Acoustic signatures of the seafloor: Tools for predicting grouper habitat

Groupers are important components of commercial and recreational fisheries. Current methods of diver-based grouper census surveys could potentially benefit from development of remotely sensed methods of seabed classification. The goal of the present study was to determine if areas of high grouper abundance have characteristic acoustic signatures. A commercial acoustic seabed mapping system, QTC View Series V, was used to survey an area near Carysfort Reef, Florida Keys. Acoustic data were clustered using QTC IMPACT software, resulting in three main acoustic classes covering 94% of the area surveyed. Diver-based data indicate that one of the acoustic classes corresponded to hard substrate and the other two represented sediment. A new measurement of seabed heterogeneity, designated acoustic variability, was also computed from the acoustic survey data in order to more fully characterize the acoustic response (i.e., the signature) of the seafloor. When compared with diver-based grouper census data, both acoustic classification and acoustic variability were significantly different at sites with and without groupers. Sites with groupers were characterized by hard bottom substrate and high acoustic variability. Thus, the acoustic signature of a site, as measured by acoustic classification or acoustic variability, is a potentially useful tool for stratifying diver sampling effort for grouper census

A study of near-surface currents in Endicott Arm

Thesis (Ph.D.) University of Alaska Fairbanks, 1972Currents in Endicott Arm were measured by parachute drogues and ice drift photogrammetry. The parachute drogues showed mean outflow speeds between 2 and 20 cm/sec. The mean outflow extended at reduce speeds to below ten meters and may have extended to Bill depth at twenty meters. From equations of drag and inertia, a differential equation was formed to describe tidal ice drift speeds. The equation was solved on an Analog computer and the solution shown as plotted. Coupling curves were used to measure the net tidal speed. Ice drift mean out flow speeds based upon these computations agreed with parachute drogue mean outflow speeds

A study of near-surface currents in Endicott Arm

Thesis (Ph.D.) University of Alaska Fairbanks, 1972Currents in Endicott Arm were measured by parachute drogues and ice drift photogrammetry. The parachute drogues showed mean outflow speeds between 2 and 20 cm/sec. The mean outflow extended at reduce speeds to below ten meters and may have extended to Bill depth at twenty meters. From equations of drag and inertia, a differential equation was formed to describe tidal ice drift speeds. The equation was solved on an Analog computer and the solution shown as plotted. Coupling curves were used to measure the net tidal speed. Ice drift mean out flow speeds based upon these computations agreed with parachute drogue mean outflow speeds