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Remote Sensing of Submerged Oceanic Turbulence and Fossil Turbulence

Microstructure and internal-wave measurements from vertical and horizontal profilers near a Honolulu municipal wastewater outfall are compared to soliton-induced sea-surface brightness anomalies from optical and synthetic-aperture-radar space satellite images. Spectral anomalies with wavelengths 30-1000 m were detected September 2, 2002. Anomaly areas covered 70 km in 10 km and 5 km SW and SE lobes extending from the diffuser. Studies in 2003 and 2004 increase the range of detection to 20 km from the outfall in areas covering 200 km. The remote detection mechanism indicated by these remarkable observations is a complex interaction between advected 10 m outfall fossil turbulence patches and internal-soliton-waves (ISWs). ISWs supply new turbulent-kinetic-energy to outfall patches near the pycnocline depth. Energy, mixing, and information is radiated near-vertically by both the primary and secondary fossil turbulence patches in ISW patterns of surface smoothing, as detected from space. Nonlinear vertical-amplification