skyradiometer(675nm)

Optical Depth

TKY

0

0.5

1.0

1.5

2.0

MO

D04(4

70-6

60nm

)

0 0.5 1.0 1.5 2.0Skyradiometer(400-675nm)

Angstrom Exponent

TKY

0

0.5

1.0

1.5

2.0

MO

D04(4

70-6

60nm

)

0 0.5 1.0 1.5 2.0Skyradiometer(400-675nm)

Angstrom Exponent

TKY

TGFTGF TGFTGF

TGFTGF TGFTGF

Page 6: Requirement for atmospheric corrections Linear stretch images of TOA and Rayleigh/Ozone/Water Vapor Corrected reflectance by using the same reflectance.

Previous System FrameworkPrevious System Framework

MODIS MOD08 Daily image

• Time consuming and need high level user experience.

• Lack of Robustness and scalable

• Not convenience for sharing among communities

On developing

PEN Observation System

PEN Observation System

SPSP

ADFCADFC

HSSRHSSR

PSSPSSPSSPSS

Site BSite BSite BSite B

Site CSite CSite CSite CSite DSite DSite DSite D

PMSPMSPMSPMSInput Web

Page

PEN DB & Backup

Page 7: Requirement for atmospheric corrections Linear stretch images of TOA and Rayleigh/Ozone/Water Vapor Corrected reflectance by using the same reflectance.

52NorthSOS52NorthSOS Mapserver Mapserver

OGC System Framework OGC System Framework

PEN Observation System

PEN Observation System

SPSP

ADFCADFC

HSSRHSSR

PSSPSSPSSPSS SOSSOSSOSSOS

MODIS MOD08 MODIS MOD08 Daily imageDaily image

WMS,WMS-TWMS,WMS-TWMS,WMS-TWMS,WMS-T

WPSWPSWPSWPS

GetFeatureInfo[MODIS value

from start to end]

JSONGetObservation[During MODIS

overpass time from start to end]

JSON

Overpass time Overpass time scenescene

PyWPS• Validation process• Least Square Fitting process

PyWPS• Validation process• Least Square Fitting process

ClientClientClientClient

Execute[station,start,end,product]

JSON

GetObservation ADFC

Page 8: Requirement for atmospheric corrections Linear stretch images of TOA and Rayleigh/Ozone/Water Vapor Corrected reflectance by using the same reflectance.

Satellite-Field Data Integrator (SFI)

Page 9: Requirement for atmospheric corrections Linear stretch images of TOA and Rayleigh/Ozone/Water Vapor Corrected reflectance by using the same reflectance.
Page 10: Requirement for atmospheric corrections Linear stretch images of TOA and Rayleigh/Ozone/Water Vapor Corrected reflectance by using the same reflectance.

ConclusionConclusion

• Comprehensive web-based GIS system framework enabled – Based on various open standards of OGC specifications– Using FOSS

• Mapserver, 52North SOS, PyWPS• OpenLayers, jQuery,

• Assimilation of sensor observation data and satellite image– Wider area, More accuracy, Reasonable cost

• Validation of aerosol properties from Satellite estimation with ground based sites– Improve the following product which relied on satellite image

“surface reflectance”

Page 11: Requirement for atmospheric corrections Linear stretch images of TOA and Rayleigh/Ozone/Water Vapor Corrected reflectance by using the same reflectance.

Future DevelopmentFuture Development

• Increase atmospheric observation network– Skynet

• Improving performance– Distributing ground site data source

• More than two million records for two station and four years

– WMS-T full supported with Mapserver– MOD03 overpass time to MOD08 Global dataset

• Possible to error 5 minutes observation

• Satellite image product validation– GLEON (Global Lake Ecological Observatory Network)

• Lake monitoring : SST, Chl. A : MODIS Ocean product

– CO Flux monitoring : Asiaflux / Japanflux

• Water Column Correction– CREON (Coral Reef Environmental Observatory Network)

• Validation with higher satellite image resolution– ASTER, FOMARSAT