Abstract
According to W. Levingston a change of the solar energy distribution (with total flux conserved) could have an impact on climate through changes of the ocean albedo or absorption. His idea is based on the water absorption curve given by Smith and Baker (1978), showing a sharp increase in absorption at wavelength longer than 500nm. In the following we comment on this hypothesis.
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© 1994 Springer-Verlag Berlin Heidelberg
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Braconnot, P. (1994). Comment on the Ocean Albedo and Absorption. In: Nesme-Ribes, E. (eds) The Solar Engine and Its Influence on Terrestrial Atmosphere and Climate. NATO ASI Series, vol 25. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-79257-1_33
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DOI: https://doi.org/10.1007/978-3-642-79257-1_33
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-79259-5
Online ISBN: 978-3-642-79257-1
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