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  • 1
    Publication Date: 2022-05-25
    Description: © The Author(s), 2016. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in PeerJ 4 (2016): e1770, doi:10.7717/peerj.1770.
    Description: A research cruise to Hannibal Bank, a seamount and an ecological hotspot in the coastal eastern tropical Pacific Ocean off Panama, explored the zonation, biodiversity, and the ecological processes that contribute to the seamount’s elevated biomass. Here we describe the spatial structure of a benthic anomuran red crab population, using submarine video and autonomous underwater vehicle (AUV) photographs. High density aggregations and a swarm of red crabs were associated with a dense turbid layer 4–10 m above the bottom. The high density aggregations were constrained to 355–385 m water depth over the Northwest flank of the seamount, although the crabs also occurred at lower densities in shallower waters (∼280 m) and in another location of the seamount. The crab aggregations occurred in hypoxic water, with oxygen levels of 0.04 ml/l. Barcoding of Hannibal red crabs, and pelagic red crabs sampled in a mass stranding event in 2015 at a beach in San Diego, California, USA, revealed that the Panamanian and the Californian crabs are likely the same species, Pleuroncodes planipes, and these findings represent an extension of the southern endrange of this species. Measurements along a 1.6 km transect revealed three high density aggregations, with the highest density up to 78 crabs/m2, and that the crabs were patchily distributed. Crab density peaked in the middle of the patch, a density structure similar to that of swarming insects.
    Description: This work was sponsored by a grant from the Dalio Foundation, Inc, through the Woods Hole Oceanographic Institution.
    Keywords: Swarms ; Ecological hotspot ; Patchiness ; Panama ; Eastern Pacific ; Seamount ; Pleuroncodes planipes ; Hypoxic environment ; Anomuran crabs
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 2
    Publication Date: 2022-05-26
    Description: A system has been developed recently at W.H.O.I. for tracking nearsurface drogues equipped with sonobuoys using an acoustic navigation system. Surface and submerged drogues of mean depths ranging from 0.15 m to 4.88 m were tracked in the vicinity of deepwater dumpsite #106 . A least squares linear regression technique was used to determine drogue velocities over 2 hour periods. Water velocities at depths from 8 - 110 m were measured using a ship-deployed current meter coupled with acoustic tracking of the ship. The results indicated very little velocity shear in the surface mixed layer. There were two regions of _strong shear at greater depths, one associated with the main thermocline and the other presumably associated with a halocline .
    Description: Prepared for the Department of Energy under Contract DE-AC02-79EV10005 and NOAA under Grant 04-8-M01-62
    Keywords: Acoustically tracked drogues ; Ocean currents ; Waste disposal in the ocean
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 3
    Publication Date: 2022-05-26
    Description: During July and August of 1980 our research group measured nearsurface water velocities near the eastern coast of Lake Huron by tracking drogues using acoustic travel time and compass sighting techniques. The velocity fields appeared to consist of two components. These have been termed: a sub-current, which varied slowly with depth (compared to the deepest drogue depth of 5.2 m) and, in most cases, was apparently in geostrophic balance with the cross shore pressure gradient; and, a surface layer-current (defined by the relative velocity from deeper to shallower drogues) which decayed rapidly with depth and was directed nearly parallel with the wind and waves. There was no discernable relationship between wind speed and relative velocity. There was, however, a direct dependence of relative velocity with estimated surface roughness, suggesting that Stokes drift may have been primarily responsible for the shear. The magnitudes of the observed relative velocities were approximately equal to Stokes drift magnitudes calculated from representative wave energy spectra. Also reported are measurements of current and temperature structure made prior to and following a coastal upwelling.
    Description: Prepared for the Department of Energy under Contract DE-AC02-79EV10005 and the National Oceanic and Atmospheric Administration under Contract 03-5-022-26.
    Keywords: Ocean currents ; Oceanographic buoys ; Acoustic drogue measurements ; Nearsurface water measurement
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 4
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: From 1974 through 1978 a series of intensive measurements were made in the coastal waters within 12 km of Long Island. The data were derived from two sources: a mooring array from which time series of temperature, salinity and water velocity were measured at four depths at each of four offshore distances; and high resolution, daily hydrographic surveys. Analysis of subtidal cross-shore velocity fluctuations has indicated a two-layer response to wind forcing, with near-surface flow to the right of the longshore wind and opposing flow below. The magnitude of these fluctuations increased in the seaward direction on a scale nearly equal to the internal deformation radius. The phase between longshore velocity fluctuations and longshore wind stress approached zero with decreasing bottom depth, probably the result of bottom stress. The vertical structure of longshore fluctuations during stratified conditions markedly differed from that during unstratified conditions, and resembled the structure derived from a simple two-layer coastal flow model. Significant mean offshore flow was measured during experiments in August and September, despite negligible mean wind stress during the same periods. This flow was most likely due to persistent longshore density gradients, as are consistently inferred from hydrographic data taken in the vicinity.
    Description: Funding was provided by the Department of Energy under contract DE-AC02-79EV10005.
    Keywords: Water masses ; Ocean temperature ; Salinity ; Boundary layer ; Ocean currents
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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