TY - JOUR KW - Heat Island KW - Solar reflectance KW - Methods & Protocols KW - Pyranometer KW - Solar heat gain KW - Solar spectrophotometer KW - Solar Spectrum Reflectometer KW - Spectrally selective AU - Ronnen M Levinson AU - Hashem Akbari AU - Paul H Berdahl AB -
Solar reflectance can vary with the spectral and angular distributions of incident sunlight, which in turn depend on surface orientation, solar position and atmospheric conditions. A widely used solar reflectance metric based on the ASTM Standard E891 beam-normal solar spectral irradiance underestimates the solar heat gain of a spectrally selective “cool colored” surface because this irradiance contains a greater fraction of near-infrared light than typically found in ordinary (unconcentrated) global sunlight. At mainland US latitudes, this metric RE891BN can underestimate the annual peak solar heat gain of a typical roof or pavement (slope ⩽ 5:12 [23°]) by as much as 89 W m−2, and underestimate its peak surface temperature by up to 5 K. Using RE891BN to characterize roofs in a building energy simulation can exaggerate the economic value N of annual cool roof net energy savings by as much as 23%.
We define clear sky air mass one global horizontal (“AM1GH”) solar reflectance Rg,0, a simple and easily measured property that more accurately predicts solar heat gain. Rg,0 predicts the annual peak solar heat gain of a roof or pavement to within 2 W m−2, and overestimates N by no more than 3%. Rg,0 is well suited to rating the solar reflectances of roofs, pavements and walls. We show in Part II that Rg,0 can be easily and accurately measured with a pyranometer, a solar spectrophotometer or version 6 of the Solar Spectrum Reflectometer.
BT - Solar Energy DA - 09/2010 DO - 10.1016/j.solener.2010.04.018 IS - 9 LA - eng N2 -Solar reflectance can vary with the spectral and angular distributions of incident sunlight, which in turn depend on surface orientation, solar position and atmospheric conditions. A widely used solar reflectance metric based on the ASTM Standard E891 beam-normal solar spectral irradiance underestimates the solar heat gain of a spectrally selective “cool colored” surface because this irradiance contains a greater fraction of near-infrared light than typically found in ordinary (unconcentrated) global sunlight. At mainland US latitudes, this metric RE891BN can underestimate the annual peak solar heat gain of a typical roof or pavement (slope ⩽ 5:12 [23°]) by as much as 89 W m−2, and underestimate its peak surface temperature by up to 5 K. Using RE891BN to characterize roofs in a building energy simulation can exaggerate the economic value N of annual cool roof net energy savings by as much as 23%.
We define clear sky air mass one global horizontal (“AM1GH”) solar reflectance Rg,0, a simple and easily measured property that more accurately predicts solar heat gain. Rg,0 predicts the annual peak solar heat gain of a roof or pavement to within 2 W m−2, and overestimates N by no more than 3%. Rg,0 is well suited to rating the solar reflectances of roofs, pavements and walls. We show in Part II that Rg,0 can be easily and accurately measured with a pyranometer, a solar spectrophotometer or version 6 of the Solar Spectrum Reflectometer.
PY - 2010 SP - 1717 EP - 1744 T2 - Solar Energy TI - Measuring solar reflectance—Part I: Defining a metric that accurately predicts solar heat gain VL - 84 ER -