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Comparison of UV climates at Summit, Greenland; Barrow, Alaska and South Pole, Antarctica

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Academic year: 2021

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Fig. 1. Ratio of SUV-150B and GUV-511 measurements of spectral irradiance at 320, 340, and 380 nm for six periods using data with solar zenith angles smaller than 85 ◦
Fig. 2. Ratio of measured and modeled clear-sky spectra integrated over the wavelength range 342.5–347.5 nm
Fig. 3. Total ozone at Summit, South Pole and Barrow as a function of time of year (Panel (a)) and solar zenith angle (Panel (b))
Fig. 4. Measurements of irradiance at 345 nm in units of µW/cm 2 at South Pole, Summit, and Barrow
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