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Immediate report of Victoria University of Wellington Antarctic Expedition 1989-90: VUWAE 34

Figure 2 Time evolution of the transmission of the ice (a) at the UV wavelengths 250 nm (●), 280 nm (∆), 300 nm (O), 350 nm (▲), and 400 nm (□), and (b) at visible wavelengths of 500 nm (O), 600 nm (□), and 700 nm (∆)

Figure 2 Time evolution of the transmission of the ice (a) at the UV wavelengths 250 nm (●), 280 nm (∆), 300 nm (O), 350 nm (▲), and 400 nm (□), and (b) at visible wavelengths of 500 nm (O), 600 nm (□), and 700 nm (∆).

Figure 2 Time evolution of the transmission of the ice (a) at the UV wavelengths 250 nm (●), 280 nm (∆), 300 nm (O), 350 nm (▲), and 400 nm (□), and (b) at visible wavelengths of 500 nm (O), 600 nm (□), and 700 nm (∆).