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  1. The MCD43C3 Climate Modeling Grid (CMG) Albedo Product (MODIS/Terra Albedo Daily L3 Global 0.05 deg CMG) provides both the white-sky albedos and the black-sky albedos (at local solar noon) for MODIS bands 1-7 as well as for three broad bands (0.3-0.7 µm, 0.7-5.0 µm, and 0.3-5.0 µm) at a 0.05 degree spatial resolution in global files in a geographic (lat/long) projection.

  2. Albedo One. Entry updated 19 February 2024. Tagged: Publication. Irish low-paying magazine of sf, fantasy and horror fiction which appears irregularly; formerly two or three times per year, latterly once or twice; there was a three-year gap between issue #47 in 2016 and #48 in 2019. First issue, Summer 1993, but undated from issue #4.

  3. link.springer.com › 10 › 978/3/662-65093-6_43Albedo | SpringerLink

    Jan 1, 2023 · The geometric albedo is defined as the ratio of a planet’s reflectivity measured at zero phase angle (opposition) to that of a Lambert disk (which has the same apparent brightness at all viewing angles) of the same radius. The geometric albedo is a function of wavelength and, because it is measured at opposition (when the phase angle ϕ = 0 ...

  4. Jan 1, 2024 · These maps show albedo on a scale from 0 (no incoming sunlight being reflected) to 0.9 (nearly all incoming light being reflected). Darker blue colors indicate that the surface is not reflecting much light, while paler blues indicate higher proportions of incoming light are being reflected.

  5. Checklist of Albedo One. Albedo One. 1993 #1 Summer #2 Autumn #3 Winter: 1994 #4 Spring #5 Summer

  6. Nov 28, 2013 · Albedo One – Guidelines to Artists. Please submit a sample of your work. We currently require cover artwork only. Artwork may be commissioned on the basis of your initial sample submission. We pay €20 for artwork, on publication. Our address: Albedo One. 2 Post Road. Lusk.

  7. link.springer.com › 10 › 978/3/642-11274-4_43Albedo | SpringerLink

    The geometric albedo is a function of wavelength and, because it is measured at opposition (when the phase angle ϕ = 0), does not require information on the dependence of scattering with phase to measure. For a perfectly reflecting Lambert sphere the geometric albedo is 2/3 and for a semi-infinite purely Raman scattering atmosphere it is 3/4.

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