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  • Ocean currents  (58)
  • Cell & Developmental Biology
  • General Chemistry
  • Limnology
  • Woods Hole Oceanographic Institution  (59)
  • Iranian Fisheries Science Research Institute  (6)
  • 2015-2019  (65)
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  • 1
    Publication Date: 2021-05-19
    Description: Aquaculture activity is restricted mainly to rainbow trout in cold waters and carps in warm waters in inland waters of Iran as well as Fars Province. Probably for this reason saline waters of south and southeast Fars have not been used for aquaculture. These rivers are ecosystems with a diverse biota, it is predictable that can be found some there endemic aquatic organisms with a potential for aquaculture. Finding a suitable organism can help increase wise use of this natural resource, and local production and recruitment. However, it is highly needed to investigate various environmental elements prior to any use to obtain an estimation of the environmental consequences, parallel to finding usage potentials. In This study, we investigated Dehram saline river in south of Fars Province. Hydrological and physiographical properties, chemical composition of the river, and aquatic populations were sampled and measured monthly in 3 stations in one year. Salinity, electrical conductivity, and total dissolved solids increased from station 1 to 3, reaching from 6.6 g/L, 14.3 g/L, and 12800 µs/cm to 13.5 g/L, 17.7 g/L, and 16500 µs/cm, respectively. Dissolved oxygen and oxygen saturation were higher in station 3, and in autumn and winter. Nitrite showed lowest values in winter (0.006 mg/L) and highest values in spring (0.013 mg/L). Nitrate showed the lowest concentration in station 3 (0.43 mg/L), but no differences were seen among seasons. Ammonium showed no differences among stations or seasons. Phosphate levels in station 1 and 3 were 0.13 mg/L‌to 0.17 mg/L, with the highest level (0.29 mg/L) seen in the spring. Five species of fishes were identified in the river, which all were widely favored by local people. Some of these have been categorized as edible in previous studies, others as ornamental. On the other hand, intensive growth of an algal species throughout the river demonstrates a potential for algal cultivation. Significant role of algae in production of food for both man and livestock is now well recognized in aquaculture industry.
    Description: Iranian Fisheries Science Research Institute
    Description: Published
    Keywords: Ecology ; Dehram River ; Limnology ; Saline water ; Physico-chemical parameters ; Aquaculture
    Repository Name: AquaDocs
    Type: Report , Refereed
    Format: 62pp.
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  • 2
    Publication Date: 2021-05-19
    Description: Limnological factors of brackish water pounds of the rainbow trout, Onchorhynchus mykiss were studied at Bafgh region in Yazd province. Physicochemical factors, phytoplankton, zooplankton and benthic populations of pools, supply and drainage channels from different farms were studied in aquaculture cycle in 2002 and 2003. Means were compared using Tukey HSD and t tests. Meanings of factors in 2002 and 2003 were respectively: and 9.3 0.2ppt; dissolved oxygen 7.9 0.2mg/l water temperature 13.8 0.3°c and 14.9 0.6°c; salinity 12.3 0.2ppt and 7.2 0.1mg/l; pH between 7.8 to 9.2 and 8.1 to 9.5; depth of hyalinity 0.85 0.1m and 1.1 0.1m; ammonium 0.1-0.5mg/l; and nitrate 1.8-21mg/l. Main phytoplankton were diatoms specially Chaetoceros, and Cyanophyta. Rotifera were the dominant zooplankton. Benthic fauna mainly included immature Chironomids. Final mean lengths were between 24.7cm to 31.5cm, mean weights between 11179.9gr to 434.6gr. FCR between 1.16 to 1.6; DGR between 1.04gr/day to 3.03gr/day; production 0.03kg/m2 to 0.84 kg/m2. Supply channels had the optimum limnological condition for trout aquaculture. Limnological factors were often not significantly different between pools and drainage channels. Saeeid and Rangin-Kaman farms were the most successful farms.
    Description: Iranian Fisheries Science Research Institute
    Description: Published
    Keywords: Limnology ; Brackish water ; Onchorhynchus mykiss ; Rainbow trout ; Phytoplankton ; Zooplankton ; Chaetoceros ; Survey ; Pond culture
    Repository Name: AquaDocs
    Type: Report , Refereed
    Format: 175pp.
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  • 3
    Publication Date: 2021-05-19
    Description: Gahar-roud is in 18 kilometer far from Doroud city from East of lorestan province . This river orginated from internal part of Oshteran-kouh mountain altitude and Gahar-Lake . Survey on Gahar roud Limnology began from the end of 2001 year and during the 18 month achived, at first on the length of 20 kilometer five station of sampling was selected and biological, physical and chemical character of this river was surveyed this river in all path of it feeding with large and small spring, little rivers and water of icehouse. The amount water of this river is different and maximum water is about 21 m/s in April month. Specifity of this river is be enough the temperature of water for fish. Minimum in the Jan is about 3 centigrad deegree and maximum is July and Aug about 24 centigrade deegree phis between 6.5-8.2 and is few basic . solauble oxigen is enough and is between 8.5-13 mg/lit.during the year.This river is very bright and haven t the source of polution and during the path of river and be enaugh the dosage of mineral in water are the important physical and chemical character of this river. Gahar-roud is not biological hardness quality. About 31 genus and species from 5 family of phytoplangton and 42 genus from 26 family from the order of insects, molusca, worms and crustacea and 9 species from 12 family from the side aquatic. Plants was collected and recognized. Based on ecological potential of this region, because Gahar- roud river is poor for food material and classified in oligotroph river and hasn t high biological value. And also have a few population and in fact haven t any population and based on the safer system belong to the quatiy elass of oligotroph and amount of water, regular circulation of water with microclima condition rate of natural resource land around river, having program for culture of cold water fish is important but it is better that use from culture of fish, be regulated key word limnology, Gahar-roud, river plangton, bentoz, fish.
    Description: Iranian Fisheries Science Research Institute
    Description: Published
    Keywords: Limnology ; Fish ; Bentos ; Plankton
    Repository Name: AquaDocs
    Type: Report , Refereed
    Format: 84pp.
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  • 4
    Publication Date: 2022-05-25
    Description: Joint US-USSR Mid-Ocean Dynamics Experiment (POLYMODE)
    Description: Under grant OCE78-25612 from the Office of the International Decade of Ocean Exploration of the National Science Foundation .
    Keywords: Ocean currents
    Repository Name: Woods Hole Open Access Server
    Type: Working Paper
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  • 5
    Publication Date: 2021-05-19
    Description: Dorudzan reservoir is the main provider of drinking water for the capital Shiraz, as well as the most significant storage of water in the Kor river course. In addition of eroded material, a load of agricultural outputs from upstream are moved to the lake every year. Main physiographic, physical and chemical, and biological components of the lake were monthly sampled and analysed from Novembr 2010 to October 2011. Mean annual measures were water temperature 16.7 ˚C (SD=5.8), pH 8.2 (SD=0.3), dissolved oxygen 7.6 mg/l (SD=1.7), ammonium 0.05 mg/l (SD=0.08), nitrite 0.004 mg/l (SD=0.003), nitrate 0.44 mg/l (SD=0.44), phosphate 0.20 mg/l (SD=0.23), silicate 7.00 mg/l (SD=2.49), BOD 2.29 mg/l (SD=1.00), COD 24.49 mg/l (SD=15.47), electrical conductivity 720 µs/cm (SD=219), total dissolved solids 457.67 mg/l (SD=138.72), calcium hardness 61.30 mg/l (SD=13.45), and magnesium hardness 20.23 mg/l (SD=9.18). Living parts of the ecosystem including species of fish, orders and families of benthic invertebrates, zooplanktons, and phytoplanktons were investigated. Benthic macroinvertebrates included various nematodes, oligochates, gastropods, bivalves, and insect larvae (dipteral and coleptera), most abundant of which were dipteran larvae, mollusks, and nematodes. Dominant zooplankton was Bosmina, with Daphnia and Cyclops in next ranks. Among rotifer, Trichocera was more abundant than Lecanae. Bosmina showed the most abundance in summer and Daphnia in spring. Trichocera had its most abundance in summer as well, while Lecanae was more abundant in Automn and winter. A total of 41 algal genera from 8 divisions were found. Dominant phytoplankton division was Chlorophyta, with genus Pediastrum. Dominant microalga was Dynobrion (Chrysophyta) in Spring, Cylindrospermum and (both Cyanophyta) in Summer, Microsystis in Automn, and Ceratium (Dynophyta) in Winter. Ceratium were found in all seasons in most of the sampling sites, and showed highest abundance compared to other genera of its division. Dominant genus of diatoms was Fragilaria. Fish populations include Alburnus mossulensis, Capoeta aculeate, Capoeta damascina, Carasobarbus luteus, Carassius gibelio, Cyprinus carpio, and Hypophthalmichthys molitrix. Main different parts of the lake showed quite different composition of fish species. An epidemic occurance of the crustacean ectoparasite Lernea cyprinacea among most fishes was another important finding. These findings will serve as a base for future studies as a set point of drought situations.
    Description: Iranian Fisheries Science Research Institute
    Description: Published
    Keywords: Limnology ; Reservoir ; Plankton ; Fish ; Alburnus mossulensis ; Capoeta aculeate ; Capoeta damascina ; Carasobarbus luteus ; Carassius gibelio ; Cyprinus carpio ; Hypophthalmichthys molitrix
    Repository Name: AquaDocs
    Type: Report , Refereed
    Format: 72pp.
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  • 6
    Publication Date: 2021-05-19
    Description: Abbarik River is an important river in Kerman. Study of limnology of Abbarik River for aquatics & culture was started from Mehr 1381 to Day 1382. Base of this study was physical- chemical and Biological factors. In this research 3 stations was appointed. PH- oxygen- salinity- Ca- Mg- Na- K- Cl and was majored and bentetic- fish was recognized. This study was achievement in 4 season and twice in month. Bentosis recognize was Ephemeroptera- Diptera- Anisoptera- Cleoptera Trichoptera Fishes recognize was Capoeta damascina- Nemachilus sargadensis- Cyprinion watsoni.
    Description: Iranian Fisheries Science Research Institute
    Description: Published
    Keywords: Physical ; Chemical ; Biological ; Limnology ; Bentosis fish ; Aquatic ; Culture ; PH ; Salinity ; Oxygen ; Ephemeroptera ; Diptera ; Anisoptera ; Cleoptera Trichoptera ; Capoeta damascina ; Nemachilus sargadensis ; Cyprinion watsoni
    Repository Name: AquaDocs
    Type: Report , Refereed
    Format: 44pp.
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  • 7
    Publication Date: 2021-05-19
    Description: The shiroud river is one of the important riveres in point of view of fisheries matter which located in western part of Mazndran provience. The project of Limnological study have done in this river during June/ 2002 - Jun / 2003 for more and better underestanding situations, of biological and nonbiological parameters like as phytoplankton, zooplonkton, benthoses, Ichthyology, physico - chemical and pesticides of water. - Physico- chemical paramaters by ASTM methods and spectrophotometer and pestisides by US-EPA- method and GC- ECD determined. The procedures of detemination of zooplanklon and phytoplankton by manuals of Newell, 1970 and Sorina, 1974 idantify and determined respectinely. In Ichthyology, by manual procedure Berg, 1949 identifind. The sampeling have been in four stations during four seasons and result as follow: - The maximum and minimum amount of pH were in station 5 (spring) and Station no. 4 (summer) 8.19 and 7.75 respectively. - The maximum and minimum temperature of water were in station no. 8 (summer) and stations no. 2 (winter) 27.7 c and 7.7c respectively. The fluctuatcions of nutroients datas of this study and other studies done during last 5 years showed, there were not big diffrence between them but also these datas were very close to each other. - The maximum residues of pesticides for heptachlor Epoxide (Winter ) and Lindane (spring) betweenresidues of sixteen pesticdes were 79.4 and 3.7 ppb respectively. - The maximum and minimum amount of phytoplankton biomass belong to chrysophyta during four seasons were 2572 through 1081 mg/m3. - The percentage of zooplankton belong to Rotatoria , Protozoa , Copepoda , Cladocera and Zoobenthos were in 41 , 31 , 12 , 4 and 12 percent recpectively. - The maximum aboundant percentage of bentheic animals belong to Diptera with 42 percent and were dominate whole sampeling stations . - The abundence of fishes in this river belong to two species of C. capoeta gracilis and Al. bipunctatus were catched in four seasons at eight stations . The percentages of C. capoeta gracilis species were catched in four seasons at eight stations during winter, summer , spring and fall with 96 ,81 , 73 and 67 percent respectively. The percentages of Al. bipunctatus species were catched in four seasons at eight stations during winter, summer , spring and fall with 47 , 44 , 43 and 40 percent respectively.
    Description: Iranian Fisheries Science Research Institute
    Description: Published
    Keywords: Pesticdes residues ; Phytoplankton ; Zooplankton ; Riverine fishes ; Nutrients ; Limnology ; ASTM ; Rotatoria ; Protozoa ; Copepoda ; Cladocera ; Zoobenthos
    Repository Name: AquaDocs
    Type: Report , Refereed
    Format: 127pp.
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  • 8
    Publication Date: 2022-05-26
    Description: The New England Shelf/Slope Experiment (NESS76) was conducted from February to August in 1976 over the continental margin south of the New England coast. The initial objective of the experiment was to examine the kinematic and dynamic coupling of the low frequency oceanic motions between the outer New England shelf and the deeper slope/rise regions; and in particular, to monitor simultaneously the current, temperature, and bottom pressure fluctuations across the New England continental margin. The field program contained several components: (1) a six-month moored array to monitor current, temperature, and bottom pressure; (2) two hydrographic cruises conducted around the moored array; (3) a collection and synthesis of the synoptic meteorological data; and (4) detailed bathymetric surveys conducted around the deeper moorings. The two hydrographic cruises were conducted during May 11-21 and August 12-23 of 1976, and the initial results from the cruises have been reported elsewhere by Limeburner, Vermersch, and Beardsley (1978). Only the moored array and the meteorological data will be presented here.
    Description: Prepared for the National Science Foundation under Grants OCE 76-01813, OCE 78-19513, OCE 76-2590 and OCE 76-02190.
    Keywords: Moored arrays ; Continental margins ; Ocean currents
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 9
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: A ship towed log for use on ships-of-opportunity to measure ocean surface currents was built and tested over the past two years. The technique used is one of the oldest known to navigators. The ship's dead reckoned position is calculated from the speed and heading as measured by the towed log. This is then compared to the ship's true position as obtained from a reference navigation system (Loran, satellites, etc.) and the difference is attributed to the currents encountered by the ship. The system was used on six sea cruises and was successfully towed over 11,000 miles. While it i s not capable of making high precision current measurements as would be obtained from moored current meters, it can distinguish features on the order of 20 to 30 em/sec. over a large horizontal scale in the upper ocean.
    Description: Prepared for the Office of Naval Research Grant N00014-79-C-0071; NR 083-004.
    Keywords: Ocean currents
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 10
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: When current meters are used to measure mean horizontal currents in surface gravity waves, immunity to the vertical component of flow is important, even though the net vertical flow averages to zero and is normal to the desired horizontal components. A technique is presented for estimating the magnitude of the errors introduced by imperfect rejection of the off-axis flows (cross-talk) from laboratory measurements of the current meter "vertical-cosine-response." The predicted dynamic response is shown to compare favorably with laboratory measurements. The measured steady state vertical-cosine-response functions for several practical current sensors are summarized and used to estimate the magnitude of wave-induced errors in horizontal mean current measurements. A new dye technique for evaluating near-surface current meter performance in waves is shown.
    Description: Prepared for the Working Con6enence on CURRENT MEASUREMENTS sponsored by the NOAA 0ffice of Ocean Engineering with the Delaware Sea Grant College Program.
    Keywords: Water current meters ; Flow meters ; Ocean currents
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 11
    Publication Date: 2022-05-26
    Description: General information about mooring locations, durations and data gathered by the Moored Array Project (also known as Buoy Group) between late 1963 and 1978 is listed. Also included is a comprehensive list of scientific and technical publications written by the Buoy Group staff.
    Description: Prepared for the Office of Naval Research under Contract N00014-76-C-0197; NR 083-400 and for the National Science Foundation under Grant OCE 77-19403 .
    Keywords: Oceanographic buoys ; Ocean currents ; Ocean circulation
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 12
    Publication Date: 2022-05-26
    Description: Also published as: Journal of Marine Research 36 (1978): 725-734
    Description: Relatively energetic low frequency fluctuations in horizontal currents are found to exist below the thermocline in the northern trough of the Charlie-Gibbs Fracture Zone. For example, deep eddy kinetic energy levels there are about twice as large as those observed at similar relative depths in the MODE-I region. Eddy kinetic energies are about 2-10 times larger than mean kinetic energies. The vertical distribution of eddy kinetic energy is frequency dependent, increasing toward the thermocline for the longer time scales and intensifying toward the bottom at higher frequencies. In addition to the expected mean westward motion of Norwegian Sea Overflow Water through the northern trough of the fracture, rather consistent mean southward flow is observed at a depth immediately above the overflow.
    Description: Prepared f or the Office of Naval Research under Contract N00014-76-C-0197; NR 083- 400.
    Keywords: Ocean circulation ; Ocean currents ; Charles Gibbs Fracture Zone
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 13
    Publication Date: 2022-05-26
    Description: This report describes the performance of a freely-falling velocity profiler called the Absolute Velocity Profiler (AVP) . The AVP is distinguishable from our previously developed velocity profiler the Electro-Magnetic Velocity Profiler (EMVP) in that acoustic Doppler measurements are used, to determine the reference velocity for the EMVP profiles. The AVP contains the essential measurements of the motional electric currents in the sea as implemented in the EMVP and in addition, collects acoustic Doppler measurements of frequencyshifted bottom echoes. The former measurements yield a profile of the horizontal components of velocity relative to a reference velocity, independent of depth, while the latter measurements determine the absolute velocity of the AVP vehicle with respect to the sea floor. The EM profile is obtained from the sea surface to bottom, and the acoustic Doppler measurements are made within about 300 m of the sea floor. The combination of the EM and acoustic Doppler measurements yields an absolute velocity profile throughout the water column. Performance analyses included in this report set method uncertainties of between 1 and 2 cm/s r.m.s. Measurements of temperature and its gradient are also made.
    Description: Prepared for the National Science Foundation, Office of the International Decade of Ocean Exploration under Grant OCE76-24605.
    Keywords: Doppler effect ; Electromagnetism ; Ocean currents ; Oceanographic instruments
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 14
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: Also published as Journal of Geophysical Research, 83(C6), 1978, pp. 2921–2938
    Description: As part of a field study of the relation between fine scale and large‐scale variations of water properties in the western North Atlantic, the waters in the vicinity of Bermuda were investigated in detail. Previous work in the area had revealed regions of intense temperature fine structure confined to the sides of the island. Generally quieter levels of activity elsewhere in the midocean have suggested that significant mixing might only occur at the solid and fluid boundaries of the ocean. During the course of our investigation, two Gulf Stream rings were found in the vicinity of the island. The exchange of water between them caused three regions of strong alongshore flow. In these three areas we find elevated levels of temperature fine structure in the upper 800 m as measured by the variance in the temperature gradient normalized by the square of the mean temperature gradient over the interval. The normalized temperature variances on small scales (0.2–1 m) are most energetic in patches tightly bound to the island sides, whereas the fine structure on larger scales (5–25 m) is also energetic away from the island in a region of outflow. Velocity profiles show that vertical scales shorten as one approaches the island, and the energy increases in the counterclockwise component. There is no correlation evident between the shear measurements of the internal wave field and the intensity of the fine structure. Possible mechanisms for the production of fine structure are explored within the context of these observations.
    Description: This research was carried out with funding from the Office of Naval Research under contracts NOOOI4-74-C- 0262 NR083-004 (N .G.H. and T.B.S.) and the National Science Foundation under grant OCE74-19608 (E.J.K.).
    Keywords: Oceanic mixing ; Turbulence ; Ocean currents
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 15
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: This is a report describing activities associated with the Matamek program in 1977. Research was conducted on biological, chemical and physical factors related to salmonid production in Matamek River and Matamek Lake. Canadian universities, the Quebec government and Woods Hole Oceanographic Institution cooperated in the program.
    Description: Supported by Woods Hole Oceanographic Institution and the Department of Tourism, Fish and Game of the Province of Quebec.
    Keywords: Ecology ; Limnology
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 16
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: Leg VI of CHAIN 112 was scheduled from 24 June to 9 July, St. Georges, Bermuda to Woods Hole. The original plans called for the following work: Recovery of sixteen intermediate moorings at the MODE site (28° N., 69° 40'W.) Recovery of three subsurface moorings in the MODE area for the University of Rhode Island. Launching of two new intermediate moorings at the MODE site. Bathymetric and meteorological observations in the MODE area. Bathymetry at Site D. Acoustic checks of three intermediate moorings at Site D. CTDs at each mooring recovery and setting
    Description: Prepared for the Office of Naval Research under Contract N00014-66-C0241; NR 083-004.
    Keywords: Mid-Ocean Dynamics Experiment (MODE) ; Deep-sea moorings ; Ocean currents ; Chain (Ship : 1958-) Cruise CH112
    Repository Name: Woods Hole Open Access Server
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  • 17
    Publication Date: 2022-05-26
    Description: Summaries are presented of basic current, temperature and pressure measurements which were made from moored instruments as a part of the Mid-Ocean Dynamics Experiment (MODE) which took place March to July 1973. Current data are presented as Basic Statistics, Spectral Diagrams , Progressive Vector Diagrams, East vs. North Plots, and Variables vs . Time Plots.
    Description: Prepared for the Office of Naval Research under Contracts N00014-66-C-0241; NR 083-004 and N00014-76-C-0197; NR 083-400.
    Keywords: Deep-sea moorings ; Ocean currents ; Ocean temperature ; Mid-Ocean Dynamics Experiment (MODE)
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 18
    Publication Date: 2022-05-26
    Description: A meeting was held March 11-15, 1980 to develop and refine the hierarchy of problems to be addressed by the high energy benthic boundary layer experiment. This document outlines revised program goals and the critical scientific tasks needed to attain those goals. Also included is an interim "state of the program" report and a critical review by the Advisory Committee.
    Description: Prepared for the Office of Naval Research under Contract N00014-79-C-0071; NR 083-004.
    Keywords: High Energy Benthic Boundary Layer Experiment (HEBBLE) ; Ocean currents
    Repository Name: Woods Hole Open Access Server
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  • 19
    Publication Date: 2022-05-26
    Description: Also published as: Journal of Physical Oceanography (1979) 9: 1294-1297
    Description: It is demonstrated that the outcome of an intercomparison between data and the vertical distribution of eddy kinetic energy predicted by a previously developed numerical model of the MODE area is frequency dependent. In the range of periods from 50 to 150 or even to 400 days (one definition of the temporal mesoscale, the scale that the model was designed to simulate), the comparison is quite good. For periods in the range of 5 to 50 days, the agreement is poor. For periods longer than 400 days , the comparison is indeterminate. Earlier conclusions concerning the relation of model results to the MODE data should be qualified by stipulating frequency range , and future intercomparisons for any model in all regions should be conscious of the desirability of doing so across common frequencies.
    Description: Prepared for the Office of Naval Research under Contract N00014-76-C-0197; NR 083-400 and for the International Decade of Ocean Exploration Office of the National Science Foundation under Grant OCE 75-03962.
    Keywords: Mid-Ocean Dynamics Experiment (MODE) ; Ocean currents ; Eddies
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 20
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: Also published as: Journal of Marine Research 38 (1980): 111-133
    Description: Time-averaged horizontal currents obtained from long-term moored instruments deployed in the western North Atlantic over the Sohm Abyssal Plain along 55W exhibit two segments of weakly depth-dependent flow: one, near 36N, predominantly westward and narrow or jet-like (~ 200 km wide or less); the second primarily eastward, located near 37.5N, about 200-300 km south of the mean position of the axis of the Gulf Stream (its width cannot be estimated quantitatively with the data available because only one mooring with adequate vertical coverage is clearly located in this flow regime, but an upper bound of roughly 200 km seems plausible). In both cases, long-term mean zonal currents between 600 and 4000 m depths (nominal) vary in amplitude from only 6 to 10 cm s-1 (approximately). The vertical structure of the westward recirculation varies with horizontal position, being both surface and bottom intensified. The possibility exists that the identification of these weakly depth-dependent flow regimes may point to one way of increasing the transport of the Gulf Stream. That is, flow with weak vertical shear is added offshore of the more baroclinic segment of the Stream, and possibly recirculated accordingly. This notion is generally consistent with all previous investigations which find the weakest vertical shears at the offshore edge of the Stream, wherever and however examined, and in particular with the addition of transport to the Florida Current over the Blake Plateau, after emerging from the Straits of Florida (Richardson, Schmitz, and Niiler, 1969). The horizontal patterns of the two weakly depth-dependent flow regimes found at 55W may be quite complex, containing variability on comparatively short and intermediate scales, associated to some extent with bottom topography. A specific example of the effect of bottom topography on the 55W data has been presented by Owens and Hogg (1980). It is hypothesized that the observations described here may indicate the presence of a previously unknown, weakly depth-dependent smaller scale gyre recirculating within the subtropical gyre, with the former confined between the New England Seamounts and the Grand Banks of Newfoundland. It should be emphasized that other horizontal and vertical structures may be characteristic of different locations in the recirculation of the North Atlantic. Eddy kinetic energy (Schmitz, 1978) and the off-diagonal component of Reynolds' stress are also to some extent weakly depth-dependent in each of the weakly depth-dependent mean flow regimes noted above, relative to more mid-ocean locations. At one site in particular, the off-diagonal component of the Reynolds' stress is found to be essentially depth-independent. The observation of weak depth-dependence in association with relatively strong abyssal currents for the recirculation regime could in principle help rationalize (Schmitz, 1977; Stommel, Niiler and Anati, 1978; Wunsch, 1978) some of the difficulties in geostrophica\ly balancing (at the leading order of approximation!), according to Worthington (1976), the North Atlantic Circulation in this type of region. Estimates of contributions to momentum balances (based on the available moored instrument data) involving horizontal gradients of the Reynolds' stresses, or of the momentum transport by the time-averaged flow, are typically at least an order of magnitude less than the Coriolis force associated with the zonal (or downstream) mean flow component, and possibly also the meridional (or cross-stream) flow component at most locations, thereby precluding violation of geostrophy at leading order by these effects. Geostrophic terms associated with estimates of the curvature of the Reynolds' stresses and/or mean momentum flux could be significant at the next order of approximation in the immediate vicinity of the Gulf Stream or near topographic features. Niiler (1979) has developed a model of an eddy-driven mean flow, where the eddy-terms in the vorticity equation are locally significant only in the Gulf Stream, but with a basin-wide mid-ocean flow driven in response to the noncompensated eddy-induced pressure gradient at the offshore edge of the region where eddy effects are locally significant dynamically. Two recent hydrographic sections across the Gulf Stream and recirculation along SSW were found to be in mass balance geostrophically, relative to the bottom (McCartney, Worthington and Raymer, 1980).
    Description: Prepared for the Office of Naval Research under Contract N00014-78-C-0197; NR 083-400 and for the Office of the International Decade of Ocean Exploration of the National Science Foundation under Grant OCE 75-03982.
    Keywords: Ocean circulation ; Ocean currents
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  • 21
    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
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  • 22
    Publication Date: 2022-05-26
    Description: The near bottom density and velocity fields above the Hatteras abyssal plain were observed with a current/temperature measuring array and a towed-yo-yoing profiler. This report describes the array data and includes details of calibration and data quality. Sources of direction error were diagnosed from vane and compass performance and bearing direction .
    Description: Prepared for the National Science Foundation under Grant OCE 76-81190 and for the Office of Naval Research under Contract N00014-76-C-0197; NR 083-400.
    Keywords: Ocean currents ; Ocean temperature
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  • 23
    Publication Date: 2022-05-26
    Description: Also published as: Journal of Geophysical Research 85 (1980): 6654-6660
    Description: An early stage of the Somali eddy circulation was mapped in the period May 29 to June 13, 1978, using expendable bathythermograph data at closely spaced stations. By this time the SW monsoon had been blowing at 5°N for about 4 weeks and the large anticyclonic eddy in the northern Somali Basin was clearly discernible between 3°N and 10°N. It is estimated that the offshore transport at this time was approximately half of that occurring during the period when the eddy reaches maximum size and strength during August and September. A smaller southern eddy was observed just offshore between the equator and 3°N.
    Description: Prepared for the Office of Naval Research under Contracts N00014-74-C-0262; NR 083-004 and N00014-79-C-0071; NR 083- 004.
    Keywords: Ocean currents ; Monsoons ; Eddies
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  • 24
    Publication Date: 2022-05-26
    Description: The purpose of this report is to discuss the use of a Neil Brown Instrument Systems internal recording CTD. The components of the instrument are described along with the advantages and disadvantages of the internal recording system. Calibration of the pressure and temperature sensors in the laboratory and the method used for in situ calibration of the conductivity sensor is described. A step by step description of the use of the CTD/IR at sea is also included.
    Description: Prepared for the Office of Naval Research under Contract N00014-76-C-0197; NR 083-400 .
    Keywords: Ocean temperature ; Ocean currents ; Oceanographic instruments
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  • 25
    Publication Date: 2022-05-26
    Description: The report presents summaries of three data sets taken at and in the vicinity of the oceanographic moorings deployed in the 1978 Joint Air-Sea Inte raction Project (JASIN). The data sets are: (1) the temperature, pressure and vertical motion records from the freely drifting Vertical Current Meters (VCMs) deployed from the ATLANTIS II, (2) the temperature data from the Aanderaa thermistor chains on W.H.O.I. mooring 653, designated as JASIN mooring W3, and (3) the expendable bathythermograph (XBT) data collected from the ATLANTIS II while participating in the JASIN Project.
    Description: Prepared for the Office of Naval Research under Contract N00014-76-C-0197; NR 083- 400 and for the National Science Foundation under Grant OCE 77-25803 .
    Keywords: Joint Air-Sea Interaction Project ; Ocean temperature ; Ocean currents ; Ocean-atmosphere interaction ; Deep-sea moorings ; Atlantis II (Ship : 1963-) Cruise AII102
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  • 26
    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
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  • 27
    Publication Date: 2022-05-26
    Description: New laboratory measurements and numeric model studies show the present folded-path ATT current meters are stable and sensitive, but are not well suited for mean flow observations in surface gravity waves. Alternate designs which reduce unwanted wake effects are proposed. ATT flowmeter history, principles of acoustic flow sensors, mean flow near cylinders, and the need for linear flow sensors are reviewed.
    Description: Prepared for the Office of Naval Research under Contract Number N00014-76-C-0197; NR083-400 to the Woods Hole Oceanographic Institution.
    Keywords: Flow meters ; Acoustic velocity meters ; Ocean currents
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  • 28
    Publication Date: 2022-05-26
    Description: In 1978, the first Keystone Conference addressed the scientific problems of sediment transport in a high energy flow such as the Western Boundary Undercurrent. Sedimentologists, physical oceanographers, geologists, optical oceanographers, biologists, and ocean engineers planned a program called the High Energy Benthic Boundary Layer Experiment (HEBBLE) to measure ocean floor bed-forms, sediment properties, turbulent flow structure, suspended sediment concentrations and fluxes, mixed layer thickness, outer scale velocity and horizontal gradients of density in a carefully surveyed site yet to be selected. While measurements were suggested, specific instruments were not identified to implement them. It was encouraging that the scientists participating in the first HEBBLE Conference wanted to continue to plan a multi-disciplinary experiment. Because of the Jet Propulsion Laboratory's experience in management of planetary science experiments, autonomous instrumentation, image processing and data handling, we invited them to develop our experimental plan. Conferences were held in September at Woods Hole and November, 1978 at JPL to develop the instrumental ensemble. JPL involvement was concentrated on the extended deployment part of HEBBLE: the 6-month experiment. The March 20-23, 1979 conference brought JPL engineers and managers, HEBBLE scientists and PI's, ONR and NASA program managers together in Keystone, Colorado for presentation and discussion of the JPL program plan. This report summarizes the conference and includes reports by subcommittees of the conference on measurements and data sampling.
    Description: Prepared for the Office of Naval Research under Contract N00014-74-C-0262; NR 083-004.
    Keywords: High Energy Benthic Boundary Layer Experiment (HEBBLE) ; Sediment transport ; Ocean currents
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  • 29
    Publication Date: 2022-05-26
    Description: Also published as: Journal of Physical Oceanography 9 (1979): 489-517
    Description: A total of four moorings from POLYMODE array I and II were analyzed in an investigation of the interaction of wavefields and mean flow. In particular, evidence for internal wave-mean flow interaction was sought by searching for time correlations between the vertically acting Reynolds stress of the wavefield (estimated using the temperature and velocity records), and the mean shear. No significant stress-shear correlations were found at the less energetic moorings (u¯≲10 cm s−1), indicating that the magnitude of the eddy viscosity was under 200 cm2 s−1, with the sign of the energy transfer uncertain. This is considerably below the O(4500 cm2 s−1) predicted by Müller (1976). An extensive error analysis indicates that the large wave stress predicted by the theory should have been observable clearly under the conditions of measurement. At moorings typified by a higher mean velocity (u¯≈25 cm s−1), statistically significant stress-shear correlations were found, and the wavefield energy level was observed to modulate with the strength of the mean shear. The observations were consistent with generation of short (∼1 km horizontal wavelength) internal waves by the mean shear near the thermocline, resulting in an effective eddy viscosity of ∼100 cm2 s−1. Theoretical computations indicate that the wavefield “basic state” may not be independent of the mean flow as assumed by Müller (1976) but can actually be modified by large-scale vertical shear and still remain in equilibrium. In that case, the wavefield does not exchange momentum with a large-scale vertical shear flow and, excepting critical-layer effects, a small vertical eddy viscosity is to be expected. Using the Garrett-Munk (1975) model internal wave spectrum, estimates were made of the maximum momentum flux (stress) expected to be lost to critical-layer absorption. This stress was found to increase almost linearly with the velocity difference across the shear zone, corresponding to a vertical eddy viscosity of −100 cm2 s−1. Stresses indicative of this effect were not observed in the data.
    Description: Prepared for the Office of Naval Research under Contract N00014-76-C-0197; NR 083-400.
    Keywords: Internal waves ; Ocean currents
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  • 30
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: The W.H.O.I. portion of the MODE I array was to be installed on the first two legs of CHAIN 112, along with other work to be done at Site D. The original schedule called for the ship to leave Woods Hole on the 6th of March and return on the 20th. After a two-day layover in Woods Hole, Leg II was scheduled for 22 March through 2 April, terminating in Bermuda. Objectives of the cruises were: Setting of sixteen intermediate moorings and one surface mooring at the MODE Site (centered at 28° N., 69° 40'W.). Recovery of two MODE-Site maintenance moorings. Recovery of three intermediate moorings in the vicinity of Site D (39° 10'N., 70°00'W.). Setting of three new intermediate moorings at Site D. These were to be set by a faking-box technique, rather than the conventional method. CTDs at each new mooring. Bathymetry and meteorological observations. Gravity section, Woods Hole to MODE area and return
    Description: Prepared for the Office of Naval Research under Contract N00014-66-C0241; NR 083-004.
    Keywords: Mid-Ocean Dynamics Experiment (MODE) ; Deep-sea moorings ; Ocean currents ; Chain (Ship : 1958-) Cruise CH112
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  • 31
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: Ten SOFAR floats were instrumented during the MODE field experiment to record pressure, temperature, and vertical water displacement during a four month drift. This report describes the acquisition and reduction of this data and then summarizes in graphical form some of the principal results.
    Description: Prepared for the National Science Foundation, International Decade of Ocean Exploration Grant GX-30220
    Keywords: Mid-Ocean Dynamics Experiment (MODE) ; Data processing ; Oceanography ; Ocean currents
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  • 32
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: Prepared for the Office of Naval Research under Contract N00014-66-C0241; NR 083-004
    Keywords: Joint US-USSR Mid-Ocean Dynamics Experiment (POLYMODE) ; Ocean currents ; Deep-sea moorings ; Chain (Ship : 1958-) Cruise CH116
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  • 33
    Publication Date: 2022-05-26
    Description: Also published as Journal of Physical Oceanography, Vol. 7, No. 3, May 1977, pp. 329-337
    Description: Estimates of horizontal derivatives of velocity made by differencing velocity measurements are used to show that the observed velocity field due to low-frequency mesoscale motions during the preliminary MidOcean Dynamics Experiment (MODE-0) field program is horizontally nondivergent within estimated errors. The errors in horizontal derivatives of 0.15 X lQ-6 s-1 are too large for direct estimates of horizontal divergence to be made accurately. The vorticity, however, can be estimated from these horizontal derivatives with an error small compared with its magnitude. Over the measurement period of SO days, the advection of planetary vorticity balances only one-half of the local change of vorticity so these observations cannot be explained in terms of barotropic Rossby waves alone. There are indications that vortex stretching, estimated from a linear heat balance, may balance the remaining local change of vorticity as expected for baroclinic Rossby waves. Based on other measurements in this region; however, it is likely that the horizontal advection of relative vorticity is also important in the vorticity balance. A positive, but not significantly different from zero, correlation between estimates of relative vorticity and advection of planetary vorticity suggests that the ens trophy of the observed velocity field is decreasing with time. In conjunction with a similar result for the perturbation potential energy obtained in this region, this result supports the view that the MODE region is a region of decay, rather than growth, of the low-frequency mesoscale motions.
    Description: Prepared for the Office of Naval Research under Contract N00014-66-C-0241; NR 083-004 and for the National Science Foundation, Office of the International Decade of Ocean Exploration under Grant ID0?5-03962.
    Keywords: Ocean currents ; Temperature measurements ; Mid-Ocean Dynamics Experiment (MODE)
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  • 34
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: Originally issued as Reference No. 61-17, series later renamed WHOI-.
    Description: A series of current measurements were made southwest of Plantagenet Bank. Bermuda from October 5-18, 1959, at various depths ranging from 5 fathoms to the bottom in water depths of from 40 to over 1000 fathoms. With the exception of the bottom measurements which were made with a camera type current meter, all the current measurements were made with parachute drogues. The magnitude of the currents ranged from 1 knot at 5 fathoms to less than 0.02 knot just off the bottom and the direction of flow was generally southeast. The somewhat erratic behavior in the movement of the drogues just south of the bank seemed to indicate turbulent flow in this region. The currents do not seem to be tidal in nature, but during the period of measurement flowed fairly consistently in one direction. perhaps indicating association with the Gulf Stream.
    Description: Submitted to the Office of Naval Research Under Contract Nonr-2866(00)
    Keywords: Project Artemis ; Ocean currents
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  • 35
    Publication Date: 2022-05-25
    Description: Laboratory, theoretical and numerical research was conducted into the structure and stability of baroclinic non-linear currents in a rotating fluid. A rotating version of the dam-break problem in which a . density current is generated after a barrier has been removed was studied. The speed of the current and its width and depth were measured by Whitehead (1981) and more extensively by Stern, Whitehead, and Lien Hua (1982), who report the experiments and compare the results to theory. Properties of a limiting bore solution for rotation density currents predicted earlier by Stern are incorporated into the above theory to predict the speed of the nose of the current. Experiments are described in which the current width is measured to be in reasonable agreement with the theory. Theoretical studies of the stability of a free isolated baroclinic jet whose free surface in cross-section intersects the water surface at two points by Griffiths, Killworth and Stern (1982) was undertaken. The waves permit the release of both kinetic and potential energy. They can have rapid growth rates, thee-folding time for waves on a current with zero potential vorticity being close to one-half of a rotation period. Experiments with a current of buoyant fluid at the free surface of a lower layer were also conducted. The current was observed to be always unstable. Killworth and Stern (1982) showed that a coastal density current in a rotating system is unstable to downstream wave disturbances when the mean potential vorticity increases towards the (vertically-walled) coast and when the mean current vanishes there. Other new instability modes were also found which do not require the potential vorticity extremum of quasi-geostrophic theory. Paldor, in his Ph.D. thesis, used Rayleigh integral to prove that an unbounded geostrophic front of uniform potential vorticity is stable with respect to small perturbations of arbitrary wavelength. Stern and Paldor (1983) used extremum concepts to analyze large amplitude disturbances in a boundary layer shear flow with an inviscid and longwave theory. It was found that initially weak horizontal convergences were concentrated and amplified in time.
    Description: Prepared for the Office of Naval Research under Contract N00014-81-C-0010 and for the National Science Foundation, Ocean Science Division under Grant 0CE 80-18322.
    Keywords: Ocean currents ; Hydrodynamics
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  • 36
    Publication Date: 2022-05-25
    Description: The Nantucket Shoals Flux Experiment (NSFE79) was conducted across the continental shelf and upper slope south of Nantucket from March, 1979 to April , 1980 to measure the flow of shelf water from the Georges Bank/Gulf of Maine region into the Middle Atlantic Bight. Conceived as a cooperative field experiment involving the Northeast Fisheries Center (NMFS), U.S. Geological Survey (Woods Hole), University of New Hampshire, and the Woods Hole Oceanographic Institution, the experiment contained two principal components, a moored array of current meter and bottom instrumentation deployed at six locations across the shelf and upper slope spanning a depth range from 46 m to 810 m, and a series of 27 hydrographic surveys made along or near the moored array line during the experiment. A basic description of the NSFE79 hydrographic data has been given in Part 1 by Wright (1983). A description of the moored array components and the basic moored array data sets is presented here in Part 2.
    Description: The NEFC participation was supported by the NMFS Marine Resources Monitoring, Assessment, and Prediction (MARt-1AP) Program. The U.S. Bureau of Land Management (BLM) supported the USGS field and analysis component under t~emoranda of Understanding M550-MU6-79, M551-MU8- 24, M551-MU9-4, and M551-MU0-18. The WHO! and UNH field programs were supported by the National Science Foundation under Grants OCE 78-19513 and OCE 78-26229.
    Keywords: Oceanography ; Hydrography ; Ocean currents ; Moored arrays
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  • 37
    Publication Date: 2022-05-26
    Description: The underway current profiling system used in this study consists of a microprocessor-controlled data logger that collects and formats data from a four-beam Ametek-Straza 300 kHz acoustic Doppler current profiler, heading from the ship's gyrocompass, and navigation information from a Loran-C receiver and a satellite navigation unit. Data are recorded on magnetic tape and some real time calculations are made. The system was first used on a May, 1981 cruise aboard the R.V. OCEANUS in the western North Atlantic. Horizontal currents were profiled to depths of 100m. Time averaging is required to remove effects of ship motion. Errors in our ability to profile ocean currents are estimated to be 5-10 em s-1 for a ten-minute vector average. An intercomparison is made with a moored vector measuring current meter (VMCM). The mean difference in hourly-averaged APOC and VMCM currents over the four-hour intercomparison is a few mm s-1. Data from a variety of oceanic regimes are presented and discussed: these regimes include two Gulf Stream crossings, a warm core ring survey, and shallow water in a frontal zone to the east of Nantucket Shoals.
    Description: Prepared for NASA under Grant NAG 1-91 through NASA-Langley.
    Keywords: Acoustic imaging ; Ocean currents ; Oceanus (Ship : 1975-) Cruise OC96
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  • 38
    Publication Date: 2022-05-26
    Description: The Bedford Institute of Oceanography, E.G.&G., National Marine Fisheries Service, U.S. Geological Survey, and Woods Hole Oceanographic Institution have conducted separate moored array experiments during 1974- 1980 to study various aspects of the regional circulation in the Gulf of Maine and adjacent Scotian and New England shelf and slope regions. The mean currents and current variances measured in these experiments are summarized here in tabular and graphical form, together with other information about each experiment. While there have been few measurements made in the interior of the Gulf of Maine, the map of mean subsurface currents demonstrate (a) a net inflow of Scotian shelf water past Cape Sable into the Gulf, (b) a net inflow of slope water through the Northeast Channel into the Gulf, (c) a partially closed anticyclonic circulation around Georges Bank, and (d) a net outflow of shelf water south of Nantucket from the Gulf of Maine into the New England shelf.
    Description: Funding was provided by the Department of Interior, Bureau of Land Management under Contract AA 551-MU0-18 and by the National Science Foundation under Grant OCE 80-14941.
    Keywords: Ocean currents ; Ocean circulation
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  • 39
    Publication Date: 2022-05-26
    Description: The flow through the Strait of Gibraltar has always held a special fascination for oceanographers. Attempts to understand and measure the strong currents in the Strait stimulated many of the early advances in oceanography (Deacon, 1971). Over the centuries, the focus of scientific investigations has shifted from understanding how the mass budget of the Mediterranean is maintained in the presence of the strong inflow of Atlantic water through the Strait of Gibraltar, to observing the outflow of Mediterranean water over the Gibraltar sill, to measuring the two-layer. exchange of Atlantic inflow and Mediterranean outflow through the Strait. In the past few years the focus has again shifted to the study of how the dynamical constraints for flow through a narrow and shallow strait act to control the amount of exchange between the Atlantic and Mediterranean basins. To investigate the dynamics of flow through a strait, a year-long field experiment has been designed to measure the flows through the Strait of Gibraltar, including their time variability over tidal to seasonal time scales, and to assess the importance of friction, mixing, rotation, and nonlinear processes in controlling the exchange through the Strait. This field program, called the Gibraltar Experiment, will be carried out by a group of American, Spanish, Moroccan, Canadian and French scientists during the period from Fall 1985 to Fall 1986.
    Description: Funding was provided by the Office of Naval Research under contracts no. N00014-82-C-0019, NR 083-004, and N00014-85-C-0001, NR 083-004.
    Keywords: Oceanography ; Oceanic mixing ; Ocean currents
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  • 40
    Publication Date: 2022-05-26
    Description: In October, 1984, the Woods Hole Oceanographic Institution SOFAR float group began a three-year long field program to observe the low frequency currents in the Canary Basin. The principal scientific goal was to learn how advection and diffusion by these currents determine the shape and amplitude of the Mediterranean salt tongue. Fourteen floats were launched at a depth of 1100 min a cluster centered on 32N, 24W, and seven other floats were launched incoherently along a north/south line from 24N to 37N. At the same time investigators from Scripps Institution of Oceanography and the University of Rhode Island used four other SOFAR floats to tag a submesoscale lens of Mediterranean water. Slightly over twenty years of float trajectories were p reduced during the first year of the experiment. In this report we briefly describe the 1984 field operations and show the first year's SOFAR float data. Perhaps the most striking result is that westward flow within the Mediterranean salt tongue was found to be confined to a rather narrow jet {roughly 150 km in meridional extent) which had a mean speed of roughly 2 em s -l. To the north or south of this jet the mean flow was much weaker and eastward. This suggests that currents associated with the salt tongue itself {rather than the gyre scale circulation) may be most important for determining the salt distribution.
    Description: Funding was provided by the National Science Foundation under grant Nos. OCE 82-14066 and OCE 86-00055.
    Keywords: Ocean currents
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  • 41
    Publication Date: 2022-05-26
    Description: The Long-Term Upper Ocean Study (LOTUS) was a two-year field experiment near 34°N, 70°W, designed to acquire a continuous set of measurements of currents and temperatures in the upper, open ocean together with local hydrography, meteorology, and mesoscale oceanographic features. The first scientific moorings were deployed in May 1982. The first year of mooring data, from May 1982-April 1983, is presented by Tarbell, Pennington and Briscoe (1984, W.H.O.I. Tech. Rept. 84-36). The second year of mooring data, from April 1983-May 1984, when the final mooring recovery occurred, is presented here.
    Description: Funding was provided by the Office of Naval Research under contract Nos. N00014-76-C-0197, NR 083-400, and N00014-84-C-0134, NR 083-400.
    Keywords: Long Term Upper Ocean Study (LOTUS) ; Ocean temperature ; Ocean currents ; Ocean-atmosphere interaction ; Deep-sea moorings
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  • 42
    Publication Date: 2022-05-26
    Description: Summaries of current and temperature measurements from three moorings in the 1978 Joint Air-Sea Interaction Project . (JASIN) are presented; the moorings are WHOI/JASIN numbers 651/Wl, 652/W2, and 653/W3. The instruments were either Vector Averaging Current Meters (VACM), Scripps Institution of Oceanography Vector Measuring Current Meters (VMCM) , or Neil Brown Acoustic Current Meters (ACM). Displays include time series, histograms, progressive vector diagrams, scatter plots, and spectra; statistics are given for the entire deployment period (some 40 days) and for each 5-day segment. Additional measurements include pressure and vertical temperature gradient. Wind records and other meteorological observations from one of the moorings are given, as well as partial wind records from another JASIN mooring (H2) .
    Description: Prepared for the Office of Naval Research under Contract N00014-76-C-0197; NR 083-400 to the Woods Hole Oceanographic Institution and Contract N00014-75-C-0152; NR 083-005 to Scripps Institution of Oceanography, and for the National Science Foundation under Grant OCE 77- 25803 .
    Keywords: Deep-sea moorings ; Ocean currents ; Ocean temperature ; Ocean-atmosphere interaction
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 43
    Publication Date: 2022-05-26
    Description: An acoustic Doppler profiler has been designed into a multi-sensor Acoustic Profiler of Ocean Currents system (APOC). All four major components of this data collecting ensemble are microprocessor based units, allowing programmatic flexibility. Various water column, meteorological, and navigation data are recorded in a raw and/or processed form. Plots and listings of processed data are generated and displayed in real-time for use by investigators. Once installed, the system requires only a periodic change of cartridge recording media. The equipment has collected data during five cruises, for a total of approximately 190 days at sea. A hardware and software description of the system is presented. Preliminary technical results are discussed and evaluated.
    Description: Funding was provided by the National Science Foundation under grant Nos. OCE 84-16197 and OCE 84-00128.
    Keywords: Ocean currents ; Acoustic velocity meters
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  • 44
    Publication Date: 2022-05-26
    Description: The OPUS (Organization of Persistent Upwelling Structures) program deployed two current meter (VMCM) moorings near Point Conception, California, during April-July 1983. Current and temperature data from these moorings are summarized here. In addition, data from two nearby NDBC (National Data Buoy Center) meteorological buoys are presented.
    Description: Funding was provided by the National Science Foundation under grants OCE 82-13968 and OCE 80-14942.
    Keywords: Upwelling ; Ocean currents ; Ocean-atmosphere interaction
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  • 45
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: SOFAR float observations from the years 1972 to 1981 have been edited and analyzed to·produce a uniform and error-free data set suitable for archiving. These data were collected from the western North Atlantic during three major experiments directed by H. T. Rossby of the .University of Rhode Island. The data are shown here in plots of the composite and individual trajectories, as time series plots of velocity components, and for the LDE floats, as time series plots of temperature, pressure, vertical velocity, and vertical displacement. These data comprise about 72 years of SOFAR float observations, and are a unique resource for Lagrangian studies of the North Atlantic circulation.
    Description: Funding was provided by the National Science Foundation under Grant Nos. OCE-8109145, OCE-8117467, OCE-8214066, OCE-8600055.
    Keywords: Mid-Ocean Dynamics Experiment (MODE) ; SOFAR Float Pilot Studies (PRE-LDE) ; Local Dynamics Experiment (LDE) ; Ocean currents
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 46
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: The dynamic response of electromagnetic current meters (manufactured by Marsh-McBirney, Inc.) has been clarified through a comprehensive laboratory measurement program combined with a thorough literature review. Elucidation of the behavior of these flowmeters under a variety of dynamic conditions has been neglected in the past. Since flow past a spherical body has considerable hydrodynamic complexity for different dynamic conditions, a careful laboratory study was carried out for pure steady, pure oscillatory (horizontal plane), and combined steady/oscillatory conditions at two test facilities. Test results indicate that flowmeter behavior under pure steady flow is excellent in the absence of high levels of free-stream turbulence, with an r.m.s. error of 1-5 cm/sec. These errors could· be reduced with a higher-order polynomial regression fit. Pure oscillatory response was also excellent, with r.m.s. errors of 1-2 cm/sec, and sensitivity which is correlated with the oscillatory Reynolds number, (Re)o, and the Keulegan-Carpenter number, (A/d). Combined steady/oscillatory flows degraded current meter performance with larger residual errors (1-6 em/sec) and significant differences in sensitivity (up to 20°/o). Horizontal cosine response showed systematic deviations from pure cosine behavior, with a notable inter-cardinal undersensitivity and cosine "shoulder" at lower Reynolds numbers. Error analysis shows these current sensors are adequate for many kinematic measurements, but may lead to excessive errors when using velocity to calculate dynamical quantities (such as bottom friction, Reynolds Stress, or log-layer friction velocities). A careful error analysis must precede any use of these meters for estimating dynamical quantities. These studies pointed out a potential difficulty in using these meters in areas of large ambient turbulence levels (20°/o turbulent intensities), which are characteristic of many near-bottom shallow water environments. Further study is needed to clarify this behavior.
    Description: Prepared for the U.S. Army Corps of Engineers, Coastal Engineering Research Center, Waterways Experiment Station, Vicksburg, MS, under contract DACW/2-82-C-0014; work was initiated with funding from the NOAA National Office of Sea Grant under grant number NA80-AA-D-00077; the Coastal Research Center of the Woods Hole Qceanographic Institution provided support.
    Keywords: Ocean currents ; Water current meters ; Oceanographic instruments
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 47
    Publication Date: 2022-05-26
    Description: Thirty-nine neutrally buoyant SOFAR floats were tracked in the western North Atlantic at depths of 700 m and 2000 m. These floats were launched in an effort to measure the deep current structure of the Gulf Stream and its recirculation near 55°W. Three separate deployments were made in April and October 1980 and July 1981. The floats were tracked by means of moored autonomous listening stations. The basic data consist of float trajectories, and temperature, pressure, and velocity measurements along the trajectories. This report describes the GUSREX experiment and instrument performance. It presents plots illustrating the horizontal structure and scales of the general circulation in the Gulf Stream and its recirculation for the period October 1980 to May 1982.
    Description: Funding was provided by the National Science Foundation under Grant No. OCE 81-09145
    Keywords: Gulf Stream Recirculation Experiment ; Ocean circulation ; Ocean currents
    Repository Name: Woods Hole Open Access Server
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  • 48
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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
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  • 49
    Publication Date: 2022-05-26
    Description: This report presents current and wind data from the first of three surface mooring deployments in the Atlantic North Equatorial Countercurrent near 6°N and 28°W. A Vector Averaging Wind Recorder (VAWR) measured wind velocity, sea surface temperature and air temperature, barometric pressure and solar insolation. Four Vector Measuring Current Meters (VMCM) measured current velocity and temperature at depths of 20, 50, 75 and 150m. The mooring was deployed on February 25 and recovered (and replaced) on September 13, 1983 .
    Description: Funding was provided by the National Science Foundation under grants OCE82-17112 and OCE82-11108.
    Keywords: Deep-sea moorings ; Ocean currents ; Ocean temperature
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  • 50
    Publication Date: 2022-05-26
    Description: This report presents current and wind data from the second of three surface mooring deployments in the Atlantic North Equatorial Countercurrent near 6°N and 28°W. A Vector Averaging Wind Recorder (VAWR) measured wind velocity, sea surface temperature, air temperature, barometric pressure and solar insolation. Four Vector Measuring Current Meters (VMCM) measured current velocity and temperature at depths of 20, 50, 75 and 150 m. The mooring was deployed on September 12,1983 and recovered (and replaced) on March 24,1984.
    Description: Funding was provided by the National Science Foundation under grants OCE82-17112 and OCE82-11108.
    Keywords: Deep-sea moorings ; Ocean currents ; Ocean temperature
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  • 51
    Publication Date: 2022-05-26
    Description: Haidvogel and Keffer (1984) have examined the stirring and mixing of a passive tracer in a turbulent mesoscale eddy field for environmental parameters characteristic of a homogeneous mid-ocean region. This study utilized two numerical models, based respectively on the barotropic vorticity and advective-diffusive equations, to simulate the evolving mid-ocean eddy field and the associated dispersion of an embedded tracer spot. Here, these models are described in detail, and the full suite of tracer release simulations are shown in the form of contour plots.
    Description: Funding was provided by the National Science Foundation under Grant No. OCE81-09486, and the Center for Analysis of Marine Systems (CAMS).
    Keywords: Ocean currents ; Eddies
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  • 52
    Publication Date: 2022-05-26
    Description: Summaries of wind and current measurements made with wind recorders and current meters by the Woods Hole Oceanographic Institution during the year 1968 are presented. Averaged quantities are presented in computer-generated output as basic statistics, spectra diagrams, progressive vector diagrams, and east-north component plots.
    Description: Prepared for the Office of Naval Research under Contract N00014-66-C0262; NR 083-004.
    Keywords: Deep-sea moorings ; Ocean currents ; Ocean temperature ; Ocean-atmosphere interaction ; Crawford (Ship) Cruise 167 ; Atlantis II (Ship : 1963-) Cruise AII46 ; Atlantis II (Ship : 1963-) Cruise AII44 ; Gosnold (Ship : 1962-1973) Cruise 139 ; Chain (Ship : 1958-) Cruise CH86 ; Chain (Ship : 1958-) Cruise CH90 ; Chain (Ship : 1958-) Cruise CH92
    Repository Name: Woods Hole Open Access Server
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  • 53
    Publication Date: 2022-05-26
    Description: Originally issued as Reference No. 71-50, series later renamed WHOI-.
    Description: Summaries of wind and current measurements made with current· meters and wind recorders by the Woods Hole Oceanographic Institution during the year 1966 are presented. Averaged quantities are presented in computer generated output as histograms, basic statistics, spectra, progressive vector diagrams, and east-north component plots.
    Description: Supported by the Office of Naval Research under Contract N00014-66-C0241; NR 083-004.
    Keywords: Deep-sea moorings ; Winds ; Ocean currents ; Atlantis II (Ship : 1963-) Cruise AII18 ; Chain (Ship : 1958-) Cruise CH56B ; Chain (Ship : 1958-) Cruise CH57 ; Crawford (Ship) Cruise 139 ; Crawford (Ship) Cruise 140 ; Crawford (Ship) Cruise 143 ; Atlantis II (Ship : 1963-) Cruise AII25 ; Atlantis II (Ship : 1963-) Cruise AII27 ; Atlantis II (Ship : 1963-) Cruise AII29
    Repository Name: Woods Hole Open Access Server
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  • 54
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: Originally issued as Reference No. 65-44, series later renamed WHOI-.
    Description: Summaries of current measurements made with Richardson current meters at three moored stations in the Western North Atlantic are presented. Averaged quantities are presented in the form of computer-plotted curves.
    Description: Submitted to the Office of Naval Research under Contract Nonr-3351(00)NR 083-501 Nonr-2196(00)NR 083-004.
    Keywords: Ocean currents ; Ocean temperature
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  • 55
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: Originally issued as Reference No. 67-66, series later renamed WHOI-.
    Description: Summaries of current measurements made with Richardson current meters in two regions of the Western North Atlantic are presented. Averaged quantities are presented in the form of computer-plotted curves.
    Description: Submitted to the Office of Naval Research under Contract Nonr-3351(00) NR 083-501 and NR-2196(00) NR 083-004.
    Keywords: Ocean currents ; Ocean temperature
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  • 56
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: Originally issued as Reference No. 66-60, series later renamed WHOI-.
    Description: Summaries of current measurements made with Richardson current meters at a group of moored stations near Bermuda, and at a single station south of Bermuda are presented. Averaged quantities are presented in the form of computer-plotted curves.
    Description: Submitted to the Office of Naval Research under Contract Nonr-3351(00) NR 083-501 Nonr-2196(00) NR 083-004.
    Keywords: Ocean currents ; Ocean temperature
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  • 57
    Publication Date: 2022-05-26
    Description: This report reviews the working principles of the InterOcean S4 electromagnetic current meter and outlines the practical difficulties and engineering solutions to convert these basic principles into a working instrument. Presented are the test procedures and results performed on three production units placing emphasis on the oceanographic users point of view. These tests, performed by the Ocean Structures and Moorings Laboratory, Ocean Engineering Department, Woods Hole Oceanographic Institution (WHOI), include laboratory, dockside, and both surface and subsurface mooring tests. S4s are compared to each other and to other types of current meters in various intercomparison tests. Results of. this evaluation program are next summarized. Also, suggestions for areas of improvement and further developments are made. Finally, recommendations for the acceptance, calibration, and burning in of new instruments conclude the report.
    Description: Office of Naval Research Contract No. N00014-82-c-0019
    Keywords: Ocean currents ; Water current meters ; Oceanographic instruments ; Electromagnetic devices
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  • 58
    Publication Date: 2022-05-26
    Description: LOTUS was a two-year experiment near 34°N, 70°W, designed to acquire and analyse a continuous set of measurements of currents and temperatures in the upper, open ocean together with local hydrography, meteorology, and mesoscale oceanographic features. The first scientific moorings were deployed in May 1982. The first year of mooring data, from May 1982- April 1983, is presented here.
    Description: Funding was provided by the Office of Naval Research under Contracts No. N00014-76-C-0197, NR 083-400 and N00014-84-C-0134, NR 083-400.
    Keywords: Long Term Upper Ocean Study (LOTUS) ; Ocean temperature ; Ocean currents ; Ocean-atmosphere interaction ; Deep-sea moorings
    Repository Name: Woods Hole Open Access Server
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  • 59
    Publication Date: 2022-05-26
    Description: This third and final report presents current and wind data from a three part mooring deployment in the Atlantic North Equatorial Countercurrent near 6°N and 28°W. A Vector Averaging Wind Recorder (VAWR) measured wind velocity, sea surface temperature, air temperature, barometric pressure and solar insolation. Four Vector Measuring Current Meters (VMCM) measured current velocity and temperature at depths of 20, 75, 150, and 300m. The mooring was deployed on March 26, 1984 and recovered on October 12, 1984.
    Description: Funding was provided by the National Science Foundation under grants OCE 82-17112 and OCE 82-11108.
    Keywords: Deep-sea moorings ; Ocean currents ; Ocean temperature
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  • 60
    Publication Date: 2022-05-26
    Description: Thirty freely drifting drogued surface buoys were tracked by satellite in the vicinity of the Atlantic North Equatorial Countercurrent from February 1983 to February 1985 as part of the SEQUAL (Seasonal Equatorial Atlantic) Experiment. Buoys were launched at several different times of the year in order to sample the Countercurrent in different seasons. The purpose was to measure the seasonal variation of the Countercurrent in relation to wind forcing. The basic data set consists of buoy trajectories, and sea surface temperature, velocity, and wind speed along the trajectories. A comparison is made between the data from the buoys and from a current meter mooring near 6N, 28W. The main results presented here consist of the collection of figures which show trajectories and time series data along the Countercurrent, and in the North and South Equatorial Currents, Guinea Current and North Brazil Current.
    Description: Fulnding was provided by the National Science Foundation under grant Number OCE 82-08744.
    Keywords: Oceanography ; Ocean currents ; Oceanographic buoys
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  • 61
    Publication Date: 2022-05-25
    Description: During the period October 1985 to October 1986 a large group of oceanographers collaborated in an intensive field effort called the Gibraltar Experiment. Scientists from Morocco, Spain, France, the United Kingdom, Canada and the United States joined together to obtain an extensive suite of measurements which greatly enlarged the oceanographic data base for the Strait of Gibraltar. Primary experiment goals included obtaining one realization of the annual flow cycle, understanding the dynamical balances of the strait flow, developing strategies for long-term monitoring of the Strait, and increasing knowledge of strait effects on the adjacent ocean. Preliminary results show progress toward each of these four goals.
    Description: Funding was provided by the Office of Naval Research through contract Numbers N00014-82-C-0019, N00014-85-C-0001, and N00014-87-K-0007.
    Keywords: Oceanography ; Ocean currents ; Oceanus (Ship : 1975-) Cruise ; Malaspina (Ship) Cruise ; Lynch (Ship) Cruise ; Tofino (Ship) Cruise
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    Type: Technical Report
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  • 62
    Publication Date: 2022-05-26
    Description: In October, 1984, the Woods Hole Oceanographic Institution SOFAR float group began a three-year-long field program to observe the low frequency currents in the Canary Basin. The principal scientific goal was to learn how advection and diffusion by these currents determine the shape and amplitude of the Mediterranean salt tongue. Fourteen floats were launched at a depth of 1100 min a cluster centered on 32°N, 24°W, and seven other floats were launched incoherently along a north/south line from 24°N to 37°N. At the same time investigators from Scripps Institution of Oceanography and the University of Rhode Island used four other SOFAR floats to tag a Meddy, a submesoscale lens of Mediterranean water. In October, 1985, seven additional floats were launched, four in three different Meddies, one of which was tracked during year 1. This report describes the second year of the floats launched in 1984 and the first year of the ones launched in 1985. Approximately 41 years of float trajectories were produced during the first two years of the experiment. One of the striking accomplishments is the successful tracking of one Meddy over two full years plus the tracking of two other Meddies during the second year.
    Description: Funding was provided by the National Science Foundation under grant Numbers OCE 82-14066 and OCE 86-00055.
    Keywords: Ocean currents
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  • 63
    Publication Date: 2022-05-26
    Description: The Sea Duct Ocean-Bottom Laboratory is a computer controlled recirculating inverted flume for the in-situ study of sediment transport. It is designed to measure the sea floor response to controlled currents analogous to those generated by surface waves, tidal, or deep ocean storms. The external support frame is an equilateral triangle with sixteen foot sides. It is 12 feet high, has an air weight of 12,500 lbs., and a 2800 lb. submerged weight. Three lead acid battery packs located at the vertex of the triangle legs provide power for the recirculating water pumps, hydraulic power, and ancillary equipment. The inner rotatable structure consists of a 4 foot long by 2 foot wide open bottom windowed test section that is 9 inches high. It is connected to 30 feet of 8 inch tube configured as an elongated toroid. Above the test section is a traverse carriage with stereo camera, flash, and a laser Doppler velocimeter to measure fluid stresses. Internal flow velocities are controlled and can be ramped up to approximately 2 ft/sec providing shear stress sufficient to scour sand, silts, and fine clays. Water and sediment sampling devices obtain specimens from inside and outside the test section. This report consists of three sections. The first subdivision discusses the electro-mechanical systems and deployment- recovery techniques, while the second portion covers the microprocessor controller and its support equipment. The third section contains the appendices, which consists of program listings, schematics, system and deployment check-list, etc.
    Description: Office of Naval Research, Environmental Sciences Directorate, under Contracts N00014-85-C-0001 and N00014-87-K-007
    Keywords: Marine sediments ; Sediment transport ; Ocean bottom ; Ocean currents ; Data processing
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    Type: Technical Report
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  • 64
    Publication Date: 2022-05-26
    Description: Nordic Seas sedimentation data file, v. 2
    Description: Records from ten Aanderaa current meters deployed along with 5 current meter/sediment trap mooring arrays in the Fram Strait and Greenland Basin, each deployed for approximately one year between 1983 and 1986, are presented in this data file. Data included are current vectors, temperatures, frequency spectra, and two- and three-dimensional vector diagrams.
    Description: Funding was provided by the Office of Naval Research under Grant Number N00014-85-C-0001.
    Keywords: Ocean currents
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  • 65
    Publication Date: 2022-05-26
    Description: Data are shown from a two-year current meter mooring in the Canary Basin near 32°N, 24°W. Current meters were located at depths of 470 m, 970 m, 1070 m and 2970 m during the period October 19, 1984 to October 4, 1986. The mooring deployment is part of an 1984-1988 experiment to measure features of advection and diffusion of Mediterranean outflow water with neutrally buoyant SOFAR floats.
    Description: Funding provided by the National Science Foundation under grant Nos. OCE 82-14066 and OCE 86-00055
    Keywords: Ocean currents ; Moored arrays
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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