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  • 1
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2016. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research: Oceans 121 (2016): 1789–1805, doi:10.1002/2015JC011252.
    Description: The drivers of spring and summer variability within the coastal ocean east of Cape Cod, Massachusetts, a critical link between the Gulf of Maine and Mid-Atlantic Bight, are investigated using 2 years of shipboard and moored hydrographic and velocity observations from 2010 and 2011. The observations reveal sharp differences in the spring transition and along-shelf circulation due to variable freshwater and meteorological forcing, along with along-shelf pressure gradients. The role of the along-shelf pressure gradient is inferred using in situ observations of turbulent momentum flux, or Reynolds stresses, estimated from the ADCP-based velocities using recently developed methods and an inversion of the along-shelf momentum balance. During spring, the locally relevant along-shelf pressure gradient contains a sizable component that is not coupled to the along-shelf winds and often opposes the regional sea level gradient. Together with the winds, local pressure gradients dominate along-shelf transport variability during spring, while density-driven geostrophic flows appear to match the contribution of the local winds during summer. These results suggest that local effects along the Outer Cape have the potential to cause significant changes in exchange between the basins.
    Description: NOAA. Grant Number: NA10OAR4170083; Woods Hole Oceanographic Institution
    Description: 2016-09-19
    Keywords: Coastal circulation ; Reynolds stresses ; Pressure gradients ; Along shelf transport ; Inter-annual variability
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 2
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    Woods Hole Oceanographic Institution, Department of Physical Oceanography
    Publication Date: 2022-05-26
    Description: This data was collected by Kirincich and Lentz as part of the Inner Shelf Lateral Exchange Study focused on examining the spatial variability of the mechanisms and process that lead to the exchange of water masses across the inner part of the continental shelf. The ISLE study area spanned a 15 km by 25 km domain south of the Island of Martha’s Vineyard Massachusetts. See published works by Kirincich (2016, JOAT) or Kirincich and Lentz (2017, JGR) for details on the study area. The two zip files contain three types of files: HF radar surface currents, station/mooring velocity data, and station/mooring hydrography data. See the text files for additional information. Converted to netCDF via MATLAB by A. Kirincich.
    Description: HF radar surface currents data was collected by Kirincich as part of ongoing studies examining the spatial variability of the mechanisms and process that lead to the exchange of water masses across the inner part of the continental shelf. The data consists of estimates of the near-surface horizontal (East and North) ocean currents made via High Frequency (HF) radar-based remote sensing of the ocean backscatter spectrum. The dataset spans an 18-month period from February 2011 to August 2012. The effective measurement depth of the WHOI HF radars is 0.5 m below the ocean surface.
    Description: Station/mooring velocity and hydrography data was collected by Kirincich and Lentz as part of the Inner Shelf Lateral Exchange Study focused on examining the spatial variability of the mechanisms and process that lead to the exchange of water masses across the inner part of the continental shelf. The data consists of estimates of Water Temperature and Salinity using SBE 37 Microcats, and horizontal (East and North) ocean currents made via ADCPs with transmit frequencies of 600 or 120 kHz. The dataset spans the 6—8 month period of June 9th 2014 to January 15, 2017.
    Description: The observations used in this study were supported by NSF OCE Grant #1332626 and internal funding from the Woods Hole Oceanographic Institution.
    Repository Name: Woods Hole Open Access Server
    Type: Dataset
    Location Call Number Expected Availability
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  • 3
    Publication Date: 2022-05-26
    Description: Author Posting. © American Geophysical Union, 2017. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research: Oceans 122 (2017): 2360–2381, doi:10.1002/2016JC012491.
    Description: This study examines the spatial variability of transport within the inner-shelf south of Martha's Vineyard Massachusetts, its time and space dependence, and its importance to the total volume exchanged between the nearshore and the coastal ocean. The exchange of water across the inner shelf is often considered to be driven primarily by wind forcing, yet the effects of small-scale O(1–10 km) variability on the total exchange have not been well quantified. Using a combination of high-resolution HF radar-based surface currents and a dense array of moorings to document the lateral variability of across-shelf exchange, the cumulative wind-driven across-shelf transport over the summer stratified period was less than the volume of the inner-shelf onshore of the 25 m isobath. Along-shelf variations in the wind-driven exchange were as large as the spatial mean of the wind-driven exchange. A spatially varying time-averaged circulation caused by tidal rectification resulted in across-shelf exchange larger in magnitude than, and independent of, the integrated wind-forced exchange. Coherent submesoscale eddies also occurred frequently within the domain due to flow-topography effects onshore and horizontal density gradients offshore, generally with lifespans shorter than 10 h, diameters smaller than 6 km, and vertical depths shallower than 10 m. The across-shelf volume transport due to eddies, estimated by seeding particles within the surface current fields, was more than half the wind-driven depth-dependent exchange. Thus, accounting for the potential coherent along-shelf variability present over the inner shelf can significantly increase estimates of the across-shelf transfer of water masses and particles.
    Description: The 2014 ISLE field study as well as this analysis was supported by NSF OCE grant 1332646 and the Woods Hole Oceanographic Institution.
    Description: 2017-09-24
    Keywords: Inner shelf ; Across-shelf transport ; Spatial variability ; Exchange ; Eddies ; Martha's Vineyard
    Repository Name: Woods Hole Open Access Server
    Type: Article
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