Journal cover Journal topic
Ocean Science An interactive open-access journal of the European Geosciences Union
Ocean Sci., 8, 455-471, 2012
http://www.ocean-sci.net/8/455/2012/
doi:10.5194/os-8-455-2012
© Author(s) 2012. This work is distributed
under the Creative Commons Attribution 3.0 License.
Research article
10 Jul 2012
On the influence of wind and waves on underwater irradiance fluctuations
M. Hieronymi1,2,3 and A. Macke1 1Leibniz Institute for Tropospheric Research (IFT), Leipzig, Germany
2Helmholtz Centre for Ocean Research (GEOMAR), Kiel, Germany
3Institute of Coastal Research, Helmholtz Centre Geesthacht (HZG), Germany
Abstract. The influence of various wind and wave conditions on the variability of downwelling irradiance Ed (490 nm) in water is subject of this study. The work is based on a two-dimensional Monte Carlo radiative transfer model with high spatial resolution. The model assumes conditions that are ideal for wave focusing, thus simulation results reveal the upper limit for light fluctuations. Local wind primarily determines the steepness of capillary-gravity waves which in turn dominate the irradiance variability near the surface. Down to 3 m depth, maximum irradiance peaks that exceed the mean irradiance Ed by a factor of more than 7 can be observed at low wind speeds up to 5 m s−1. The strength of irradiance fluctuations can be even amplified under the influence of higher ultra-gravity waves; thereby peaks can exceed 11 Ed. Sea states influence the light field much deeper; gravity waves can cause considerable irradiance variability even at 100 m depth. The simulation results show that under realistic conditions 50% radiative enhancements compared to the mean can still occur at 30 m depth. At greater depths, the underwater light variability depends on the wave steepness of the characteristic wave of a sea state; steeper waves cause stronger light fluctuations.

Citation: Hieronymi, M. and Macke, A.: On the influence of wind and waves on underwater irradiance fluctuations, Ocean Sci., 8, 455-471, doi:10.5194/os-8-455-2012, 2012.
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