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  • 1
    Type of Medium: Book
    Pages: 84 Seiten , Illustrationen, Graphen, Karte
    Series Statement: Nordic Seas sedimentation data file Vol. 1
    Language: English
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  • 2
    Type of Medium: Book
    Pages: 65 Seiten , Illustrationen, Graphen, Karten
    Series Statement: Nordic Seas sedimentation data file Vol. 2
    Language: English
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  • 3
    Publication Date: 2022-05-25
    Description: Based upon the 1987-88 Arctic Environmental Drifting Buoy (AEDB), the Ice-Ocean Environmental Buoy (IOEB) was developed to acquire and telemeter in near real-time inter-relatable time-series data on atmospheric, oceanographic and ice physics in ice-covered oceans during all seasons. Two IOEBs were successfully deployed in two Arctic Sea Basin Stations in April, 1992. Since then, although some sensors malfunctioned, for 18 continuous months, they have been sending massive amounts of information. In this report we describe the technology which was developed for the 1991 IOEB. Mechanically, the IOEB consists of an extremely durable surface flotation package and an underwater mooring line of instruments and sensors. The apex contains data loggers for air, ice and engineering measurements, microcontroller modules for accumulating the data from all the instruments, and ARGOS platform transmit terminals (PTTs) for broadcasting the data. Extending above the surface float, a mast supports a wind monitor and air temperature probe, which along with a barometer provides meteorological data. Thermistor strings, vibrating wire stress sensors, and a thickness gauge are installed in the ice surrounding the buoy, and are interrogated by the modules inside the apex. In the ocean, 110m of conducting strength cable passes the data from conductivity/temperature recorders, an Acoustic Doppler Current Profier and data compression module, a dissolved oxygen sensor, a transmissometer and fluorometers to the PTT microcontrollers. Furthermore, a suspended particle collector and sediment trap transmit status information along the two-wire multidrop network cable. Because the IOEB differs from the AEDB by telemetering the majority of the scientific data, a complicated compression scheme is incorporated to broadcast the data from the 103 variables within the allowable 256-bit ARGOS data stream. Via Service ARGOS, this data currently becomes available to scientists in several countries within eight hours of transmission. In April 1992, two IOEBs were deployed at separate ice camps in the Arctic Ocean with battery power adequate to sustain the systems for over two years. One was deployed 115 miles from the North Pole in the center of the Transpolar Drift sea-ice current, and the other off of the coast of Alaska along the edge of the Beaufort Gyre. Airplanes capable of landing on ice were used for the transportation of the systems to their final destination. Simultaneously, a third, reduced version of the IOEB was deployed in the Weddell Sea by the Scott Polar Research Institute.
    Description: Funding was provided by the Office of Naval Research, Arlington, Virginia, USA and Japan Marine Science and Technology Center, Yokosuka, Japan.
    Keywords: Arctic ; Telemetry ; Underwater mooring
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
    Format: 8010412 bytes
    Format: application/pdf
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  • 4
    Publication Date: 2022-05-25
    Description: There are strong reasons to gather data on polar oceanogrphy and climatology in real time using fully automated, unattended instrumentation systems for long periods; particularly during the inaccessible winter months when moving ice is extremely hazardous. We deployed an Artic Environmental Drifting Buoy (AEDB) on 4 August 1987 at 86°7'N, 22°3'E off of the FS Polarstern on a large 3.7 m thick ice island. The AEDB consisted of 2 major components: a 147 cm diameter surface float housing ARGOS transmitters and a data logger for ice-profiling thermistors, and a 125 m long mooring line attached to the sphere and fed though a 1m diameter ice hole. Along the mooring were deployed 2 fluorometers, conductivity and temperature loggers, an Acoustic Doppler Current Profiler (ADCP), a current meter, and a time-series sediment trap/micro-filter pump/transmissometer unit. The AEDB proceeded southwesterly with the Transpolar Drift at an average speed of 15.3 km/day, with a maximum speed of 88.8 km/day. On 2 January 1988, the AEDB dropped into the water while passing through the Fram Strait and for the remaining drift period was either free-floating on the water surface or underneath the sea ice. Throughout this period, the transmitters onboard successfully transmitted position, temperature, and strain caused by ice on the sphere. Although the sediment trap package was lost during the drift, valuable data was collected by the other instruments throughout the experiment. The ice thermistor data was used to determine oceanic heat flux, while continuous ADCP observations over the Yermak Plateau provided a wealth of information for understanding internal waves in the ice-covered ocean. The buoy was recovered by the Icelandic ship R/S Arni Fridriksson on 15 April 1988 at 65°17'N, 31°38'W, off southeatern Greenland, completing 3,900km of drift in 255 days. We are in the process of constructing the next automated stations which are planned for deployment in both the north and south polar regions in 1991-92.
    Description: Funding was provided by the Office of Naval Research, through grant Number NOOOI4-87,88,89,J-1288.
    Keywords: Transpolar drift ; Ice ocean environment ; ADCP ; Polarstem (Ship) Cruise ; Arni Fridriksson (Ship) Cruise
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
    Format: 5426126 bytes
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  • 5
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-25
    Description: Filtered and Earth-referenced ADCP data from the B92, B97 and S97 IOEBs were demodulated to remove inertial and near-inertial tidal frequencies, in order to highlight the low frequency components for examination of Arctic submesoscale eddys. This report describes the raw data, processing scheme, and numerical and graphical results of this analysis, which are also available at http://ioeb.whoi.edu/ioebeddys.htm. Using the demodulated timeseries of current profiles from each buoy, characteristics of 95 possible eddy encounters are quantified by (1) identifying anomalously large velocities associated with subsurface vortices, (2) determining the vortex centers and their drift, and (3) determining vortex properties as a function of radius and depth. Out of 44 total months of observations, 81 of the encounters were determined to be subsurface eddies, and 29 were eddy core encounters. Only 14 of the confirmed subsurface encounters were cyclonic, versus 66 anticyclonic, and one indeterminate. Within the southern and central Canadian basin portion of the Beaufort Gyre, halocline eddys with maximum velocities between 10 and 45 cm/s, centered around 140 m depth, and over 100 m thick were prevalent. Over the Northwind Ridge, eddy encounters were absent from any timeseries. Farther north and west over the Chukchi Cap, encounters resumed, but were generally smaller, more shallow and less intense (although these observations were mostly derived from a lower resolution transmitted data subset).
    Description: Funding was provided by the National Science Foundation Grant No. OPP-9815303, and by the Office of Naval Research Grant No. N00014-97-1-0135.
    Keywords: Arctic halocline eddys ; Upper ocean currents ; Drifting buoy observations
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
    Format: 15792824 bytes
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  • 6
    Publication Date: 2022-05-25
    Description: Between 1992 and 1998, three Ice-Ocean Environmental Buoys (IOEBs) were deployed a total of six times on multiyear pack ice in the Arctic Ocean. The processing scheme for the telemetered environmental data, as well as the individual IOEBs and field operations, are described, and the processed data are presented in graphical form. The IOEB Archived Data Processing (IADP) processing scheme was conceived specifically to remove noise in data telemetered from IOEBs caused by errors in network or satellite communications, and to calibrate to absolute values. The location data consists of Argos quality 2 or 3 positions from each platform transmit terminal (PTT) on a particular IOEB, which are subsequently screened, interpolated, and combined with similarly processed locations from the other PTT, and further smoothed with a 6-hr triangular filter to produce an hourly timeseries with a standard error estimated to be -150 m. The sensor data is prefiltered, combined, adjusted for buoy drift, and screened with a Gaussian first difference filter to produce unevenly spaced timeseries of each variable measured by the IOEB. Every variable is output to a unique file per year, per buoy consisting of a two-column ACSII timeseries. Drift and sensor data are presented from the 1992 Transpolar Drift IOEB which operated for only 4 months, IOEB-1 which drifted with the Beaufort Gyre in a large anticyclonic circle from April 1992 to November 1998, and IOEB-2 which drifted through the Fram Strait in 9 months in 1994, and 1997-98 was redeployed concurrently with SHEBA at a distance 50 km from the main camp.
    Description: Funding was provided by the Office of Naval Research under contract number N00014-99-10335 and Japan Marine Science and Technology Center.
    Keywords: Arctic buoy ; Air data ; Ice data ; Ocean data ; Environmental observations ; Ocean-atmosphere interaction ; Sverdrup II (Ship) Cruise ; Des Grosilliers (Ship) Cruise ; Louis S. St. Laurent (Ship) Cruise
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
    Format: 5216445 bytes
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  • 7
    Publication Date: 2022-05-25
    Description: This technical report presents the results of analyses on opal, organic carbon, nitrogen and phosphorus content in each of 156 specimen samples collected from the moored sediment trap experiment that was a part of JGOFS North Atlantic Bloom Experiment. The analyzed samples represent a spatio-temporal matrix formed by 6 time-series sediment traps that provided 26 periods of uniform and synchronized periods of 14 days, except for one longer and one shorter period. Traps were deployed at 3 depths, 1 km, 2 km and 0.7 km above the bottom, and at 2 stations, 34°N 21°W and 48°N 21°W from April 4, 1989 to April 17, 1990, as shown in Tables 1 and 2. There was an 20-day hiatus in September /October 1989 for changeover of the trap moorings. Some samples were unusable because of the in trusion of fish. Samples were separated into several aliquots by wet-splitting, then water sieved into larger-than- and smaller-than-1-mm sizes. The fluxes of biogeochemical elements and constituents were determined on these aliquots and size fractions for: carbonate by vacuum gasometric method; opal by selective leaching method; reactive phosphorus by high temperature oxidation hydrolysis method; and organic carbon and nitrogen by applying an elementary analyzer. The annual fluxes, fluxes during the bloom, pre- and post-bloom episodes were normalized to a 365-day calendar year (Table 6) and are summarized in Tables 7 to 12. Variabilty of particle fluxes by each period at the two stations in terms of size fractions, sedimentary constituents and elements are shown in Tables 13 and 14. The molar ratios between pairs of critical biogeochemical elements during each episode and annually, shown at various depths and stations, are included in Tables 10 through 14.
    Description: Funding was provided by the National Science Foundation through Grant No. OCE 88-14228.
    Keywords: Particle flux ; Bloom ; North Atlantic Ocean ; Terminal ratio ; Ocean interior ; Atlantis II (Ship : 1963-) Cruise AII119-2 ; Endeavor (Ship: 1976-) Cruise EN203 ; Charles Darwin (Ship) Cruise CD5B
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
    Format: 6589166 bytes
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  • 8
    Publication Date: 2022-05-26
    Description: This document represents the cruise report of the highly successful Leg 1 of the R/V Knorr cruise to the Black Sea (Cruise 134-8) as a joint Turkish-American Oceanographic Expedition (Izmir to Istanbul, April 16 to May 7,1988). The focus of Leg 1 was to study the biogeohemical variability in sedimentation in the present and throughout the anoxic history of the Black Sea with high spatial and temporal resolution. In particular, this study involved the integrated study of water column fluxes (sediment traps, suspended sediment investigations, etc.), benthic boundary layer ("fluff layer"), and laminated bottom sediments (box cores, giant gravity cores). Highlights of the cruise include the collection of 62 giant gravity cores, and 30 box cores with perfectly laminated sediment and, for the first time ever, with the intact fluff layer. Three moorings with time-series sediment traps were deployed in the abyssal regions of the eastern, central, and western Black Sea to collect continuous samples over a time period of about 1 year and 3 months. Summarized in the cruise report are logistics of the cruise, sample collections and descriptions, and preliminary discussions of observations and first measurements.
    Description: Funding was provided by the National Science Foundation under various grants to shipboard participants
    Keywords: Particle flux ; Laminated sediments ; Knorr (Ship : 1970-) Cruise KN134-8
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
    Format: 9137651 bytes
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  • 9
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: A large, open ocean applicable sediment trap has been developed at the Woods Hole Oceanographic Institution in order to assess the fluxes of particles sinking through the deep water column, under the sponsorship of the National Science Foundation. PARFLUX Mark II trap, 1978-79 version for PARFLUX phase 1 program, has been successfully developed and has gathered much meaningful data. A trap opening is 1.5 m2 and consists of 94 hexagonal buffer cells with the nominal form ratio of 2. Sediment particles are concentrated to the receiving cup located at the bottom of the funnel-shaped trap. Two types of receiving cups have been developed; a trap with Type S cup is open at both ends as it sinks to the designated depth. Twenty-four hours after the deployment the receiving cup moves into alignment with the funnel to store the sediment. At the end of deployment a spring mechanism activated by a quartz oscillator based electrical timer-release retracts the receiving cup, seals the collected sample and leave the funnel open at both ends while the trap ascends for recovery. Type C mechanism is installed with a shutter which seals the cup during recovery; this type involves a simple mechanism with less moving parts. Sodium azide/sodium chloride solution is diffused through a series of membrane filters to keep the cup contents in an aseptic condition. Since October 1976 to December 1979, we have deployed and recovered 24 traps successfully along with several moorings as deep as 5,600 m for as long as 112 days. This reports the engineering detail and lists the required parts to assist the construction, operation and maintenance of the PARFLUX Mark II sediment trap.
    Description: Prepared for the National Science Foundation under Grants OCE 76-82063 and OCE 77-27004.
    Keywords: Suspended sediments ; Oceanographic instruments ; Scientific apparatus and instruments
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 10
    Publication Date: 2022-05-26
    Description: With the support of the National Science Foundation, we have completed the first cruise devoted to the GOFS and JGOFS program for the North Atlantic Bloom studies between March 28 and April 6 on board R/V Atlantis II. The major task of this cruise, to deploy bottom-tethered mooring arrays with time-series sediment traps along with current meters at two critical stations, 34°N and 47°N along 20°W, was accomplished. All 6 sediment traps, 3 on each array, were set at 14-day intervals for 13 periods from April 3 to September 26, 1989. Their opening and closing times were synchronized throughout the period of deployment. The arrays and instruments will be recovered and redeployed in September/October, 1989. Ancillary water column data, such as CTD, fluorometry, pigments, and major nutrient distribution, were also successfully completed (except for transmissometry profiling at the 47°N station) in order to understand the prebloom setting at JGOFS 34°N, 47°N, and 60°N stations. At the 47°N station on April 2, the mixed layer depth was 248m.
    Description: Funding was provided by the National Science Foundation through grant Number OCE 88-14228.
    Keywords: Joint Global Ocean Flux Study ; Marine sediments ; Atlantis II (Ship : 1963-) Cruise AII119-2
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
    Format: application/pdf
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