Thesis (S.M.)--Joint Program in Oceanography/Applied Ocean Science and Engineering (Massachusetts Institute of Technology, Dept. of Mechanical Engineering; and the Woods Hole Oceanographic Institution), September 2011. / "September 2011." "©2011"--P. 2. Cataloged from PDF version of thesis. / Includes bibliographical references (p. 97-101). / The ocean depths provide an ever changing and complex imaging environment. As scientists and researches strive to document and study more remote and optically challenging areas, specifically scatter-limited environments. There is a requirement for new illumination systems that improve both image quality and increase imaging distance. One of the most constraining optical properties to underwater image quality are scattering caused by ocean chemistry and entrained organic material. By reducing the size of the scatter interaction volume, one can immediately improve both the focus (forward scatter limited) and contrast (backscatter limited) of underwater images. This thesis describes a relatively simple, cost-effective and field-deployable low-power dynamic lighting system that minimizes the scatter interaction volume with both subjective and quantifiable improvements in imaging performance. / by Geoffrey Allen Gorman. / S.M.

Although mass coral bleaching events are generally triggered by high seawater temperatures, experiments have demonstrated that corals and reef-dwelling foraminifers bleach more readily when exposed to high energy, short wavelength solar radiation (blue, violet and ultraviolet [UVR]: Lambda ~ 280 - 490 nm). In seawater, colored dissolved organic matter (CDOM), also called gelbstoff, preferentially absorbs these shorter wavelengths, which consequently bleach and degrade the CDOM. Alteration of watersheds and destruction of coastal wetlands have reduced natural sources of CDOM to reefal waters. I tested the null hypothesis that CDOM does not differ between reefs that differ in coral health, and that water transparency to UVR is not a factor in reef health. I measured absorption of UVR and UV irradiance at various reefs in the Florida Keys that differ in distance from shore and degree of anthropogenic development of the adjacent shoreline. My results show that intact shoreline - associated reefs and inshore reefs tend to be exposed to lower intensities of UVR, and lower degrees of photic stress, than developed shoreline - associated reefs and offshore reefs. Absorption due to CDOM (ag320) was higher, and photic stress, as revealed by increased production of UV-absorbing compounds, Mycosporine - like Amino Acids (MAAs), was lower at the surface compared to the bottom. The following results support my conclusion: ag320 and UV attenuation coefficients (Kd 's) were higher at intact compared to developed shoreline - associated reefs, and at inshore compared to offshore reefs. Spectral slope, S, was higher at offshore compared to inshore reefs, indicating a higher degree of photobleaching of CDOM. Relative expression of MAAs was higher at developed compared to intact shoreline - associated reefs, at offshore reefs compared to inshore reefs, and at the surface compared to the bottom. Solar energy reaching the benthos at two inshore reefs of the same depth (6m) was approximately an order of magnitude higher at the reef near developed shoreline compared to the reef near intact shoreline, and may be due to greater degree of diffuseness of the underwater light field combined with lower ag at the developed shoreline-associated reef.