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Type of solar resource parameter Type of solar resource parameter for specific applications, e.g. for specific applications, e.g. Sky luminance Sky luminance Tilted Irradiance Tilted Irradiance Direct Irradiance Direct Irradiance Perez et al., ASRC

Type of solar resource parameter for specific … · france – entpe-lyon / ecole des mines norway – u. bergen japan – u. kyoto n. zealand – industrial research canada –

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Type of solar resource parameterType of solar resource parameterfor specific applications, e.g.for specific applications, e.g.

Sky luminanceSky luminanceTilted IrradianceTilted Irradiance

Direct IrradianceDirect Irradiance

Perez et al., ASRC

Perez et al., ASRC

In situ In situ MeasurementMeasurement

customizedcustomized parametersparameters

Per

ez e

t al.,

ASR

C

In situ In situ MeasurementMeasurement

ModelsModels

ModelModel

Direct & DiffuseDirect & DiffuseIrradiancesIrradiances

GlobalGlobalIrradianceIrradiance

Primary irradiance NetworksPrimary irradiance Networks

customizedcustomized parametersparameters

Per

ez e

t al.,

ASR

C

In situ In situ MeasurementMeasurement

ModelsModels

ModelModel

Direct & DiffuseDirect & DiffuseIrradiancesIrradiances

GlobalGlobalIrradianceIrradiance

Primary irradiance NetworksPrimary irradiance Networks

customizedcustomized parametersparameters

Satellite Remote Satellite Remote SensingSensing

ModelsModels

Geostationary Weather Satellites- High resolution

(decaying at high latitudes)- Continuous in time

Polar Orbiters- Very High resolution

at all latitudes- Twice a day only

0

100

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0 200 400 600 800 1000

satellite-derived global irradiance (W/sq.m)

measured global irradiance (W/sq.m)

Perez et al., ASRC

Sat

ellit

e-de

rived

glo

bal i

rrad

ianc

e

Measured global irradiance

Short term Effective AccuracyShort term Effective Accuracy

time/site specific datatime/site specific data

Perez et al., ASRC

0%

5%

10%

15%

20%

25%

30%

35%

40%

45%

50%

0 50 100 150 200 250 300

Northeastern US

Switzerland

satellite confidence level -- simple model(accounting for time mismatch and solar geometry)

Relative RMSE (%)

Distance from station (km)

Nugget Effect

0

100

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0 200 400 600 800 1000

satellite-derived global irradiance (W/sq.m)

measured global irradiance (W/sq.m)

0

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0 200 400 600 800 1000

satellite-derived global irradiance (W/sq.m)

measured global irradiance (W/sq.m)

0

100

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0 200 400 600 800 1000

measured global irradiance --site No.1 (W/sq.m)

measured global irradiance --- site No.2 (W/sq.m)

0

100

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0 200 400 600 800 1000

measured global irradiance --site No.1 (W/sq.m)

measured global irradiance --- site No.2 (W/sq.m)

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0 200 400 600 800 1000

satellite-derived global irradiance (W/sq.m)

measured global irradiance (W/sq.m)

0

100

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0 200 400 600 800 1000

satellite-derived global irradiance (W/sq.m)

measured global irradiance (W/sq.m)0

100

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0 200 400 600 800 1000

satellite-derived global irradiance (W/sq.m)

measured global irradiance (W/sq.m)

0

100

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400

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1000

0 200 400 600 800 1000

satellite-derived global irradiance (W/sq.m)

measured global irradiance (W/sq.m)

0

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600

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800

900

1000

0 200 400 600 800 1000

satellite-derived global irradiance (W/sq.m)

measured global irradiance (W/sq.m)

0

100

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300

400

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600

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900

1000

0 200 400 600 800 1000

measured global irradiance --site No.1 (W/sq.m)

measured global irradiance --- site No.2 (W/sq.m)

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0 200 400 600 800 1000

measured global irradiance --site No.1 (W/sq.m)

measured global irradiance --- site No.2 (W/sq.m)0

100

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0 200 400 600 800 1000

measured global irradiance --site No.1 (W/sq.m)

measured global irradiance --- site No.2 (W/sq.m)

0

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0 200 400 600 800 1000

measured global irradiance --site No.1 (W/sq.m)

measured global irradiance --- site No.2 (W/sq.m)

0

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500

600

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0 200 400 600 800 1000

measured global irradiance --site No.1 (W/sq.m)

measured global irradiance --- site No.2 (W/sq.m)

7000

Wh/sq.m/day

5000

Summer Global Irradiance

A: SatelliteB: NSRDB

Perez, Seals, Zelenka & Renné

GOES-8GOES-10

overlap

Perez et al.

Albuquerque (SNLA)

Burlington (ARM)

Albany (SUNY)

Cocoa (FSEC)

Kramer Junction (SEGS)

Gladstone (U-Oregon)Hermiston (U-Oregon)

Eugene (U-Oregon)Burns (U-Oregon)

Klamath Falls (U-Oregon)

DIRECT IRRADIANCE (average W/sq.m)GLOBAL IRRADIANCE (average W/sq.m)100

120

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190

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• Time/site specific PV output data

• Coincident electric load data

Per

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t al.,

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Richard Perez et al., ASRC

15

source: RReDC

lowest highest

ENERGYENERGY

CAPACITYCAPACITY

Perez et al., 2002

“ Improved solar resource information would greatly assist the solarindustry as customers require increasing specificity and accuracyregarding the savings solar can deliver for their applications. Inparticular, higher spatial resolution, and time specific information,would deliver the highest value. Ideally, NREL would employ emergingsatellite technology to make a database available via the internet. Amap (initially US, later Europe, Asia, etc) that the user could selectareas from, and specific periods from which to evaluate insolation, isneeded. This solar information could then easily plug into a variety ofavailable performance simulation products such as PVWatts.

From our standpoint this is clearly the next step for resourceassessment. The technology is available, it would be a terrific benefit

to the industry to make it happen ”

Dan Shugar, PowerLight

INTERNATIONAL COLLABORATION / EXCHANGE

INDER THE AUSPICES OF IEA

Global satellite coverageHigh resolution informationTime specific information [past, current, future]

Insuring coherence between models and satellite-platformsValidation of satellite-derived productsFacilitating access/exchange of data

IEA – Potential partners

US – NREL / SUNY / NASAGERMANY – DLR/ISE/U.OLDENBURGSWITZERLAND – METEOSUISSE / U.GENEVAFRANCE – ENTPE-LYON / ECOLE DES MINESNORWAY – U. BERGENJAPAN – U. KYOTON. ZEALAND – INDUSTRIAL RESEARCHCANADA – U.CHICOUTIMI

Associated teams

BRAZIL -- IMPEINDIA – TERI….