Biblioteca Digital

176 resultados para 379.1

Fraction of spectral solar radiance transmitted through snow and sea ice as measured in different depths under sea ice (transflectance) at sea ice station PS78/218-1

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Total Sky Imager observations during POLARSTERN curise ANT-XXVIII/1 on 2011-10-30 with links to images

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Horizontal profiles of downward irradiance at 350 to 819 nm at Barrow, Alaska, observations on day 1, 2011-06-05

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Pore-water chemistry of sediment core GeoB13113-1

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Downward spectral solar radiance as measured in different depths under sea ice (transmitted radiance) at sea ice station PS80/323-1

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Downward spectral solar radiance as measured in different depths under sea ice (transmitted radiance) at sea ice station PS80/335-1

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Fraction of spectral solar radiance transmitted through snow and sea ice as measured in different depths under sea ice (transflectance) at sea ice station PS80/323-1

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Fraction of spectral solar irradiance transmitted through snow and sea ice as measured in different depths under sea ice (transmittance) at sea ice station PS80/323-1

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Fraction of spectral solar irradiance transmitted through snow and sea ice as measured in different depths under sea ice (transmittance) at sea ice station PS80/335-1

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Downward spectral solar radiance as measured in different depths under sea ice (transmitted radiance) at sea ice station PS80/384-1

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Fraction of spectral solar irradiance transmitted through snow and sea ice as measured in different depths under sea ice (transmittance) at sea ice station PS80/360-1

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Downward spectral solar irradiance as measured in different depths under sea ice (transmitted irradiance) at sea ice station PS80/349-1

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Downward spectral solar irradiance as measured in different depths under sea ice (transmitted irradiance) at sea ice station PS80/360-1

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Downward spectral solar radiance as measured in different depths under sea ice (transmitted radiance) at sea ice station PS80/360-1

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Incident spectral solar irradiance measured above sea ice at sea ice station PS80/349-1

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