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Calculations of street level spectral irradiances using the Google Street View photographic database: Implementation and potential applications on ultraviolet light studies Roberto Carrasco-Hernandez, Andrew R.D. Smedley & Ann R. Webb University of Manchester, School of Earth, Atmospheric and Environmental Sciences & Williamson Research Centre for Molecular Environmental Science, University of Manchester, UK.

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  • Calculations of street level spectral irradiances using the Google Street View

    photographic database: Implementation and potential applications on ultraviolet light studies

    Roberto Carrasco-Hernandez, Andrew R.D. Smedley &

    Ann R. Webb University of Manchester, School of Earth, Atmospheric and Environmental Sciences & Williamson Research Centre for Molecular Environmental Science, University of Manchester, UK.

  • The Problem

    UV & Spectral measurements

    are taken up here

    People are exposed to

    UV light down here

    Photograph: Google Street View.com

  • Layout

    • Important: Easy Access Modelling Tools

    • Image processing approach to reconstruct urban canyon geometries from Google.

    • Considerations needed for Canyon Irradiance Models (Total shortwave and spectral irradiances).

    • Current state of development and future scope of the project.

  • Image Digital Processing Software tools:

    Google Street View + Hugin

    Snapshots of the Hugin interface: A.-Independent photographs covering the

    full upper hemispheric view. B.-The reconstructed hemispheric view

    using a fisheye projection.

    Set of photographs linked to one single position in the city of Manchester, taken from Street View.

  • Image Digital Processing Software tools:

    Google Street View + Hugin

    Snapshots of the Hugin interface: A.-Independent photographs covering the

    full upper hemispheric view. B.-The reconstructed hemispheric view

    using a fisheye projection.

    SVF = 0.503

    SVF = 0.325

    SVF = 0.550

    A.- Orthographic reconstructed projection; B.- Equidistant reconstructed projection;

    C.- Control fisheye photograph, taken with an adaptable phone mini fisheye lens.

    Pictures were taken at the Zochonis Canyon, University of Manchester.

    SVF: Sky View Factor for each image.

  • Total Shortwave Irradiance Calculations: Rayman Software (Matzarakis et al. 2010)

    Diagrammatic output results from Rayman.

    The software can calculate Sky View Factor (SVF), Global, Direct and Diffuse

    Irradiances.------We tested it

  • Assumptions and Limitations of the Rayman Model.

    • NO Spectral Irradiances

    • “Black” Obstructions

    • Isotropic Diffuse Irradiance

    (NO Circumsolar Irradiance)

  • Assumptions and Limitations of the Rayman Model.

    • NO Spectral Irradiances

    • “Black” Obstructions

    • Isotropic Diffuse Irradiance

    (NO Circumsolar Irradiance)

    This anisotropic distribution is not considered by these models

  • First approach to calculate Spectral Irradiances in Urban Canyons

    • Assumption 1: Canyon Spectral Irradiance -at any wavelength- is a fraction of Rooftop Spectral Irradiance, at the same wavelength. And it is a function of the SVF.

    • Assumption 2: The ratio of Diffuse/Global irradiance is explained by Rayleigh scattering, and is dependent on wavelength, Ozone, turbidity and SZA.

    • Assumption 3: Diffuse light is isotropic.

    UV

    People

    0.00E+00

    2.00E-01

    4.00E-01

    6.00E-01

    8.00E-01

    1.00E+00

    280.0 380.0 480.0 580.0 680.0 780.0

    10 Deg SZA

    20 Deg SZA

    30 Deg SZA

    40 Deg SZA

  • Model:

    𝐺𝑢,𝛌 = 𝐺𝑓,𝛌 ∗ 1 − 𝐷𝑖𝑓𝑓𝑢𝑠𝑒/𝐺𝑙𝑜𝑏𝑎𝑙𝛌 ∗ 𝑆𝑏𝑖𝑛 + 𝐺𝑓,𝛌 ∗ 𝐷𝑖𝑓𝑓𝑢𝑠𝑒/𝐺𝑙𝑜𝑏𝑎𝑙𝛌 ∗ 𝑠𝑣𝑓𝑢

    • 𝐺𝑢,𝛌 : Global “Canyon” Irradiance in canyon"𝑢", canyon and at wavelength"𝛌”

    • 𝐺𝑓,𝛌: Global “Rooftop” Irradiance -also “full viewirradiance”- at wavelength"𝛌”

    • 𝐷𝑖𝑓𝑓𝑢𝑠𝑒/𝐺𝑙𝑜𝑏𝑎𝑙𝛌 : Ratio of diffuseto global irradiances at wavelength"𝛌”, accordingto the

    equation: 𝐷𝑖𝑓𝑓𝑢𝑠𝑒

    𝐺𝑙𝑜𝑏𝑎𝑙=

    𝑙𝑜𝑔305𝑛𝑚 1+𝐴𝑂𝐷+ 305𝑛𝑚

    (305𝑛𝑚−𝝀)

    𝑆𝑍𝐴100 +0.9

    1+𝑙𝑜𝑔305𝑛𝑚 1+ 305𝑛𝑚

    (305𝑛𝑚−𝝀)𝟐

    • 𝑠𝑣𝑓𝑢: Sky View Factor at canyon"𝑢"

    First approach to calculate Spectral Irradiances in Urban Canyons

  • Model Validations

    • Simulated Canyons

    SI1 SVF = 0.545

    Full SVF = 0.545

    SI2 SVF = 0.415

    SI3 SVF = 0.42

    Diode Array Spectroradiometer

  • 0

    0.2

    0.4

    0.6

    0.8

    1

    320 420 520 620 720

    Obstructed/Full Ratio

    Wavelength

    Measured Obstructed/Full Ratios for simulated canyons

    si1/full

    si2/full

    si3/full

    • Results: Ratios of obstructed global spectral irradiance to full sky view.

  • 0.8

    0.85

    0.9

    0.95

    1

    320 420 520 620 720

    Comparison Modelled vs. Measured Ratios -Second Simulated Canyon (SI2)-

    si2/full

    calc si2/full

    0.8

    0.85

    0.9

    0.95

    1

    320 420 520 620 720

    Comparison Modelled vs. Measured Ratios -First Simulated Canyon (SI1)-

    si1/full

    calc si1/full

    Comparisons Modelled vs. Measured Ratios

    SI1 SVF = 0.545

    SI2 SVF = 0.415

    5% difference

  • • Results: Comparisons Modelled vs. Measured Ratios

    0.8

    0.85

    0.9

    0.95

    1

    320 420 520 620 720

    si1/full

    si2/full

    Measurements

    0.8

    0.85

    0.9

    0.95

    1

    320 420 520 620 720

    calc si1/full

    calc si2/full

    Models

    SI1 SVF = 0.545

    SI2 SVF = 0.415

  • • Results: Comparisons Modelled vs. Measured Ratios

    0

    0.2

    0.4

    0.6

    320 370 420 470 520 570 620 670 720

    Comparison Modelled vs. Measured Ratios -Third Simulated Canyon (SI3)-

    si3/full

    calc si3/full

    It is necessary to consider the anisotropic distribution of diffuse light, as well as the potential effect of reflective surfaces in the canyons.

  • Conclusions • The reconstruction and “fisheye” projection of urban geometries is

    possible from Google Street View. This has the potential to become a useful tool in solar radiation studies at street level.

    • The Rayman software allows the calculation of total-shortwave irradiances in urban canyons from the reconstructed “fisheye” images, but there is a need for spectral irradiance models.

    • The spectral model proposed here represented an acceptable approximation, however, -in order to improve the performance of the models at canyons with different orientations- methods that account for diffuse light anisotropy and reflectivity of horizon obstructions are yet to be developed.