Fast acoustic tomography of costal, tidally-driven temperature and current fields

Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Ocean Engineering, 1998.Includes bibliographical references (leaves 160-169).by Pierre Elisseeff.Ph.D

A review of progress and applications of pulsed doppler wind LiDARs

Doppler wind LiDAR (Light Detection And Ranging) makes use of the principle of optical Doppler shift between the reference and backscattered radiations to measure radial velocities at distances up to several kilometers above the ground. Such instruments promise some advantages, including its large scan volume, movability and provision of 3-dimensional wind measurements, as well as its relatively higher temporal and spatial resolution comparing with other measurement devices. In recent decades, Doppler LiDARs developed by scientific institutes and commercial companies have been well adopted in several real-life applications. Doppler LiDARs are installed in about a dozen airports to study aircraft-induced vortices and detect wind shears. In the wind energy industry, the Doppler LiDAR technique provides a promising alternative to in-situ techniques in wind energy assessment, turbine wake analysis and turbine control. Doppler LiDARs have also been applied in meteorological studies, such as observing boundary layers and tracking tropical cyclones. These applications demonstrate the capability of Doppler LiDARs for measuring backscatter coefficients and wind profiles. In addition, Doppler LiDAR measurements show considerable potential for validating and improving numerical models. It is expected that future development of the Doppler LiDAR technique and data processing algorithms will provide accurate measurements with high spatial and temporal resolutions under different environmental conditions

Patterns among micronekton communities in relation to environmental conditions at two shallow seamounts in the south-western Indian Ocean

Seamounts are ubiquitous topographic features across all ocean basins. They rise steeply through the water column from abyssal depths. Depending on their size, shape and summit depths, seamounts reportedly have an influence on the physical flow regimes which may promote the aggregation of zooplankton, micronekton, and top predators above or in the immediate vicinity of their summits. Micronekton form a key trophic link between zooplankton and top marine predators, and are divided into the broad categories: crustaceans, cephalopods and mesopelagic fishes. The vertical and horizontal distributions, assemblages and trophic relationships of micronekton were investigated at two shallow seamounts of the south-western Indian Ocean. La Pérouse is a steep bathymetric feature rising from a deep seabed located at 5000 m and with a summit depth at ~60 m below the sea level. This seamount is located at the north-western periphery of the oligotrophic Indian South Subtropical Gyre province. A seamount to the south of Madagascar, named “MAD-Ridge” in this study, has a summit depth at ~240 m below the sea level and rises from a base at ~1600 m. MAD-Ridge is located within an “eddy corridor” within the productive East African Coastal Province. The micronekton acoustic densities were greater at MAD-Ridge relative to La Pérouse, in accordance with the difference in productivity between the two sites. Physical processes within the cyclonic mesoscale eddy sampled during the MAD-Ridge cruise led to enhanced micronekton acoustic densities in the eddy relative to the MAD-Ridge seamount. While the shallow scattering layer (0-200 m) consisted of common oceanic micronekton species, the summits and flanks of La Pérouse and MAD-Ridge both showed presence of resident or seamount-associated fish species during day and night. Micronekton were also shown to exhibit a range of migration strategies such as diel vertical migration, mid-water migration and no diel migration. However, despite the differing productivity between both pinnacles, crustaceans, smaller-sized squids and mesopelagic fishes exhibited trophic levels ranging from 3 to 4 at both seamounts. This thesis highlights important knowledge gaps on seamount ecosystems and ecological patterns associated to shallow pinnacles. It also underlines the importance of studying seamount ecosystems of the south-western Indian Ocean in order to promote management and conservation measures for a sustainable use of such specific environments

Proceedings of the NASA Symposium on Global Wind Measurements

This Proceedings contains a collection of the papers which were presented at the Symposium and Workshop on Global Wind Measurements. The objectives and agenda for the Symposium and Workshop were decided during a planning meeting held in Washington, DC, on 5 February 1985. Invited papers were presented at the Symposium by meteorologists and leading experts in wind sensing technology from the United States and Europe on: (1) the meteorological uses and requirements for wind measurements; (2) the latest developments in wind sensing technology; and (3) the status of our understanding of the atmospheric aerosol distribution. A special session was also held on the latest development in wind sensing technology by the United States Air Force