Currents, temperature, conductivity, and sigma-theta data collected from moored instruments deployed from the platform ARGO MAINE in the Stellwagen Bank National Marine Sanctuary in support of Massachusetts Bay Internal Wave Experiment between August 4, 1998 and September 2, 1998 (NCEI Accession 0061443)
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title: Currents, temperature, conductivity, and sigma-theta data collected from moored instruments deployed from the platform ARGO MAINE in the Stellwagen Bank National Marine Sanctuary in support of Massachusetts Bay Internal Wave Experiment between August 4, 1998 and September 2, 1998 (NCEI Accession 0061443)
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abstract: A 1-month 4-element moored array experiment to measure the currents associated with large-amplitude internal waves generated by tidal flow across Stellwagen Bank.
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supplementalInformation: This archival package contains only a snapshot of the USGS time series database. The data on the originator's website, http://stellwagen.er.usgs.gov/, may have updates that are not yet captured here. USGS PI: B. Butman Collaborators: R. Beardsley, A. Scotti and S. Anderson (Woods Hole Oceanographic Institution) Publications: Butman, Bradford, Alexander, P.S., Anderson, S.P., Lightsom, F.L., Scotti, Alberto, and Beardsley, R.C., 2006, The Massachusetts Bay internal wave experiment, August 1998; Data Report: U.S. Geological Survey Data Series 85, DVD-ROM. Also available online at https://pubs.usgs.gov/ds/2006/85/ *** NOTE: NODC received a DVD copy of Version 2 of this data report as part of the data submission. The disc contents and disc image are located in 0-data directory. Data files in USGS Data Series 85 V.2 may be preliminary versions of the data. Therefore, this data report should be used for reference purposes only. Data files are also provided in the 0-data directory, which may be updated versions or duplicates of the files from the DVD. Butman, B. Alexander, P.S., Scotti, A., Beardsley, R.C., and Anderson, S.P., 2006, Large internal waves in Massachusetts Bay transport sediments offshore. Continental Shelf Research. v. 26/17-18, pp 2029-2049. https://doi.org/10.1016/j.csr.2006.07.022 Scotti, A., Beardsley, R.C., Butman, B., 2006, On the interpretation of energy and energy fluxes of nonlinear internal waves: An example from Massachusetts Bay. J. Fluid Mechanics, v. 561, pp. 103-1112. https://doi.org/10.1017/S0022112006000991 Scotti, A., Beardsley, R.C., and Butman, B., 2007, Generation and propagation of nonlinear internal waves in Massachusetts Bay, Journal of Geophysical Research, 112, C10001, https://doi.org/10.1029/2007JC004313. Scotti, A., Beardsley, R.C., Butman, B., and Pineda, J., in press, Shoaling of nonlinear internal waves in Massachusetts Bay. Journal of Geophysical Research. https://doi.org/10.1029/2008JC004726 Scotti, A., Butman, B., Beardsley, R.C., Alexander, P. Soupy, Anderson, S.P., 2005, A modified beam-to-earth transformation to measure short-wavelength internal waves with an Acoustic Doppler Current Profiler (ADCP), J. Atmospheric and Oceanic Technology, 22(5), pp. 583-591. https://doi.org/10.1175/JTECH1731.1
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description: Acoustic Doppler Current Profiler The Acoustic Doppler Current Profiler (ADCP) measures currents beneath a ship while underway. Sound signals sent from the moving ship bounce back to receivers aboard the ship. This provides a profile of water movement relative to the ship-precise modern navigation, allowing the ship's motion to be subtracted from the data. These devices are also used on moorings and profilers and, along with acoustic backscattering, measure animal biomass. Particles in the path of the sound waves, mostly plankton, reflect a small part of the sound energy back toward receivers, allowing researchers to make remote estimates of the sizes and numbers of animals present in the water column. Before the 1970's, the most technologically advanced instrument used to measure water velocity was known as a Doppler speed log. This evolved into the first commercial ADCP, produced in the mid-1970's, which used averaging. Later in the 1970's, the first vessel-mounted ADCP was developed to measure water velocity more accurately and to allow measurement in range cells over a depth profile. As instruments evolved, so did new techniques in Doppler signal processing. Initially, Doppler speed logs used simple analog signal processing methods, which are still used in some commercial speed logs today. However, the first ADCPs incorporated analog-to-digital signal conversion over a narrow communication bandwidth. Around 1990, this technique was developed into broadband signal processing. Since then, broadband ADCPs have been able to generate very accurate, real-time velocity measurements.
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