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  • Inorganic Chemistry  (3,890)
  • Oceanography
  • Biology
  • LUNAR AND PLANETARY EXPLORATION
  • 2005-2009  (358)
  • 1930-1934
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  • 1
    Publication Date: 2021-05-19
    Description: During april 1995 hydrochemical research in a vertical column on the east side of the Galápagos Islands (Cruise T95/04/01) onboard of the INP R/V Tohallí indicated that concentrations of ammonium, nitrate, phosphate and chlorophyll-a were found stratified from the surface to deeper layers, on the other hand the maximum levels of nitrite and silicate were detected 70 m below the thermocline. The apparent oxygen use (AOU) varied from 1 to over 3 below the thermocline, this would indicate an oxidating environment due to the high levels of nitrate, phosphate, silicate and low concentrations of dissolved Oxygen (ca. 90-134[µM]) and ammonium (〈0,1[µM]). According to the high salinity average (35,0 ups), nutritive elements (nitrate 15,6 [µM], silicate 13,1 [µM]), phosphate 1,3 [µM]) and low average of chlorophyll-a 0,15 mg.m³, and in addition the general gradient of these parameters would suggest the presence of an upwelling event, whose nucleus presented low biological activity.
    Description: Published
    Keywords: Chemical composition ; Oceanography ; Chemical composition ; Oceanography ; Upwelling ; Oceanic islands
    Repository Name: AquaDocs
    Type: Journal Contribution
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  • 2
    Publication Date: 2021-05-19
    Description: L’étude porte sur l’évolution du pH et de la température au cours de la transformation artisanale du Cymbium, ainsi que sur les perspectives de valorisation du produit transformé. Les expérimentations menées au site de transformation artisanale de Joal ont permis de constater que : Après 12 heures de séjour en bac (1ère nuit), le Cymbium est encore en phase de rigor mortis. Le pH moyen affiché à l’issue de cette première nuit est de 7,6 ; donc proche de celui du mollusque vivant ; Le pH moyen du produit fini est légèrement acide et se situe entre 6,3 et 6,4. Donc le yeet de Joal est très peu fermenté ; Les difficultés de séchage notées sont dues : soit au manque de maîtrise des paramètres tels que, la température, l’humidité relative et la vitesse de l’air, soit à l’absence de protection du produit en cours de séchage contre les intempéries. Les essais sur les perspectives de valorisation montrent que : 47,64% du poids du Cymbium dépourvu de sa coquille font l’objet de rejets sous forme de rebuts (surtout en milieu industriel) ; Les enzymes végétales que sont, la bromélaïne, contenue dans le jus d’ananas, et la papaïne, contenue dans le latex de papaye, ainsi que les acides organiques contenus dans le vinaigre et le jus de citron, favorisent l’acidification et accélèrent la fermentation, tout en améliorant le goût, l’odeur et la texture du produit fini ; Les meilleurs résultats sont obtenus dans le cas de la fermentation sous température contrôlée, au laboratoire, où le pH du produit fini se situe entre 4,3 et 4,7. Enfin, sur l’ensemble de l’étude, il est prouvé que les rendements obtenus pour les produits ayant subi un processus de transformation complète (dans le cas des essais sur les perspectives de valorisation) sont faibles par rapport à ceux transformés à Joal. Ces rendements vont de : 2,88 à 28,57% pour le premier groupe de produits ct 31,4 à 58,3% pour le second groupe de produits.
    Description: Université Cheikh Anta Diop, Institut Universitaire de Pêche et d'Aquaculture, Dakar (Senegal)
    Description: Unpublished
    Description: cymbium; transformation artisanale; biologie; commercialisation; fermentation; séchage; température; pH; statistiques
    Keywords: pH ; Marketing ; Biology ; Fermentation ; Drying ; Temperature ; Processing fishery products ; Fermentation ; Biology ; Marketing ; Drying ; Temperature ; Statistics
    Repository Name: AquaDocs
    Type: Theses and Dissertations , Bachelor thesis
    Format: 132
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  • 3
    Publication Date: 2022-05-25
    Description: The Ocean Reference Station at 20°S, 85°W under the stratus clouds west of northern Chile is being maintained to provide ongoing climate-quality records of surface meteorology; air-sea fluxes of heat, freshwater, and momentum; and of upper ocean temperature, salinity, and velocity variability. The Stratus Ocean Reference Station (ORS Stratus) is supported by the National Oceanic and Atmospheric Administration’s (NOAA) Climate Observation Program. It is recovered and redeployed annually, with cruises that have come between October and December. During the 2008 cruise on the NOAA ship Ronald H. Brown to the ORS Stratus site, the primary activities were recovery of the Stratus 8 WHOI surface mooring that had been deployed in October 2007, deployment of a new (Stratus 9) WHOI surface mooring at that site; in-situ calibration of the buoy meteorological sensors by comparison with instrumentation put on board by staff of the NOAA Earth System Research Laboratory (ESRL); and observations of the stratus clouds and lower atmosphere by NOAA ESRL. A buoy for the Pacific tsunami warning system was also serviced in collaboration with the Hydrographic and Oceanographic Service of the Chilean Navy (SHOA). The DART (Deep-Ocean Assessment and Reporting of Tsunami) carries IMET sensors and subsurface oceanographic instruments. A DART II buoy was deployed north of the STRATUS buoy, by personnel from the National Data Buoy Center (NDBC) Argo floats and drifters were launched, and CTD casts carried out during the cruise. The ORS Stratus buoys are equipped with two Improved Meteorological (IMET) systems, which provide surface wind speed and direction, air temperature, relative humidity, barometric pressure, incoming shortwave radiation, incoming longwave radiation, precipitation rate, and sea surface temperature. Additionally, the Stratus 8 buoy received a partial CO2 detector from the Pacific Marine Environmental Laboratory (PMEL). IMET data are made available in near real time using satellite telemetry. The mooring line carries instruments to measure ocean salinity, temperature, and currents. The ESRL instrumentation used during the 2008 cruise included cloud radar, radiosonde balloons, and sensors for mean and turbulent surface meteorology. Finally, the cruise hosted a teacher participating in NOAA’s Teacher at Sea Program.
    Description: Funding was provided by the National Oceanic and Atmospheric Administration under Grant No. NA17RJ1223 for the Cooperative Institute for Climate and Ocean Research (CICOR).
    Keywords: Ronald H. Brown (Ship) Cruise RB08-06 ; Marine meteorology ; Oceanography
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 4
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    Massachusetts Institute of Technology and Woods Hole Oceanographic Institution
    Publication Date: 2022-05-25
    Description: Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution February 2009.
    Description: This thesis examines the nature of eddy-mean flow interactions in western boundary current jets and recirculation gyre dynamics from both theoretical and observational perspectives. It includes theoretical studies of eddy-mean flow interactions in idealized configurations relevant to western boundary current jet systems, namely (i) a study of the mechanism by which eddies generated from a localized forcing drive mean recirculation gyres through the process of nonlinear rectification; and (ii) a study of the role of eddies in the downstream evolution of a baroclinic jet subject to mixed instabilities. It also includes an observational analysis to characterize eddy-mean flow interactions in the Kuroshio Extension using data from the downstream location of maximum eddy kinetic energy in the jet. New insights are presented into a rectification mechanism by which eddies drive the recirculation gyres observed in western boundary current systems. Via this mechanism, eddies drive the recirculations by an up-gradient eddy potential vorticity flux inside a localized region of eddy activity. The effectiveness of the process depends on the properties of the energy radiation from the region, which in turn depends on the population of waves excited. In the zonally-evolving western boundary current jet, eddies also act to stabilize the unstable jet through down-gradient potential vorticity fluxes. In this configuration, the role of eddies depends critically on their downstream location relative to where the unstable time-mean jet first becomes stabilized by the eddy activity. The zonal advection of eddy activity from upstream of this location is fundamental to the mechanism permitting the eddies to drive the mean flows. Observational results are presented that provide the first clear evidence of a northern recirculation gyre in the Kuroshio Extension, as well as support for the hypothesis that the recirculations are, at least partially, eddy-driven. Support for the idealized studies’ relevance to the oceanic regime is provided both by indications that various model simplifications are appropriate to the observed system, as well as by demonstrated consistencies between model predictions and observational results in the downstream development of time-mean and eddy properties.
    Description: Funding was for this research and my education was provided by the MIT Presidential Fellowship and NSF grants OCE-0220161 and OCE-0825550. The financial assistance of the Houghton Fund, the MIT Student Assistance Fund, and WHOI Academic Programs is also gratefully acknowledged.
    Keywords: Ocean currents ; Oceanography
    Repository Name: Woods Hole Open Access Server
    Type: Thesis
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  • 5
    Publication Date: 2021-05-19
    Description: The document provides information on the activity of the WDC Oceanography (RIHMI-WDC, Obninsk) during the intersessional 2006-2008 period. The issues of data and metadata management, long-term archival and user services are presented in brief. The first actions to meet the requirements of ICSU on transition of World Data Centres to the World Data System also are considered.
    Description: Supported by IOC/IODE
    Description: Document available in English.
    Keywords: Data ; Oceanography ; Data ; Oceanography
    Repository Name: AquaDocs
    Format: 6
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  • 6
    Publication Date: 2022-05-26
    Description: The emphasis in this year's GFD program has been somewhat different from the past. We have tried to expose a theoretically oriented audience to the new body of observations pertaining to the Arctic and Antarctic circulation. We have, however, not departed from our traditional goal of encouraging broad based inquiries into the field of Geophysical Fluid Dynamics. We would like to believe that the breadth of interest and enthusiasm exhibited in these reports will stimulate future work in Polar Oceanography and Fluid Dynamics.
    Description: Office of Naval Research under Contract N00014-79-C-0671
    Keywords: Ocean circulation ; Oceanography
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 7
    Publication Date: 2009-01-20
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Seibel, Brad A -- Dierssen, Heidi M -- New York, N.Y. -- Science. 2009 Jan 16;323(5912):343-4. doi: 10.1126/science.1161618.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Biological Sciences, University of Rhode Island, Kingston, RI 02891, USA. seibel@uri.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/19150831" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Biomass ; Calcium Carbonate/*chemistry/*metabolism ; Carbon/chemistry ; Ecosystem ; Fishes/*metabolism ; Food Chain ; Hydrogen-Ion Concentration ; Intestines/chemistry/*metabolism ; Oceanography ; Oceans and Seas ; Phytoplankton/growth & development/metabolism ; Seawater/*chemistry
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 8
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    American Association for the Advancement of Science (AAAS)
    Publication Date: 2009-11-07
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Vogel, Gretchen -- New York, N.Y. -- Science. 2009 Nov 6;326(5954):788-91. doi: 10.1126/science.326_788.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/19892956" target="_blank"〉PubMed〈/a〉
    Keywords: *Academies and Institutes/economics/organization & administration ; Anthropology ; Biology ; Chemistry ; Germany ; Germany, East ; Physics ; Research Personnel ; Universities
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 9
    Publication Date: 2018-06-06
    Description: Combinations of sea ice freeboard and snow depth measurements from satellite data have the potential to provide a means to derive global sea ice thickness values. However, large differences in spatial coverage and resolution between the measurements lead to uncertainties when combining the data. High resolution airborne laser altimeter retrievals of snow-ice freeboard and passive microwave retrievals of snow depth taken in March 2006 provide insight into the spatial variability of these quantities as well as optimal methods for combining high resolution satellite altimeter measurements with low resolution snow depth data. The aircraft measurements show a relationship between freeboard and snow depth for thin ice allowing the development of a method for estimating sea ice thickness from satellite laser altimetry data at their full spatial resolution. This method is used to estimate snow and ice thicknesses for the Arctic basin through the combination of freeboard data from ICESat, snow depth data over first-year ice from AMSR-E, and snow depth over multiyear ice from climatological data. Due to the non-linear dependence of heat flux on ice thickness, the impact on heat flux calculations when maintaining the full resolution of the ICESat data for ice thickness estimates is explored for typical winter conditions. Calculations of the basin-wide mean heat flux and ice growth rate using snow and ice thickness values at the 70 m spatial resolution of ICESat are found to be approximately one-third higher than those calculated from 25 km mean ice thickness values.
    Keywords: Oceanography
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  • 10
    Publication Date: 2018-06-06
    Description: Ocean phytoplankton, detrital material, and water absorb and scatter light spectrally. The Ocean- Atmosphere Spectral Irradiance Model (OASIM) is intended to provide surface irradiance over the oceans with sufficient spectral resolution to support ocean ecology, biogeochemistry, and heat exchange investigations, and of sufficient duration to support inter-annual and decadal investigations. OASIM total surface irradiance (integrated 200 nm to 4 microns) was compared to in situ data and three publicly available global data products at monthly 1-degree resolution. OASIM spectrally-integrated surface irradiance had root mean square (RMS) difference= 20.1 W/sq m (about 11%), bias=1.6 W/sq m (about 0.8%), regression slope= 1.01 and correlation coefficient= 0.89, when compared to 2322 in situ observations. OASIM had the lowest bias of any of the global data products evaluated (ISCCP-FD, NCEP, and ISLSCP 11), and the best slope (nearest to unity). It had the second best RMS, and the third best correlation coefficient. OASIM total surface irradiance compared well with ISCCP-FD (RMS= 20.7 W/sq m; bias=-11.4 W/sq m, r=0.98) and ISLSCP II (RMS =25.2 W/sq m; bias= -13.8 W/sq m; r=0.97), but less well with NCEP (RMS =43.0 W/sq m ;bias=-22.6 W/sq m; x=0.91). Comparisons of OASIM photosynthetically available radiation (PAR) with PAR derived from SeaWiFS showed low bias (-1.8 mol photons /sq m/d, or about 5%), RMS (4.25 mol photons /sq m/d ' or about 12%), near unity slope (1.03) and high correlation coefficient (0.97). Coupled with previous estimates of clear sky spectral irradiance in OASIM (6.6% RMS at 1 nm resolution), these results suggest that OASIM provides reasonable estimates of surface broadband and spectral irradiance in the oceans, and can support studies on ocean ecosystems, carbon cycling, and heat exchange.
    Keywords: Oceanography
    Type: Journal of Marine Systems (ISSN 0924-7963); Volume 76; 49-63
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  • 11
    Publication Date: 2018-06-06
    Description: A state-of-the-art numerical model is used to investigate the possibility of determining freshwater flux fields from temporal changes io sea-surface salinity (SSS), a goal of the satellite salinity-measuring mission, Aquarius/SAC-D. Because the estimated advective temporal scale is usually longer than the Aquarius/SAC-D revisit time, the possibility of producing freshwater flux estimates from temporal salinity changes is first examined by using a correlation analysis. For the mean seasonal cycle, the patterns of the correlations between the freshwater fluxes and surface salinity temporal tendencies are mainly zonally oriented, and are highest where the local precipitation is also relatively high. Nonseasonal (deviations from the monthly mean) correlations are highest along mid-latitude moon tracks and are relatively small in the tropics. The complex correlation patterns presented here suggest that a global retrieval of the difference between evaporation and precipitation (E-P) from salinity changes requires more complex techniques than a simple consideration of local balance with surface forcing.
    Keywords: Oceanography
    Type: International Journal of Remote Sensing (ISSN 0143-1161); Volume 30; No. 14; 3745-3767
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  • 12
    Publication Date: 2018-06-06
    Description: Retrieval of water vapor mixing ratio using the Howard University Raman Lidar is presented with emphasis on three aspects: i) performance of the lidar against collocated radiosondes and Raman lidar, ii) investigation of the atmospheric state variables when poor agreement between lidar and radiosondes values occurred and iii) a comparison with satellite-based measurements. The measurements were acquired during the Water Vapor Validation Experiment Sondes/Satellites 2006 field campaign. Ensemble averaging of water vapor mixing ratio data from ten night-time comparisons with Vaisala RS92 radiosondes shows on average an agreement within 10 % up to approx. 8 km. A similar analysis of lidar-to-lidar data of over 700 profiles revealed an agreement to within 20 % over the first 7 km (10 % below 4 km). A grid analysis, defined in the temperature - relative humidity space, was developed to characterize the lidar - radiosonde agreement and quantitatively localizes regions of strong and weak correlations as a function of altitude, temperature or relative humidity. Three main regions of weak correlation emerge: i) regions of low relative humidity and low temperature, ii) moderate relative humidity at low temperatures and iii) low relative humidity at moderate temperatures. Comparison of Atmospheric InfraRed Sounder and Tropospheric Emission Sounder satellites retrievals of moisture with that of Howard University Raman Lidar showed a general agreement in the trend but the formers miss a lot of the details in atmospheric structure due to their low resolution. A relative difference of about 20 % is usually found between lidar and satellites measurements.
    Keywords: Oceanography
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  • 13
    Publication Date: 2018-06-06
    Description: A new empirical approach is developed for ocean color remote sensing. Called the Empirical Satellite Radiance-In situ Data (ESRID) algorithm, the approach uses relationships between satellite water-leaving radiances and in situ data after full processing, i.e., at Level-3, to improve estimates of surface variables while relaxing requirements on post-launch radiometric re-calibration. The approach is evaluated using SeaWiFS chlorophyll, which is the longest time series of the most widely used ocean color geophysical product. The results suggest that ESRID 1) drastically reduces the bias of ocean chlorophyll, most impressively in coastal regions, 2) modestly improves the uncertainty, and 3) reduces the sensitivity of global annual median chlorophyll to changes in radiometric re-calibration. Simulated calibration errors of 1% or less produce small changes in global median chlorophyll (less than 2.7%). In contrast, the standard NASA algorithm set is highly sensitive to radiometric calibration: similar 1% calibration errors produce changes in global median chlorophyll up to nearly 25%. We show that 0.1% radiometric calibration error (about 1% in water-leaving radiance) is needed to prevent radiometric calibration errors from changing global annual median chlorophyll more than the maximum interannual variability observed in the SeaWiFS 9-year record (+/- 3%), using the standard method. This is much more stringent than the goal for SeaWiFS of 5% uncertainty for water leaving radiance. The results suggest ocean color programs might consider less emphasis of expensive efforts to improve post-launch radiometric re-calibration in favor of increased efforts to characterize in situ observations of ocean surface geophysical products. Although the results here are focused on chlorophyll, in principle the approach described by ESRID can be applied to any surface variable potentially observable by visible remote sensing.
    Keywords: Oceanography
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  • 14
    Publication Date: 2018-06-06
    Description: Ocean assimilation systems synthesize diverse in situ and satellite data streams into four-dimensional state estimates by combining the various observations with the model. Assimilation is particularly important for the ocean where subsurface observations, even today, are sparse and intermittent compared with the scales needed to represent ocean variability and where satellites only sense the surface. Developments in assimilation and in the observing system have advanced our understanding and prediction of ocean variations at mesoscale and climate scales. Use of these systems for assessing the observing system helps identify the strengths of each observation type. Results indicate that the ocean remains under-sampled and that further improvements in the observing system are needed. Prospects for future advances lie in improved models and better estimates of error statistics for both models and observations. Future developments will be increasingly towards consistent analyses across components of the Earth system. However, even today ocean synthesis and assimilation systems are providing products that are useful for many applications and should be considered an integral part of the global ocean observing and information system.
    Keywords: Oceanography
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  • 15
    Publication Date: 2019-07-19
    Description: Satellites have provided us with a remarkable ability to monitor many aspects of the globe day-in and day-out and sea ice is one of numerous variables that by now have quite substantial satellite records. Passive-microwave data have been particularly valuable in sea ice monitoring, with a record that extends back to August 1987 on daily basis (for most of the period), to November 1970 on a less complete basis (again for most of the period), and to December 1972 on a less complete basis. For the period since November 1970, Ross Sea sea ice imagery is available at spatial resolution of approximately 25 km. This allows good depictions of the seasonal advance and retreat of the ice cover each year, along with its marked interannual variability. The Ross Sea ice extent typically reaches a minimum of approximately 0.7 x 10(exp 6) square kilometers in February, rising to a maximum of approximately 4.0 x 10(exp 6) square kilometers in September, with much variability among years for both those numbers. The Ross Sea images show clearly the day-by-day activity greatly from year to year. Animations of the data help to highlight the dynamic nature of the Ross Sea ice cover. The satellite data also allow calculation of trends in the ice cover over the period of the satellite record. Using linear least-squares fits, the Ross Sea ice extent increased at an average rate of 12,600 plus or minus 1,800 square kilometers per year between November 1978 and December 2007, with every month exhibiting increased ice extent and the rates of increase ranging from a low of 7,500 plus or minus 5,000 square kilometers per year for the February ice extents to a high of 20,300 plus or minus 6,100 kilometers per year for the October ice extents. On a yearly average basis, for 1979-2007 the Ross Sea ice extent increased at a rate of 4.8 plus or minus 1.6 % per decade. Placing the Ross Sea in the context of the Southern Ocean as a whole, over the November 1978-December 2007 period the Ross Sea had the highest rate of increase in sea ice coverage of any of five standard divisions of the Southern Ocean, although the Weddell Sea, Indian Ocean, and Western Pacific Ocean all also had sea ice increases, while only the Bellingshausen/Smundsen Seas experienced overall sea ice decreases. Overall, the Southern Ocean sea ice cover increased at an average rate of 10,800 plus or minus 2,500 square kilometers per year between November 1978 and December 2007, with every month showing positive values although with some of these values not being statistically significant. The sea ice increase since November 1978 was preceded by a sharp decrease in Southern Ocean ice coverage in the 1970's and is in marked contrast to the decrease in Arctic sea ice coverage that has occurred both in the period since November 1978 and since earlier in the 1970's. On a yearly average bases, for 1979-2007 the Southern Ocean sea ice extent increased at a rate of 1.0 plus or minus 0.4% per decade, whereas the Arctic ice extent decreased at the much greater rate of 4.0 plus or minus 0.4 percent per decade (closer to the % per decade rate of increase in the Ross Sea). Considerable research is ongoing to explain the differences.
    Keywords: Oceanography
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  • 16
    Publication Date: 2019-07-12
    Description: Continental shelves are believed to play a major role in carbon cycling due to their high productivity. Particulate organic carbon (POC) burial has been included in models as a carbon sink, but we show here that seasonally produced dissolved organic carbon (DOC) on the shelf can be exported to the open ocean by horizontal transport at similar rates (1-2 mol C/sq m/yr) in the southern U.S. Mid-Atlantic Bight (MAB). The dissolved organic matter (DOM) model imbedded in a coupled circulation-biogeochemical model reveals a double dynamics: the progressive release of dissolved organic nitrogen (DON) in the upper layer during summer increases the regenerated primary production by 30 to 300%, which, in turns ; enhances the DOC production mainly from phytoplankton exudation in the upper layer and solubilization of particulate organic matter (POM) deeper in the water column. This analysis suggests that DOM is a key element for better representing the ecosystem functioning and organic fluxes in models because DOM (1) is a major organic pool directly related to primary production, (2) decouples partially the carbon and nitrogen cycles (through carbon excess uptake, POM solubilization and DOM mineralization) and (3) is intimately linked to the residence time of water masses for its distribution and export.
    Keywords: Oceanography
    Type: NASA/TM-2009-214177 , 200900837
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  • 17
    Publication Date: 2019-07-12
    Description: A very strong and persistent phytoplankton bloom was observed by ocean color satellites during September - December 2003 along the northern Patagonian shelf. The 2003 bloom had the highest extent and chlorophyll a (Chl-a) concentrations of the entire Sea-viewing Wide Field-of-view Sensor (SeaWiFS) period (1997 to present). SeaWiFS-derived Chl-a exceeded 20 mg/cu m in November at the bloom center. The bloom was most extensive in December when it spanned more than 300 km across the shelf and nearly 900 km north-south (35degS to 43degS). The northward reach and the deep penetration on the shelf of the 2003 bloom were quite anomalous when compared with other years, which showed the bloom more confined to the Patagonian shelf break (PSB). The PSB bloom is a conspicuous austral spring-summer feature detected by ocean color satellites and its timing can be explained using the Sverdrup critical depth theory. Based on high-resolution numerical simulations, in situ and remote sensing data, we provide some suggestions for the probable mechanisms responsible for that large interannual change of biomass as seen by ocean color satellites. Potential sources of macro and micro (e.g., Fe) nutrients that sustain the high phytoplankton productivity of the Patagonian shelf waters are identified, and the most likely physical processes that maintain the nutrient balance in the region are discussed.
    Keywords: Oceanography
    Type: NASA/TM-2009-214176 , 200900836
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  • 18
    Publication Date: 2019-07-12
    Description: HICO and RAIDS Experiment Payload - Hyperspectral Imager For The Coastal Ocean (HREP-HICO) will operate a visible and near-infrared (VNIR) Maritime Hyperspectral Imaging (MHSI) system, to detect, identify and quantify coastal geophysical features from the International Space Station.
    Keywords: Oceanography
    Type: JSC-17962-18
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  • 19
    Publication Date: 2019-07-19
    Description: After the successful Coastal Zone Color Scanner (CZCS, 1978-1986), demonstration that quantitative estimations of geophysical variables such as chlorophyll a and diffuse attenuation coefficient could be derived from top of the atmosphere radiances, a number of international missions with ocean color capabilities were launched beginning in the late 1990s. Most notable were those with global data acquisition capabilities, i.e., the Ocean Color and Temperature Sensor (OCTS 1996-1997), the Sea-viewing Wide Field-of-view Sensor (SeaWiFS, United States, 1997-present), two Moderate Resolution Imaging Spectroradiometers, (MODIS, United States, Terra/2000-present and Aqua/2002-present), the Global Imager (GLI, Japan, 2002-2003), and the Medium Resolution Imaging Spectrometer (MERIS, European Space Agency, 2002-present). These missions have provided data of exceptional quality and continuity, allowing for scientific inquiries into a wide variety of marine research topics not possible with the CZCS. This review focuses on the scientific advances made over the past decade using these data sets.
    Keywords: Oceanography
    Type: Annual Review of Marine Science (ISSN 1941-1405); 1; 19
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  • 20
    Publication Date: 2019-07-19
    Description: Assimilation systems synthesize diverse in-situ and satellite data streams into full four-dimensional state estimates by combining the strengths of each data set and also of the model. The resulting analysis provides an integrated view of the information in the various observations as well as derived estimates of unobserved quantities. Assimilation systems are particularly important for the ocean where subsurface observations, even today, are sparse and intermittent compared with the scales needed to represent ocean variability and where satellites only sense the surface. Increasingly, models and assimilation systems are being used to provide information about the current observing system and to help in the design plans for new observations. Whether it is as a user of observations or a contributor to evaluation of the observing system, ocean synthesis and assimilation systems are now an integral part of the global ocean observing and information system. Major advances have been made over the last decade under the auspices of WCRP's Climate Variability and Predictability Project (CLIVAR) and the Global Ocean Data Assimilation Experiment (GODAE). In addition to advances in the assimilation systems, there have been major developments in the observing system, with satellite altimetry, the tropical moored buoy arrays in the Pacific and Atlantic, and more recently Argo. These developments have led to significant advances in our understanding and prediction of ocean variations at both mesoscale and climate scales. Many challenges remain. Some of these challenges lie in the observations themselves, some in the assimilation systems that, even in the more recent era of unprecedented observations from satellite altimetry and Argo, provide different views of climate variations. Yet there are many examples of successful applications from ocean assimilation products. Use of these systems for assessing the observing system helps identify the strengths of each observation type, and indicates that none of the current observations is redundant. Indeed, the indication is that the ocean remains under-sampled and that further improvements in the observing system are needed for both climate monitoring and prediction. Future developments will be increasingly towards consistent analyses across components of the Earth system using, e.g., coupled atmosphere-ocean models.
    Keywords: Oceanography
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  • 21
    Publication Date: 2019-07-19
    Description: Alabama coastal systems have been subjected to increasing pressure from a variety of activities including urban and rural development, shoreline modifications, industrial activities, and dredging of shipping and navigation channels. The impacts on coastal ecosystems are often observed through the use of indicator species. One such indicator species for aquatic ecosystem health is submerged aquatic vegetation (SAV). Watershed and hydrodynamic modeling has been performed to evaluate the impact of land use change in Mobile and Baldwin counties on SAV stressors and controlling factors (temperature, salinity, and sediment) in Mobile Bay. Watershed modeling using the Loading Simulation Package in C++ (LSPC) was performed for all watersheds contiguous to Mobile Bay for land use scenarios in 1948, 1992, 2001, and 2030. Landsat-derived National Land Cover Data (NLCD) were used in the 1992 and 2001 simulations after having been reclassified to a common classification scheme. The Prescott Spatial Growth Model was used to project the 2030 land use scenario based on current trends. The LSPC model simulations provided output on changes in flow, temperature, and sediment for 22 discharge points into the Bay. Theses results were inputted in the Environmental Fluid Dynamics Computer Code (EFDC) hydrodynamic model to generate data on changes in temperature, salinity, and sediment on a grid with four vertical profiles throughout Mobile Bay. The changes in the aquatic ecosystem were used to perform an ecological analysis to evaluate the impact on SAV habitat suitability. This is the key product benefiting the Mobile Bay coastal environmental managers that integrates the influences of temperature, salinity, and sediment due to land use driven flow changes with the restoration potential of SAVs.
    Keywords: Oceanography
    Type: M09-0611 , 23rd Alabama Water Resources Conference and AWRA Symposium; Sep 09, 2009 - Sep 11, 2009; Orange Beach, AL; United States
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  • 22
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    Instituto Oceanográfico de la Armada, Guayaquil, Ecuador
    Publication Date: 2021-05-19
    Description: Se analizan parámetros oceanográficos y meteorológicos en el Océano Pacífico Ecuatorial para el período comprendido de noviembre de 1986 a diciembre de 1988. A fines de 1986 y durante 1987 las anomalías de dichos parámetros y su intensidad indican la ocurrencia de un evento Niño de carácter moderado. El fenómeno decae hacia finales de 1987 y durante el año de 1988 se desarrollaron condiciones anómalas contrarias o anti-Niño, que se mantuvieron durante los últimos meses del año.
    Description: Incluye ref.bibl., grafs., tbls.
    Description: Published
    Description: El nino phenomena
    Keywords: Meteorological observations ; Oceanography ; Meteorological data ; Marine meteorology ; Oceanography ; Oceanographic data ; Meteorological data ; Meteorological observations
    Repository Name: AquaDocs
    Type: Journal Contribution , Non-Refereed , Article
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  • 23
    Publication Date: 2021-05-19
    Description: La creciente importancia que los recursos de calamar han adquirido en 105 últimos 30 años, los sitúa actualmente entre los más importantes recursos pesqueros del mundo. En consecuencia, paises tradicionalmente no explotadores o consumidores de productos de calamar, han orientado sus esfuerzos hacia el logro de un mejor conocimiento de las especies de cefalópodos que habitan su ambiente marino. En este sentido el aporte de disciplinas tales como la biología ha sido decisivo para desarrollar en forma exitosa pesquerías de calamar, entre otras.El programa de investigaciones del Instituto Nacional de Pesca para 1980 incluyó el estudio integral de la explotación de los calamares como un primer paso hacia el desarrollo de una pesquería del recurso. Este trabajo presenta los resultados de un estudio de los aspectos biológicos de la especie más importante del área: Illex argentinus y forma parte de una serie de tres documentos técnicos escritos por el autor referentes a recursos de calamar. Dichos documentos están relacionados con la tecnología de captura y la producción y comercialización del calamar en el Uruguay.
    Description: The growing importance of the squid resources during the last 30 years place them among the more important fish resources of the world. Therefore countries traditional1y non exploiters or consumers of squid products gave steps toward a better knowledge of the species of cephalopods inhabiting their marine environment. For instance, the contribution of subjects such as the biology lead to a successful development of squid fisheries, among others. The 1980 research program of the National Fisheries Institute included an integral study of the exploitation of the squids as a first step toward the development of a squid fishery. This paper presents the results of a study on the biological aspects of the principal species of the area: Illex argentinus. It is part of three technical reports written by the author on squid resources. These reports are fishery technology and production & marketing of squids in Uruguay.
    Description: Montevideo: Instituto Nacional de Pesca
    Description: Published
    Description: Illex argentinus, calamar, ZCP, biología, comportamiento, condiciones ambientales, desove, reproducción, relación de sexos, madurez sexual, crecimiento, frecuencia de longitudes, migraciones
    Keywords: Population structure ; Spawning ; Length ; Growth ; Biology ; Environmental conditions ; Spawning grounds ; Sex ratio ; Sexual maturity ; Reproduction ; Behaviour ; Biology ; Environmental conditions ; Population structure ; Spawning ; Spawning grounds ; Sex ratio ; Sexual maturity ; Reproduction ; Length ; Behaviour ; Migrations ; Growth
    Repository Name: AquaDocs
    Type: Report
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  • 24
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    NIOMR
    Publication Date: 2021-05-19
    Description: 35pp, Illus, Pictures.
    Description: A brief history of the achievements of (NIOMR) Nigerian Institute for Oceanography and Marine Research from 1975 to 1995. The mandate and reason for the establishment of the institute in 1975 inclucive.
    Description: NIOMR
    Description: Published
    Keywords: Oceanography ; Marine sciences
    Repository Name: AquaDocs
    Type: Report , Non-Refereed
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  • 25
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    Massachusetts Institute of Technology and Woods Hole Oceanographic Institution
    Publication Date: 2022-05-25
    Description: Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution February 2008
    Description: The subtidal circulation of the southeast Greenland shelf is described using a set of highresolution hydrographic and velocity transects occupied in summer 2004. The main feature present is the East Greenland Coastal Current (EGCC), a low-salinity, highvelocity jet with a wedge-shaped hydrographic structure characteristic of other surface buoyancy-driven currents. The EGCC was observed along the entire Greenland shelf south of Denmark Strait, while the transect north of the strait showed only a weak shelf flow. This observation, combined with evidence from chemical tracer measurements that imply the EGCC contains a significant Pacific Water signal, suggests that the EGCC is an inner branch of the polar-origin East Greenland Current (EGC). A set of idealized laboratory experiments on the interaction of a buoyant current with a submarine canyon also supported this hypothesis, showing that for the observed range of oceanic parameters, a buoyant current such as the EGC could exhibit both flow across the canyon mouth or into the canyon itself, setting the stage for EGCC formation. Repeat sections occupied at Cape Farewell between 1997 and 2004 show that the alongshelf wind stress can also have a strong influence on the structure and strength of the EGCC and EGC on timescales of 2-3 days. Accounting for the wind-induced effects, the volume transport of the combined EGC/EGCC system is found to be roughly constant (~2 Sv) over the study domain, from 68°N to Cape Farewell near 60°N. The corresponding freshwater transport increases by roughly 60% over this distance (59 to 96 mSv, referenced to a salinity of 34.8). This trend is explained by constructing a simple freshwater budget of the EGCC/EGC system that accounts for meltwater runoff, melting sea-ice and icebergs, and net precipitation minus evaporation. Variability on interannual timescales is examined by calculating the Pacific Water content in the EGC/EGCC from 1984-2004 in the vicinity of Denmark Strait. The PW content is found to correlate significantly with the Arctic Oscillation index, lagged by 9 years, suggesting that the Arctic Ocean circulation patterns bring varying amounts of Pacific Water to the North Atlantic via the EGC/EGCC.
    Description: Funding for the cruise and analysis was provided by National Science Foundation grant OCE-0450658, which along with NSF grant OCE- 0095427 provided funds for my tuition and stipend as well.
    Keywords: Ocean currents ; Oceanography ; James Clark Ross (Ship) Cruise JR105
    Repository Name: Woods Hole Open Access Server
    Type: Thesis
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  • 26
    Publication Date: 2022-05-25
    Description: Author Posting. © Acoustical Society of America, 1998. This article is posted here by permission of Acoustical Society of America for personal use, not for redistribution. The definitive version was published in Journal of the Acoustical Society of America 103 (1998): 330-335, doi:10.1121/1.421092.
    Description: Amplitude and phase fluctuations of monochromatic acoustic signals traveling through diffuse mid-ocean ridge hydrothermal vent plumes are modeled using existing theory in an attempt to find suitable frequencies and path lengths for plume monitoring. Weak-scattering solutions are evaluated numerically, with model parameters adjusted to match observed plume characteristics. Constraints required for weak-scattering solutions to be valid can be met for transmission ranges of 500–2000 m and frequencies of 20–80 kHz. Therefore, because fluid structure and scattering strength are more closely linked for weak scattering than for stronger scattering, inversion for fluid statistical properties may be possible, enabling diffuse vent monitoring. Such monitoring would be subject to geometric assumptions such as transmission entirely within a statistically homogeneous plume. Performance-limiting phase fluctuations have also been computed for a 13–17 kHz geodetic survey system.
    Description: This work was supported by the Woods Hole Oceanographic Institution with research funds provided by the Mellon Foundation.
    Keywords: Underwater sound ; Oceanography ; Acoustic wave scattering ; Seafloor phenomena
    Repository Name: Woods Hole Open Access Server
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  • 27
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    Massachusetts Institute of Technology and Woods Hole Oceanographic Institution
    Publication Date: 2022-05-25
    Description: Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution August 1980
    Description: Observational evidence of seasonal variability below the main thermocline in the eastern North Atlantic is described, and a theoretical model of oceanic response to seasonally varying windstress forcing is constructed to assist in the interpretation of the observations. The observations are historical conductivity-temperature-depth data from the Bay of Biscay region (2° to 20°W, 42° to 52°N), a series of eleven cruises over the three years 1972 through 1974, spaced approximately three months apart. The analysis of the observations utilizes a new technique for identifying the adiabatically leveled density field corresponding to the observed density field. The distribution of salinity anomaly along the leveled surfaces is examined, as are the vertical displacements of observed density surfaces from the leveled reference surfaces, and the available potential energy. Seasonal variations in salinity anomaly and vertical displacement occur as westward propagating disturbances with zonal wavelength 390 (±50) km, phase 71 (±30) days from 1 January, and maximum amplitudes of ±30 ppm and ±20 db respectively. The leveled density field varies seasonally with an amplitude corresponding to a thermocline displacement of ±15 db. The observations are consistent with the predictions of a model in which an ocean of variable stratification with a surface mixed layer and an eastern boundary is forced by seasonal changes in a sinusoidal windstress pattern, when windstress parameters calculated from the observations of Bunker and Worthington (1976) are applied.
    Description: This work was supported by the Office of Naval Research under contract N00014~76-C-197, NR 083-400.
    Keywords: Oceanography ; Ocean-atmosphere interaction ; Ocean circulation ; Energy budget (Geophysics)
    Repository Name: Woods Hole Open Access Server
    Type: Thesis
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  • 28
    Publication Date: 2022-05-25
    Description: Author Posting. © Acoustical Society of America, 2000. This article is posted here by permission of Acoustical Society of America for personal use, not for redistribution. The definitive version was published in Journal of the Acoustical Society of America 107 (2000): 3073-3083, doi:10.1121/1.429336.
    Description: Six sonic booms, generated by F-4 aircraft under steady flight at a range of altitudes (610–6100 m) and Mach numbers (1.07–1.26), were measured just above the air/sea interface, and at five depths in the water column. The measurements were made with a vertical hydrophone array suspended from a small spar buoy at the sea surface, and telemetered to a nearby research vessel. The sonic boom pressure amplitude decays exponentially with depth, and the signal fades into the ambient noise field by 30–50 m, depending on the strength of the boom at the sea surface. Low-frequency components of the boom waveform penetrate significantly deeper than high frequencies. Frequencies greater than 20 Hz are difficult to observe at depths greater than about 10 m. Underwater sonic boom pressure measurements exhibit excellent agreement with predictions from analytical theory, despite the assumption of a flat air/sea interface. Significant scattering of the sonic boom signal by the rough ocean surface is not detected. Real ocean conditions appear to exert a negligible effect on the penetration of sonic booms into the ocean unless steady vehicle speeds exceed Mach 3, when the boom incidence angle is sufficient to cause scattering on realistic open ocean surfaces.
    Description: This work was funded by the NASA Langley Research Center (Technical Monitor, Dr. Kevin Shepherd).
    Keywords: Shock waves ; Oceanography ; Underwater acoustic propagation
    Repository Name: Woods Hole Open Access Server
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  • 29
    Publication Date: 2022-05-25
    Description: Author Posting. © Acoustical Society of America, 1995. This article is posted here by permission of Acoustical Society of America for personal use, not for redistribution. The definitive version was published in Journal of the Acoustical Society of America 98 (1995): 2270-2279, doi:10.1121/1.413341.
    Description: Numerically simulated acoustic transmission from a single source of known position (for example, suspended from a ship) to receivers of partially known position (for example, sonobuoys dropped from the air) are used for tomographic mapping of ocean sound speed. The maps are evaluated for accuracy and utility. Grids of 16 receivers are employed, with sizes of 150, 300, and 700 km square. Ordinary statistical measures are used to evaluate the pattern similarity and thus the mapping capability of the system. For an array of 300 km square, quantitative error in the maps grows with receiver position uncertainty. The large and small arrays show lesser mapping capability than the mid-size array. Mapping errors increase with receiver position uncertainty for uncertainties less than 1000-m rms, but uncertainties exceeding that have less systematic effect on the maps. Maps of rms error of the field do not provide a complete view of the utility of the acoustic network. Features of maps are surprisingly reproducible for different navigation error levels, and give comparable information about mesoscale structures despite great variations in those levels.
    Description: This work was supported by Office of Naval Research grants N00014-9l-J-1138 (Arctic Sciences )and N00014-92-I-1162 (Ocean Acoustics).
    Keywords: Accuracy ; Errors ; Mapping ; Oceanography ; Remote sensing ; Simulation ; Tomography ; Wave propagation ; Sound sources ; Sound velocity
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 30
    Publication Date: 2022-05-25
    Description: Author Posting. © Acoustical Society of America, 2003. This article is posted here by permission of Acoustical Society of America for personal use, not for redistribution. The definitive version was published in Journal of the Acoustical Society of America 114 (2003): 2685-2697, doi:10.1121/1.1614258.
    Description: Acoustic scattering techniques provide a unique and powerful tool to remotely investigate the physical properties of the ocean interior over large spatial and temporal scales. With high-frequency acoustic scattering it is possible to probe physical processes that occur at the microstructure scale, spanning submillimeter to centimeter scale processes. An acoustic scattering model for turbulent oceanic microstructure is presented in which the current theory, which only accounts for fluctuations in the sound speed, has been extended to include fluctuations in the density as well. The inclusion of density fluctuations results in an expression for the scattering cross section per unit volume, σv, that is explicitly dependent on the scattering angle. By relating the variability in the density and sound speed to random fluctuations in oceanic temperature and salinity, σv has been expressed in terms of the temperature and salinity wave number spectra, and the temperature-salinity co-spectrum. A Batchelor spectrum for temperature and salinity, which depends on parameters such as the dissipation rates of turbulent kinetic energy and temperature variance, has been used to evaluate σv. Two models for the temperature-salinity co-spectrum have also been used. The predictions indicate that fluctuations in the density could be as important in determining backscattering as fluctuations in the sound speed. Using data obtained in the ocean with a high resolution vertical microstructure profiler, it is predicted that scattering from oceanic microstructure can be as strong as scattering from zooplankton.
    Description: This work was supported in part by ONR, NSF, and the Woods Hole Oceanographic Institution.
    Keywords: Acoustic wave scattering ; Underwater acoustic propagation ; Oceanography ; Remote sensing ; Oceanographic techniques
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 31
    Publication Date: 2022-05-25
    Description: Author Posting. © Acoustical Society of America, 1996. This article is posted here by permission of Acoustical Society of America for personal use, not for redistribution. The definitive version was published in Journal of the Acoustical Society of America 99 (1996): 822-830, doi:10.1121/1.414563.
    Description: In a recent paper, Lynch et al. used modal and ray based perturbation techniques to compare predicted variances of acoustic travel times due to internal waves to measured variances in the Barents Sea Polar Front experiment [Lynch et al., J. Acoust. Soc. Am. 99, 803–821 (1996)]. One of the interesting results of this work is that the modal and ray travel-time variances are substantially different for rays and modes with the same grazing angle. Specifically, the maximum modal travel-time variance shows a resonant effect in which the variance increases with increasing frequency. Unlike the modal solution, the ray travel-time variance has a geometrically constrained maximum, independent of frequency. In this paper, the linear first-order solutions for the ray and modal variances due to the internal waves are reviewed, and in an Appendix the effects of the linearizing assumptions are examined. The ray and mode solutions are then shown to be consistent by considering a truncated sum of modes that constructively interfere along a geometric ray path. By defining the travel-time perturbation due to a truncated sum of modes, the travel-time variance of the modal sum is derived. With increasing frequency the maximum value of this variance converges to a frequency-independent result with a similar magnitude to the ray maximum variance.
    Keywords: Internal waves ; Oceanography ; Sound waves ; Travelling waves ; Underwater ; Wave propagation ; Barents Sea ; Ray trajectories ; Shallow–water equations ; Travel time
    Repository Name: Woods Hole Open Access Server
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  • 32
    Publication Date: 2021-01-30
    Description: This Guide describes the operational procedures for the BATHY/TESAC Operational Programme, which includes the collection and exchange of operational BATHY, TESAC and, since 1 November 1987, TRACKOB data. The instructions and guidelines to be followed are arranged under the following main headings: • Data Collection • Data Encoding • Data Routing • Error Checking and Quality Control • Monitoring
    Description: Third Revised Edition - Original: English; also available in French, Spanish & Russian
    Description: Published
    Description: Operational Data Dissemination, data collection, Observational Strategy, Quality Control Procedures, data routing, Platform to Shore Transmission, Monitoring, National Monitoring, Monthly Exchange, Periodic GTS Monitoring,
    Keywords: Oceanography ; Monitoring ; Data processing ; Data storage ; Data acquisition ; Data collections ; Data acquisition ; Data processing ; Data storage ; Data transmission ; Quality control ; Monitoring ; Monitoring systems
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  • 33
    Publication Date: 2021-05-19
    Description: This manual sets out an approach to the identification and monitoring of shoreline change and its causative processes at local and regional scales that is appropriate to the coastal management problems of the region as reported by the regional contributors. The approach aims to promote the targeting of sparse resources on the acquisition and provision of information that is most relevant to the management of the problem. The procedures for monitoring shoreline change and its contributory processes are described, including the use of accessible relevant regional information and data or meta-data sets.
    Description: Affiliation: Mr Kuria Kairu, Kenya Marine and Fisheries Research Institute, Mombasa Kenya and Dr Ntahondi Nyandwi, Institute of Marine Sciences, University of Dar-es-Salaam Zanzibar, Tanzania
    Description: Published
    Description: Physical shoreline change, classifying coasts, coastal change,
    Keywords: Oceanography ; Environmental monitoring ; Environmental surveys ; Environmental monitoring ; Socioeconomic aspects ; Sociological aspects ; Coastal structures ; Coastal zone ; Coastal zone management ; Sediment analysis ; Sedimentary environments ; Sedimentary rocks ; Sedimentary structures
    Repository Name: AquaDocs
    Type: Non-Refereed
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  • 34
    Publication Date: 2021-05-19
    Description: IOC Manuals and guides No. 5
    Description: National Oceanographic Data Centre, NODC, expanded activities, International considerations
    Keywords: Oceanography ; Oceanographic institutions ; Oceanographic data
    Repository Name: AquaDocs
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  • 35
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    Publication Date: 2021-01-30
    Description: Published
    Description: Wave data exchange, measured wave data
    Keywords: Oceanography ; Wave buoys ; Wave data ; Wave measurement ; Wave parameters
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  • 36
    Publication Date: 2021-01-30
    Description: Published
    Description: GF3, Reference sheets, GF3-PROC
    Keywords: Oceanography ; Computer programs ; Data storage ; Data storage ; Computer programs
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  • 37
    Publication Date: 2021-01-30
    Description: 1st Revised Edition
    Description: Published
    Description: data encoding, data collection, data routing, monitoring, BATHY, TESAC
    Keywords: Oceanography ; Data acquisition ; Data storage ; Data processing ; Data acquisition ; Data storage ; Data transmission ; Data processing ; Quality control ; Salinity data ; Salinity measurement ; Salinity measuring equipment ; Surface currents ; Surface salinity ; Surface temperature
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  • 38
    Publication Date: 2021-05-19
    Description: IOC Manuals and guides No. 17, Volume 2
    Description: GF3 tapes, GF3 records, GF3 code table,
    Keywords: Oceanography ; Data processing ; Data collections ; Data processing ; Exchange capacity
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  • 39
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    UNESCO
    Publication Date: 2021-01-30
    Description: This Document is the second revision of the IOC Manuals and Guides No.5. The first edition was published in 1975 and the first revision in 1997. This document deals mainly with oceanographic data management but, as data and information management are increasingly complementary, some attention is also given to marine information management. This Guide is intended as a tool for policy makers at the national level to assist them with the decision-making related to the establishment of national facilities for the management of oceanographic data (and information). It is also intended to be a reference document for national organizations involved in, or planning to be involved in, oceanographic data and information management.
    Description: UNESCO
    Description: 2nd revised edition
    Description: Published
    Description: Oceanographic data centre, coordination data centre,
    Keywords: Oceanography ; Data acquisition ; Data processing ; Data acquisition ; Data collections ; Data processing ; Data reports ; Data transmission
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  • 40
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    Publication Date: 2021-05-19
    Description: The material on the "Black Sea Data Management Guide" are prepared in accordance with the working plans of the IOC Committee on International Data and Information Exchange (IODE) and its regional component in the Black Sea region to assist specialists of the Black Sea countries in the field of Data Management. The Guide includes the following items: national oceanographic data centres, designated national agencies, other marine centres and institutions of the Black Sea region countries dealing with problems of oceanographic data; current international and national projects and programs of the Black Sea region countries; preliminary catalogue marine observation in the Black Sea; bibliography of publications of the marine centres and institute of the Black Sea region on problems of the Black Sea data and information published mainly during the past 5 years; other information related to oceanographic data and information on the Black Sea.
    Description: Manual and Guide NO 43
    Description: Ecosystem processes, integrated coastal, shelf zone
    Keywords: Oceanography ; Oceanography ; Oceanographic surveys ; Oceanography ; Ecosystem management ; Monitoring systems ; Oceanographic data ; Oceanographic surveys ; Oceanographic institutions
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  • 41
    Publication Date: 2021-05-19
    Description: This first issue is devoted to the use of indicators for ICAM, and is a direct result of the IOC-DFO-NOAA-CSMP International Workshop on the same topic, organised in May 2002, in Ottawa. Based on a background paper prepared by the Center for the Study of Marine Policy (University of Delaware) in preparation for the workshop, the aim of this Reference Guide is to present a literature review on the use of indicators around the world, from various programmes and projects, at global, regional, national and local scale.The need for indicators and reporting techniques which reflects the performance of coastal management projects and programmes and reveals the complex relationship that exist between coastal ecosystem health and anthropogenic activities, socio-economic conditions and managerial decisions, has been reinforced recently by the World Summit on Sustainable Development’s Plan of Implementation. This Dossier will hopefully offer a first step towards the development of common practices and protocols in the application of such indicators.
    Description: ICAM Dossier 1
    Description: Published
    Description: Gouvernance aspect socioecono;ic indicator, coastal and Marine environment
    Keywords: Oceanography ; Marine environment ; Marine ecology ; Policies ; Coastal oceanography ; Coastal zone management ; Marine ecology ; Marine environment ; Environment management ; Socioeconomic aspects ; Policies
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  • 42
    Publication Date: 2021-05-19
    Description: The aim of this guide is to assist in the organisation of environmental information and thus to contribute to the concerted preparation of management plans which should be implemented by all the environmental actors : decision-makers, managers, users and scientists. The proposed methodological approach provides the unifying thread for the user of this guide. It comprises a certain number of stages which lead to the formulation of the management objectives. The assistance given contributes finally to the definition of the real management strategy to be applied (plan, diagram, programme of action and follow up). The architecture of this methodological approach is organised around a master chart, referred to as “Stages in the Approach”. This indicates the different stages to be followed for the definition of a management plan. This master chart is fed by two types of input data which constitute the information
    Description: This document is available in English and French versions
    Description: Published
    Description: methodological approach
    Keywords: Oceanography ; Coastal zone management
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  • 43
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    UNESCO
    Publication Date: 2021-01-30
    Description: This manual is concerned primarily with techniques for the measurement of what are called relative sea level changes which means changes relative to the level of the land upon which the measuring instrument (the tide gauge) is located. The subject of changes in the level of land itself is reviewed later in this document but is given more detailed presentation in other reports to which we refer. The manual also concerns itself primarily with the part of the frequency spectrum of sea level change from minutes through to centuries by means of in situ devices at the coast (tide gauges). Such changes are sometimes called still water level changes, being changes over a period long enough to average over wind waves. The devices employed to make these measurements are usually called tide gauges, although sea level recorders might be a more appropriate term. In this manual we have kept the older, conventional term.
    Description: Published
    Description: transducer gauge, acoustic gauge,data transmission methods
    Keywords: Oceanography ; Sea level measurement ; Sea level changes ; Tide gauges ; Acoustic data ; Acoustic transducers ; Acoustic current meters ; Transducers
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  • 44
    Publication Date: 2021-05-19
    Description: This document is directed to the scientific research community and users of operational ocean data. It is also intended to provide an example and be a source of information to programmes such as the Global Ocean Observing System (GOOS) for developing and implementing end-to-end data management systems. The document is also directed towards Member States of IOC. It discusses how Member States can make contributions and how they can benefit from the GTSPP.
    Description: Published
    Description: temperature profile, salinity prifile, GTSPP
    Keywords: Oceanography ; Salinity ; Temperature data ; Temperature measurement ; Ocean circulation ; Salinity ; Salinity data ; Salinity measurement ; Salinity profiles ; Salinity scales
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    Type: Report
    Format: 33
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  • 45
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    UNESCO
    Publication Date: 2021-05-19
    Description: This document is available in English, French, Spanish and Russian versions
    Description: Published
    Description: IGOSS, Training, Assistance, encoding data, data exchange, buoy monitoring system
    Keywords: Oceanography ; Sea level ; Data acquisition ; Data processing ; Sea level ; Wave data ; Data acquisition ; Data converters ; Data transmission ; Buoys ; Data collections ; Data processing
    Repository Name: AquaDocs
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  • 46
    Publication Date: 2021-01-30
    Description: Published
    Description: GF3, Package control, GF3-PROC Software
    Keywords: Oceanography ; Data acquisition ; Data processing ; Data storage ; Data acquisition ; Data processing ; Data storage
    Repository Name: AquaDocs
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  • 47
    Publication Date: 2021-05-19
    Description: IOC Manuals and guides No. 26
    Description: data quality control, International Oceanographic Data Exchange,
    Keywords: Oceanography ; Data processing ; Quality assurance ; Data processing ; Quality control ; Quality assurance
    Repository Name: AquaDocs
    Format: 437
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  • 48
    Publication Date: 2021-05-19
    Description: IOC Manuals and guides No. 9 : Revised edition
    Description: Oceanographic data exchange, Oceanographic data centre, data product, data collection, data catalogues
    Keywords: Oceanography ; Data acquisition ; Data processing ; Data acquisition ; Data processing ; Data transmission ; Data collections ; Oceanographic data
    Repository Name: AquaDocs
    Format: 84
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  • 49
    Publication Date: 2021-05-19
    Description: Published
    Description: IGOSS, Specialised Oceanographic centres, SOCs, Fonction, products, Information exchange, development plan
    Keywords: Oceanography ; Oceanography ; Oceanographic institutions ; Oceanography
    Repository Name: AquaDocs
    Format: 19
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  • 50
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    UNESCO
    Publication Date: 2021-01-30
    Description: Since the Intergovernmental Oceanographic Commission and the World Meteorological Organization adopted the IGOSS General Plan and Implementation Programme for Pbse I in 1969, the routine international exchange of oceanographic data within the framework of IGOSS has become a reality. The Pilot Project for the Collection, Exchange and Evaluation of Bathythermograph Data, which waa the initie1 operational phase of IGOSS has demonstrated that the provision of oceanographic services is feasible and beneficial.
    Description: Published
    Description: IGOSS, WMO, GEMS, observing system, telecommunication arrangement, Marine Pollution Monitoring Programme, MPMP, training programme, education programme, data archiving, data exchange
    Keywords: Oceanography ; Meteorological data ; Bathymetric data ; Bathymetric surveys ; Meteorological data
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    Format: 42
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  • 51
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    UNESCO
    Publication Date: 2021-01-30
    Description: The Integrated Global Observing Strategy Partnership (IGOS-P) established, in 1999, a thematic approach to the implementation of the IGOS. Recognising that other themes will emerge, the “Ocean Theme” was chosen to be the “pathfinder” in this approach and an Ocean Theme Team was assembled to formulate guidance. One goal of the Ocean Theme Team is to consider and study the full range of current and planned observations, while identifying potential gaps in future observations that might compromise ocean observational records. This document presents a proposed set of long-term ocean observations and identifies a number of challenges for the improvement of knowledge about both the oceans and observing techniques. The overall strategy is to create an observing system for the oceans that serves the research and operational oceanographic communities. The set of observations is based on an evaluation of the range of requirements that have already been presented by GOOS, GCOS, and GODAE. The next five years must include development of institutional structures committed to (1) managing the total data flow (in situ as well as satellite); (2) managing the production, distribution and quality assessment of relevant data products; and (3) working with end-users to ensure that the evolving system is responsive to their needs. It is also recognised that observation protocols evolve with time and, therefore, that the stated observational requirements will need to be reviewed in future. It is the recognised applications that ultimately drive the shape of the requirements for the ocean observing system. The observations on which we focus here are needed to address important issues in ocean science, and through combinations of measurements and models, to support the production of an extensive range of products for a broad community of users. The applications are directly linked to societal needs, including among other things numerical weather prediction, seasonal-to-interannual climate forecasts, and climate assessment. The data are needed for deriving fields of information about the ocean and for initialising and validating the models used to derive other products. Aside from observations we also need to improve, through the Global Ocean Data Assimilation Experiment (GODAE) and the Ocean Biology Project, how we assimilate the data into models.
    Description: Published
    Description: Ocean Biology, Ocean topography, Gravity, Geold, atmospheric pressure
    Keywords: Oceanography ; Salinity ; Surface temperature ; Wind vectors ; Sea ice ; Salinity
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  • 52
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    Publication Date: 2021-01-30
    Description: The Integrated Global Observing Strategy Partnership (IGOS-P) established, in 1999, a thematic approach to the implementation of the IGOS. Recognising that other themes will emerge, the “Ocean Theme” was chosen to be the “pathfinder” in this approach and an Ocean Theme Team was assembled to formulate guidance. One goal of the Ocean Theme Team is to consider and study the full range of current and planned observations, while identifying potential gaps in future observations that might compromise ocean observational records. This document presents a proposed set of long-term ocean observations and identifies a number of challenges for the improvement of knowledge about both the oceans and observing techniques. The overall strategy is to create an observing system for the oceans that serves the research and operational oceanographic communities. The set of observations is based on an evaluation of the range of requirements that have already been presented by GOOS, GCOS, and GODAE. The next five years must include development of institutional structures committed to (1) managing the total data flow (in situ as well as satellite); (2) managing the production, distribution and quality assessment of relevant data products; and (3) working with end-users to ensure that the evolving system is responsive to their needs. It is also recognised that observation protocols evolve with time and, therefore, that the stated observational requirements will need to be reviewed in future. It is the recognised applications that ultimately drive the shape of the requirements for the ocean observing system. The observations on which we focus here are needed to address important issues in ocean science, and through combinations of measurements and models, to support the production of an extensive range of products for a broad community of users. The applications are directly linked to societal needs, including among other things numerical weather prediction, seasonal-to-interannual climate forecasts, and climate assessment. The data are needed for deriving fields of information about the ocean and for initialising and validating the models used to derive other products. Aside from observations we also need to improve, through the Global Ocean Data Assimilation Experiment (GODAE) and the Ocean Biology Project, how we assimilate the data into models.
    Description: sea topography, Ocean vector wind, gravity, geold, atmospheric pressure
    Keywords: Oceanography ; Wind vectors ; Surface temperature ; Sea ice
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    Format: 32
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  • 53
    Publication Date: 2021-05-19
    Description: The OdinPubAfrica project (FUST-project: - see) developed a repository for scientific literature of African marine science. During the project other Odin groups, in the first place OdinCarsa were interested to develop a similar repository project for their region. As a result the OdinPubAfrica repository was extended to accept other Odin groups and was renamed to OceanDocs (http://iodeweb1.vliz.be/odin - http://www.oceandocs.net). This program proposal is based on the experiences of OdinPubAfrica and the interest by new partners.
    Description: Supported by IOC/IODE
    Description: Document available in English
    Description: Repository; oceanography, marine science
    Keywords: aquatic sciences ; Oceanography ; Marine sciences ; Information services
    Repository Name: AquaDocs
    Type: Non-Refereed , Paper
    Format: 10
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  • 54
    Publication Date: 2021-01-30
    Description: This guide has been prepared to assist Member States of Intergovernmental Oceanographic Commission (IOC) in establishing and operating a national oceanographic data centre (NODC). Since the early 1960s, approximately 55 Member States of IOC have established oceanographic data centres or designated a national agency as responsible for international oceanographic data and information exchange. These data centres and designated national agencies (DNAs) support both national and international clients with oceanographic data and information services.
    Description: 1st revised edition
    Description: Published
    Description: National Oceanographic data centre
    Keywords: Oceanography ; Data ; Data processing ; Data collections ; Data ; Data processing ; Oceanographic data
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  • 55
    Publication Date: 2021-01-30
    Description: All nations are profoundly influenced by the world oceans in many ways - some direct and obvious, others indirect and more subtle. Even those countries without ocean coastline feel the influence of the ocean, for example, as it affects world-wide weather and climate and In the availability of foreign goods and access to distant markets. Some influences of the ocean are benefitial; others may be detrimental to human activities ; most are beyond our ability to control, except in very limited ways, but, forewarned with a knowledge of the state of the ocean and even a limited prediction of future trends, it may often be possible to maximize the beneficial effects and to avoid or guard effectively against those which could be detrimental. The Integrated Global Ocean Services System (IGOSS) was conceived as a eans to collect and, exchange oceanic data in such a form that they can be readily interpreted and applied to practical problems. Data in various forms may be gathered from many sources, It is necessary to properly encode and route these data to processing centers using proper quality control procedures. It is then possible to prepare products which summarize and/or interpret the data in ways which are meaninful and useful to users, Finally, the products are distributed to users and the data are stored or "archived" for future use, The IGOSS system has been designed to carry out these functions in co-operation with other international agencies.
    Description: Manual and Guide : Revised Edition
    Description: Published
    Description: data routing, data storage, data exchange, BATHY, TESAC
    Keywords: Oceanography ; Salinity ; Subsurface water ; Current measurement ; Current data ; Current measuring equipment ; Salinity ; Salinity data ; Salinity measuring equipment ; Salinity measurement ; Temperature data ; Temperature measurement ; Temperature gradients ; Subsurface currents ; Subsurface water ; Surface salinity ; Surface temperature
    Repository Name: AquaDocs
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  • 56
    Publication Date: 2021-05-19
    Description: IOC Manuals and guides No. 1 - 2nd revision
    Description: IGOSS, IODE, GTSPP, Oceanographic data collection, Oceanographic datas exchange, oceanographic data storege
    Keywords: Oceanography ; Salinity ; Bathymetric profiles ; Bathythermographic data ; Current meter data ; Current measuring equipment ; Temperature data ; Temperature gradients ; Temperature fields ; Salinity data ; Salinity measurement ; Salinity
    Repository Name: AquaDocs
    Format: 28
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  • 57
    Publication Date: 2021-05-19
    Description: The purpose of this guide is to propose a complete methodological procedure for the creation of a database and a cartographic decision-aid system. It is illustrated by two case studies carried out in the area in the framework of the Indian Ocean Commission’s Regional Environmental Programme (REP), financed by the European Union (REP-IOC/EU).
    Description: UNESCO, EU
    Description: Manual and Guide NO. 38 : This document is available in English and French version
    Description: Published
    Description: Coastal Zone Mapping, Geomorphological units, Raw data mapping, risk notions
    Keywords: Oceanography ; Mapping ; Geomorphology ; Mapping ; Maps ; Map projections ; Coastal zone ; Coastal morphology ; Geological data ; Geomorphology
    Repository Name: AquaDocs
    Format: 44
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  • 58
    Publication Date: 2021-01-30
    Description: The handbook aims to contribute to the sustainable development of coastal and marine areas by promoting a more out-come-oriented, accountable and adaptive approach to ICOM. It provides a step-by-step guide to help users in developing, selecting and applying a common set of governance, ecological and socioeconomic indicators to measure, evaluate and report on the progress and outcomes of ICOM interventions. Intended as a generic tool with no prescriptive character, the handbook proposes analytical framework and indicators that from the basis for the customized design of sets of indicators. The handbook also includes results, outcomes and lessons learned from eight pilot case studies conducted in several countries. A network of ICOM experts in these countries has also been established. The target audience is wide, and includes coastal and ocean managers, practitioners, evaluations and researchers. The handbook forms part of an IOC toolkit on indicators. Its preparations is part of an effort to promote the development and use of ICOM indicators led by the Intergovernmental Oceanographic Commission, the Department of Fisheries and Oceans of Canada and the U.S. National Oceanic and Atmospheric Administration.
    Description: Published
    Description: ecological indicator, integrated coastal and ocean management, ecological indicator, Governance indicator
    Keywords: Oceanography ; Oceanography ; Ecological balance ; Coastal zone management ; Coastal zone ; Oceanography ; Oceanographic data ; Oceanographic institutions ; Oceanographic equipment ; Oceanographic surveys ; Indicators ; Ecological balance
    Repository Name: AquaDocs
    Format: 224
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  • 59
    Publication Date: 2021-05-19
    Description: IOC Manuals and guides No. 1 : Revised version
    Description: Published
    Description: Data archives, IGOSS, IODE, Data management, Data exchange, BATHY, TESAC, Data repository
    Keywords: Oceanography ; Data storage ; Data processing ; Data storage ; Data processing ; Data collections
    Repository Name: AquaDocs
    Format: 43
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  • 60
    Publication Date: 2021-01-30
    Description: Published
    Description: Observing practices
    Keywords: Oceanography ; Meteorological instruments ; Meteorological observations ; Thermometers ; Atmospheric pressure ; Meteorological data ; Marine technology ; Meteorological instruments ; Meteorological data ; Meteorological observations ; Oceanographic equipment ; Oceanographic surveys ; Sea surface ; Temperature measurement ; Salinity measuring equipment ; Bathythermographs ; Thermometers ; Wave measuring equipment ; Wave measurement ; Wind measurement ; Wind measuring equipment ; Swell ; Atmospheric pressure ; Water colour ; Water transparency
    Repository Name: AquaDocs
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  • 61
    Publication Date: 2021-01-30
    Description: IOC Technical Series No. 8
    Description: IGOSS, principles, scope, implementation programme, WARC
    Keywords: Oceanography ; Oceanographic stations ; Oceanographic institutions ; Oceanographic data
    Repository Name: AquaDocs
    Type: Other
    Format: 31
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  • 62
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    UNESCO
    Publication Date: 2021-05-19
    Description: Development of an African repository for electronic publications in marine science and oceanography Realisations in 2004 – Planning of 2005 The goal of OdinPubAfrica is to develop an electronic platform to collect scientific documents (articles, conference papers, working papers …) produced by members of African research institutes in the field of oceanography and marine science. A two year project was accepted by the government of Flanders in the FUST–program to realize the goal. The University Library of LUC (Belgium) is coordinating the project, which started officially on August 1, 2005.
    Description: Supported by IOC/IODE
    Description: Document available in English
    Description: e-repository
    Keywords: Marine sciences ; Oceanography ; Information services
    Repository Name: AquaDocs
    Type: Non-Refereed , Paper
    Format: 5
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  • 63
    Publication Date: 2021-05-19
    Description: IOC Manuals and guides No. 24
    Description: Remote sensing equipments, measurement, ocean sensor applications, fisheries, offshore exploration, ship trafic
    Keywords: Oceanography ; Marine environment ; Remote sensing ; Remote sensing equipment ; Remote sensing ; Satellite sensing ; Satellite photography ; Marine environment
    Repository Name: AquaDocs
    Format: 183
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  • 64
    Publication Date: 2021-01-30
    Description: IOC Manuals and guides No. 17 : Volume 3
    Description: Published
    Description: classical hydrocast data, digital wave records, measured wave spectra
    Keywords: Oceanography ; Sea level ; Geophysical data ; Sea level ; Sea level measurement ; Wave analysis ; Wave data ; Wave height ; Wave measurement ; Sea surface ; Drifting data buoys ; Bathymetric data ; Bathymetry ; Mean sea level
    Repository Name: AquaDocs
    Format: 71
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  • 65
    Publication Date: 2021-05-19
    Description: IOC Manuals and guides No. 25 : Revised Edition
    Keywords: Marine sciences ; Oceanography ; Research institutions ; Research ; Marine sciences ; Marine scientists ; Oceanographic data ; Oceanographic institutions ; Oceanographic surveys ; Oceanography ; Scientific personnel ; Research institutions ; Research programmes ; Research
    Repository Name: AquaDocs
    Type: Other
    Format: 569
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  • 66
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    Publication Date: 2021-01-30
    Description: Published
    Description: Data telemetry, Drifting buoys, hardware, dissemination
    Keywords: Oceanography ; Data processing ; Drifting stations ; Drifting data buoys ; Data collections ; Data processing
    Repository Name: AquaDocs
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  • 67
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    Publication Date: 2021-01-30
    Description: Published
    Description: Time series data, ocean data, sea surface temperature, sea level variability,
    Keywords: Oceanography ; Time series analysis ; Oceanography ; Oceanographic data ; Oceanography ; Oceanographic surveys ; Time series analysis ; Sea level measurement ; Sea level changes ; Seasonal variations
    Repository Name: AquaDocs
    Format: 54
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  • 68
    Publication Date: 2021-01-30
    Description: Published
    Description: Data station, Catalogue
    Keywords: Oceanography ; Data storage ; Data acquisition ; Oceanographic data ; Data transmission ; Data collections ; Data storage ; Data acquisition
    Repository Name: AquaDocs
    Format: 36
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  • 69
    Publication Date: 2021-01-30
    Description: Published
    Description: Oceanographical Data and Information centre Management
    Keywords: Oceanography ; Information systems ; Data ; Data processing ; Data acquisition ; Information retrieval ; Data ; Data processing ; Data acquisition ; Data collections ; Information centres ; Information handling ; Information retrieval ; Information systems
    Repository Name: AquaDocs
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  • 70
    Publication Date: 2021-01-30
    Description: This manual describes the protocol approved by the international Scientific Steering Committee for the Joint Global Ocean Flux Study (JGOFS) for the most of the 20 JGOFS Core Measurements. However, the methods for the analysis of various parameters of the seawater CO2 system are described in a separate handbook. In order to have a complete set of the JGOFS measurements protocols, you should request a copy of the "Handbook of Methods for the Analysis of the Various Parameters of the Carbon Dioxide System in Seawater"version 2, A.G. Dickson and C. Goyet, eds. ORNL/CDIAC-74.
    Description: Published
    Description: JGOFS, Marine microorganisme, measurement,
    Keywords: Oceanography ; Sampling ; Nitrites ; Nitrates ; Zooplankton ; Data processing ; Data ; Oxygen ; Microorganisms ; Bacteriology ; Bacteria ; Ocean circulation ; Oceanographic stations ; Oceanographic data ; Oceanographic surveys ; Samples ; Sampling ; Data processing ; Data ; Data collections ; Quality control ; Salinity measurement ; Oxygen ; Inorganic carbon ; Nitrites ; Nitrates ; Phosphorus compounds ; Phosphorus cycle ; Silicate minerals ; Marine organisms ; Microorganisms ; Bacteriology ; Bacteria ; Zooplankton
    Repository Name: AquaDocs
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  • 71
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    UNESCO | Paris, France
    Publication Date: 2021-01-30
    Description: The purpose of this manual (see Part I), is to assemble in convenientform forthe guidance and use of practising oceanographers the various documents concerned with the assembly and disssemination of oceanographic data of all kinds. The full and expeditious exchange of data is the core of meaningful scientific co-operation. Investigatioqs of phenomena and processes of global dimensions, such as those occurring in the ocean and atmosphere, are particularly dependent on the pooling of data from various sources. on a regional basis has been operated successfully for many years by the International Council for the Exploration of the Sea. The programme of the International Geophysical Year made necessary the creation of a world-wide system. Thus WorldData Centres A and B (Oceanography) were established in Washington and Moscow, their operations being financed by the United States and the USSR. These centres, together with those in other disciplines, are responsible to the International Geophysical Committee (CIG) of the International Couscil of Scientific Unions (see Appendix I to the manual). The Intergovernmental Oceanographic Commission has produced a "Provisional Guide for Exchange of Oceanographic Data" (Part I1 of this manual). While the terms of the ProvisionalGuide are Voluntary, it should be recognized that order is necessary in such a rapidly expanding science if the full advantages of this expansion are to be widely A system for exchanging oceanographic data realized in the most efficient way. Approximate time limits as well as methods for the submission of the various kinds of data remain therefore a feature of the revised Guide, although a less exacting one than before. The "Provisional Guide for Exchange of Oceanographic Data" is supplemented in this manual by recommendations of the IOC Working Group on Oceanographic Data Exchange (Part 111) adopted in January 1964 and approved by the Commission at its,third session. These recommendations give details which are not conveniently included in the Provisional Guide itself. World Data Centres will in due course receive oceanographic data, in accordance with the Provisional Guide for declared national, or international oceanographic programmes. Such programmes entail an obligation to send data to the W D C s . Data can be sent to WDCs by laboratories or other data centres. Part IV of the manual is a list of existing or projected national oceanographic data centres or other designated national agencies, with their addresses, methods of working, and, where applicable, the services offered by each to data contributors I The oceanographic data exchange system exists to facilitate the prosecution of marine research. Its success depends on the support of oceanographers, their supply and use of oceanographic data, and their suggestions for making the system responsive to their needs.
    Description: UNESCO
    Description: Published
    Description: data exchange
    Keywords: Oceanography
    Repository Name: AquaDocs
    Type: Report
    Format: 25pp.
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  • 72
    Publication Date: 2021-01-30
    Description: IOC Manuals and guides No. 9 Annex II
    Description: Published
    Description: Oceanographic data centre, RNODCs, IODE, Development, fonction
    Keywords: Oceanography ; Oceanographic data ; Oceanographic institutions
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  • 73
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    UNESCO
    Publication Date: 2021-01-30
    Description: Published
    Description: Ocean Climatically signifiant, physical parameters, El Nino, Hydrostation, temperature time series
    Keywords: Oceanography ; Physical oceanography ; Time series analysis ; Oceanography ; Physical properties ; Oceanography ; Oceanographic data ; Physical properties ; Physical oceanography ; Plankton surveys ; Hydrographic data ; Hydrographic surveys ; Time series ; Time series analysis ; Temperature data
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  • 74
    Publication Date: 2021-05-19
    Description: IOC Manuals and guides No. 17 - Volume 1
    Description: GF3, Oceanographic data collection,
    Keywords: Oceanography ; Data storage ; Data processing ; Oceanographic data ; Oceanographic surveys ; Data storage ; Data transmission ; Data processing ; Data converters
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  • 75
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    Acoustical Society of America
    Publication Date: 2022-05-26
    Description: Author Posting. © Acoustical Society of America, 2000. This article is posted here by permission of Acoustical Society of America for personal use, not for redistribution. The definitive version was published in Journal of the Acoustical Society of America 108 (2000): 551-555, doi:10.1121/1.429585.
    Description: Acoustic scattering by the seafloor is sometimes influenced, if not dominated, by the presence of discrete volumetric objects such as shells. A series of measurements of target strength of a type of benthic shelled animal and associated scattering modeling have recently been completed (Stanton et al., "Acoustic scattering by benthic and planktonic shelled animals," J. Acoust. Soc. Am., this issue). The results of that study are used herein to estimate the scattering by the seafloor with a covering of shells at high acoustic frequencies. A simple formulation is derived that expresses the area scattering strength of the seafloor in terms of the average reduced target strength or material properties of the discrete scatterers and their packing factor (where the reduced target strength is the target strength normalized by the geometric cross section of the scatterers and the averaging is done over orientation and/or a narrow range of size or frequency). The formula shows that, to first order, the backscattering at high acoustic frequencies by a layer of shells (or other discrete bodies such as rocks) depends principally upon material properties of the objects and packing factor and is independent of size and acoustic frequency. Estimates of area scattering strength using this formula and measured values of the target strength of shelled bodies from Stanton et al. (this issue) are close to or consistent with observed area scattering strengths due to shell-covered seafloors published in other papers.
    Description: This research was supported by the U.S. Office of Naval Research Grant No. N00014-95-1-0287.
    Keywords: Underwater sound ; Oceanography ; Acoustic wave scattering ; Backscatter
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 76
    Publication Date: 2022-05-26
    Description: Originally issued as Reference No. 52-26, series later renamed WHOI-.
    Description: During the summer of 1950, The Woods Hole Oceanographic Institution conducted a study of the waters of Great South Bay for the Town of Islip, New York, with a view to seeking the cause of the decline of the oyster industry, which has deteriorated steadily during the past twenty years. The report of these studies was submitted in January 1951. The survey revealed two conditions which in combination appeared to be unfavorable to the oyster industry. One unfavorable condition was the local change in circulation occasioned by the opening of Moriches Inlet in 1931, which had increased the salinity of Bellport Bay, creating a condition which might well be detrimental to the production of seed oysters. Aside from this, it was concluded that little change had taken place in the salinity and tidal exchange of the central and western part of the bay during the past twenty years. The second unfavorable condition was the pollution of Great South Bay by wastes from the duck farms located along the Carmans River and the tributaries of Moriches Bay. Chemical studies indicated that the bay water is unusually rich in the products of decomposing organic matter. These materials appeared to arise from the mouth of the Carmans River and the tributaries of Moriches Bay, from which they are carried westward across Great South Bay. They provide nutriment for the growth of an unusually dense population of microscopic plants. Evidence existed that oysters do not feed properly on water containing such large concentrations of plant cells, and available statistics showed a clear correlation over a period of years between the condition of bay oysters and the numbers of plant cells in the water. Finally, the decline in oyster production has been closely paralleled by the growth of the duck industry, which increased fourfold during the period. In the report on the survey of 1950, it was pointed out that a number of questions had been revealed which were not anticipated when the field work was in progress and that these questions merited additional study. One of these related to the behavior of uric acid, the peculiar form in which birds secrete nitrogenous wastes, which promised to provide unambiguous evidence on whether the duck farms are the source of pollution. Another was the more detailed study of the circulation of Moriches Bay and its connection with Great South Bay through Narrow Bay, since this appeared to be the principal avenue of the pollution of Great South Bay. Finally, more detailed information was desired concerning the actual quantities of pollutants arising from the duck farms and of the alterations of its components by biological and other action upon introduction into the bay water. Before these additional studies could be undertaken, the problem acquired a new aspect be cause of the spontaneous closure of Moriches Inlet which occurred on May 15, 1951. While this terminated any possibility of increasing knowledge of the circulation between the bays as it previously existed, it afforded an opportunity to observe the effect of the opening on the condition of the bay waters. This information was of prime importance in view of the proposal to reopen and stabilize Moriches Inlet. Field parties visited the region on three occasions during the sumer. On July 12-14, 1951, a survey was made of the entire system of bays lying between the western extremity of Great South Bay and the Shintecock Canal. Between July 27 and August 5, studies were made of the chemical conditions in Moriches Bay and its approaches, and a detailed examination was carried out on the immediate conditions associated with the duck farms along the Terrell River. On September 24-29, an attempt was made to measure the exchange of water and associated pollutants between Moriches Bay and Great South Bay, and through the Quantuck Canal. On this occasion continuous observations were made at Smith Point and Beach Lane Bridge for a period of fifty hours, including four complete tidal cycles.
    Description: The work conducted in 1951 was supported jointly by the appropriations made by the Towns of Brookhaven and Islip at the initiative of the Long Island Fishermen's Association.
    Keywords: Oceanography ; Marine pollution
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 77
    Publication Date: 2022-05-26
    Description: The Ocean Reference Station at 20°S, 85°W under the stratus clouds west of northern Chile is being maintained to provide ongoing climate-quality records of surface meteorology (air-sea fluxes of heat, freshwater, and momentum), and of upper ocean temperature, salinity, and velocity variability. The Stratus Ocean Reference Station (ORS Stratus) is supported by the National Oceanic and Atmospheric Administration’s (NOAA) Climate Observation Program. It is recovered and redeployed annually, with cruises between October and December. During the October 2007 cruise on the NOAA ship Ronald H. Brown to the ORS Stratus site, the primary activities were recovery of the Stratus 7 WHOI surface mooring that had been deployed in October 2006, deployment of a new (Stratus 8) WHOI surface mooring at that site; in-situ calibration of the buoy meteorological sensors by comparison with instrumentation put on board the ship by staff of the NOAA Earth System Research Laboratory (ESRL); and observations of the stratus clouds and lower atmosphere by NOAA ESRL. Meteorological sensors on a buoy for the Pacific tsunami warning system were also serviced, in collaboration with the Hydrographic and Oceanographic Service of the Chilean Navy (SHOA). The DART (Deep-Ocean Assessment and Reporting of Tsunami) carries IMET sensors and subsurface oceanographic instruments. A new DART II buoy was deployed north of the STRATUS buoy, by personnel from the National Data Buoy Center (NDBC) Argo floats and drifters were launched, and CTD casts carried out during the cruise. The ORS Stratus buoys are equipped with two Improved Meteorological (IMET) systems, which provide surface wind speed and direction, air temperature, relative humidity, barometric pressure, incoming shortwave radiation, incoming longwave radiation, precipitation rate, and sea surface temperature. Additionally, the Stratus 8 buoy received a partial pressure of CO2 detector from the Pacific Marine Environmental Laboratory (PMEL). IMET data are made available in near real time using satellite telemetry. The mooring line carries instruments to measure ocean salinity, temperature, and currents. The ESRL instrumentation used during the 2007 cruise included cloud radar, radiosonde balloons, and sensors for mean and turbulent surface meteorology. Finally, the cruise hosted a teacher participating in NOAA’s Teacher at Sea Program.
    Description: Funding was provided by the National Oceanic and Atmospheric Administration under Grant No. NA17RJ1223 for the Cooperative Institute for Climate and Ocean Research (CICOR).
    Keywords: Marine meteorology ; Oceanography ; Ronald H. Brown (Ship) Cruise RB07-09
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 78
    Publication Date: 2022-05-26
    Description: Originally issued as Reference No. 67-21
    Description: This supplement to Volume I of the Data File, Continental Margin, Atlantic Coast of the United States (Woods Hole Oceanographic Institution Ref. No. 66-8) consists of three parts: 1. Errata for Volume I, 2. New station and sample data added to the file, and 3. Miscellaneous tables of information pertaining to the file. The user is referred to Volume I for explanation of the headings and abbreviations used and for a discussion of the structure of the file.
    Description: Submitted to the U.S. Geological Survey under Contract No. 14-08-0001-8358.
    Keywords: Continental margins ; Oceanography ; United States
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 79
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    Unknown
    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: Originally issued as Reference No. 61-35, series later renamed WHOI-
    Description: The data collected on ATLANTIS Cruise 266 has been tabulated and presented here as an aid to the preparation of rnanuscripts. The Chief Scientist's log is reproduced in narrative form. The current meter, camera, and dredge stations, as well as the continuous seismic profiles, are located and deck notes reproduced. Included are photographs of models of the areas visited.
    Description: Submitted to Bureau of Ships, under Contract NObsr 72521
    Keywords: Atlantis (Ketch : 1931-1966) Cruise 266 ; Oceanography
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 80
    Publication Date: 2022-05-26
    Description: Originally issued as Reference No. 50-48, series later renamed WHOI-.
    Description: Between July 25 and August 7, 1950 the Woods Hole Oceanographic Institution conducted a survey of Great South Bay. The purpose of this study was to attempt to determine the cause of the almost complete cessation of the once prosperous oyster industry. Statistics show that the seed oyster production of the bay declined steadily for ten years prior to 1935 and has subsequently been negligible. The yield of market oysters fell from a maximum of 350,000 bushels in 1929 to 60,000 in 1944 and is now non-existent. Systematic records kept by the oyster companies, notably Bluepoints and Van der Borgh and Sons, provide strong evidence that the failure of oysters to fatten and grow properly is associated with the periodic occurrence in the bay of luxuriant "blooms" of microscopic plants which they have named "small forms" because of their minute size and difficulty of identification. This view is supported by experiments conducted by V. L. Loosanoff and J. B. Engle of the U. S. Fish and Wildlife Service who report that oysters stop feeding in the presence of heavy concentrations of algae. The problem which the investigators were asked to examine was whether evidence could be found that the circulation of water in Great South Bay has altered in such a way as to account for the failure of the oyster industry or whether abnormal chemical conditions arising from pollution or otherwise might provide an alternate or supplementary explanation of the difficulty. The frequent changes in the inlets cutting the beach and particularly the apparent restriction of Fire Island Inlet and the new opening of Moriches Inlet in 1931 suggest that changes in the circulation of water have taken place and have led to various proposals for modifying or supplementing these openings. On the other hand, the duck farms along the tributaries of Bellport and Moriches Bays have increased production substantially during the past twenty years and it has been suspected that pollution resulting from these farms may have provided conditions favorable to the growth of the small form and have thus been responsible for the failure of plantings of market oysters. An examination of records kept by the Coast and Geodetic Survey indicate that the tidal circulation of the bay has been reduced over the years. The change occurred prior to 1930 and thus preceded the decline in oyster production. The results of a survey of the salinity and tidal movement made in 1907-08 for the New York City Water Supply Board, when compared with information obtained last summer, indicate that the change in conditions has been small except in the eastern extremity of the bay. There a most important alteration has taken place. Whereas in 1908 Bellport Bay was relatively fresh, having only 1/3 the salinity of sea water, it now contains about twice as much salt as formerly. This change undoubtedly results from the opening of Moriches Inlet which permits salt water to flow with the rising tide into Bellport Bay from Moriches Bay and Inlet. The opinion is widely held that relatively brackish water is favorable to the production of seed oysters. It is believed, consequently, that the opening of Moriches Inlet may be responsible tor the failure of the seed oyster industry which was formerly centered in Bellport Bay. However, in the greater part of Great South Bay, where formerly market oysters were planted, the change in circulation does not appear to be sufficient to account for the failure of oysters to fatten properly. The results of the chemical studies indicate that the bay water is unusually rich in the products of decomposing organic matter. These materials appear to originate in the tributaries of Moriches Bay and the Carmans River from where they are carried westward across Great South Bay and provide nutriment for the growth of the great population of microscopic plants. These observations point strongly to the duck farms as the source of abnormal conditions in the bay. The survey has thus revealed two conditions which in combination appear to be responsible for the unfavorable conditions affecting the oyster industry. One is the pollution of the bay by wastes from the duck farms which provides nourishment for the great population of microscopic plants, which appear each summer; the other is the local change in circulation occasioned by the opening of Moriches Inlet which has increased the salinity of Bellport Bay. In considering remedial measures both these conditions should be taken into account. Since the state of pollution depends on the balance between the rate at which pollutants are added and their removal by the circulation of water, the conditions might be improved by enlarging the inlets or cutting new openings designed to increase the flushing of the bay. To be effective these engineering works would be prohibitively expensive and their effectiveness and permanence would be uncertain. In addition, they would not restore the low salinity of the eastern end of Great South Bay which appears to favor seed oyster production. A second alternative is to reduce the pollution at its source by preventing the wastes from the duck farms from reaching the water. The manure might become a valuable by-product of the farms if procedures were developed for using it for fertilizer. Even it such procedures did not yield a profit, they might at least pay the costs of preventing pollution. While this expedient might be expected to improve the conditions in the bay as a whole and thus might lead to a restoration of market oyster production, it would not restore the low salinity of Bellport Bay, on which the seed oyster production supposedly depended, unless Moriches Inlet were to be permanently closed. It this were done, the conditions in Great South Bay might be expected to be restored to very nearly those obtaining prior to 1930. A third alternative, which has much to commend it, is to prevent the exchange of water between Great South Bay and Moriches Bay. If this were accomplished the wastes from most of the duck farms would be prevented from reaching Great south Bay. In addition, the waters of Bellport Bay might be expected to become much fresher and the conditions would favor the restoration of seed oyster production in that area. Inasmuch as it is now proposed to bridge the narrows at Smith Point to provide a roadway to Great South Beach, it is suggested that at reasonable additional expense the opening might be filled completely except for a lock for the passage of boats along the intercoastal waterway. Such construction would eliminate, or place under control, the movement of water between the bays and should lead toward a restoration of the conditions required for the production of both market and seed oysters. While this method of improving the conditions, appears to be the most practical one, it should be realized that it would require either the maintenance of Moriches Inlet as an effective opening or the correction of the pollution of Moriches Bay, since otherwise the isolation of Moriches Bay from the ocean would lead to intolerable conditions.
    Keywords: Oceanography ; Oysters
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 81
    Publication Date: 2008-06-27
    Description: Roughly 60% of the Earth's outer surface is composed of oceanic crust formed by volcanic processes at mid-ocean ridges. Although only a small fraction of this vast volcanic terrain has been visually surveyed or sampled, the available evidence suggests that explosive eruptions are rare on mid-ocean ridges, particularly at depths below the critical point for seawater (3,000 m). A pyroclastic deposit has never been observed on the sea floor below 3,000 m, presumably because the volatile content of mid-ocean-ridge basalts is generally too low to produce the gas fractions required for fragmenting a magma at such high hydrostatic pressure. We employed new deep submergence technologies during an International Polar Year expedition to the Gakkel ridge in the Arctic Basin at 85 degrees E, to acquire photographic and video images of 'zero-age' volcanic terrain on this remote, ice-covered ridge. Here we present images revealing that the axial valley at 4,000 m water depth is blanketed with unconsolidated pyroclastic deposits, including bubble wall fragments (limu o Pele), covering a large (〉10 km(2)) area. At least 13.5 wt% CO(2) is necessary to fragment magma at these depths, which is about tenfold the highest values previously measured in a mid-ocean-ridge basalt. These observations raise important questions about the accumulation and discharge of magmatic volatiles at ultraslow spreading rates on the Gakkel ridge and demonstrate that large-scale pyroclastic activity is possible along even the deepest portions of the global mid-ocean ridge volcanic system.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Sohn, Robert A -- Willis, Claire -- Humphris, Susan -- Shank, Timothy M -- Singh, Hanumant -- Edmonds, Henrietta N -- Kunz, Clayton -- Hedman, Ulf -- Helmke, Elisabeth -- Jakuba, Michael -- Liljebladh, Bengt -- Linder, Julia -- Murphy, Christopher -- Nakamura, Ko-Ichi -- Sato, Taichi -- Schlindwein, Vera -- Stranne, Christian -- Tausenfreund, Maria -- Upchurch, Lucia -- Winsor, Peter -- Jakobsson, Martin -- Soule, Adam -- England -- Nature. 2008 Jun 26;453(7199):1236-8. doi: 10.1038/nature07075.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA. rsohn@whoi.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18580949" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Arctic Regions ; Geography ; Oceanography ; Oceans and Seas ; Porifera ; Seawater ; Volcanic Eruptions/*statistics & numerical data
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 82
    facet.materialart.
    Unknown
    Nature Publishing Group (NPG)
    Publication Date: 2008-03-07
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Schrope, Mark -- England -- Nature. 2008 Mar 6;452(7183):24-6. doi: 10.1038/452024a.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18322500" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Dinoflagellida/*growth & development/metabolism ; *Ecosystem ; Eutrophication/*physiology ; Florida ; Nitrogen/metabolism ; Oceanography
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 83
    facet.materialart.
    Unknown
    American Association for the Advancement of Science (AAAS)
    Publication Date: 2008-11-22
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Enserink, Martin -- New York, N.Y. -- Science. 2008 Nov 21;322(5905):1184-5. doi: 10.1126/science.322.5905.1184.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/19023058" target="_blank"〉PubMed〈/a〉
    Keywords: Academies and Institutes/economics/*history ; Biology ; History, 20th Century ; Pathology ; Romania
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 84
    Publication Date: 2008-03-22
    Description: Minerals are more complex than previously thought because of the discovery that their chemical properties vary as a function of particle size when smaller, in at least one dimension, than a few nanometers, to perhaps as much as several tens of nanometers. These variations are most likely due, at least in part, to differences in surface and near-surface atomic structure, as well as crystal shape and surface topography as a function of size in this smallest of size regimes. It has now been established that these variations may make a difference in important geochemical and biogeochemical reactions and kinetics. This recognition is broadening and enriching our view of how minerals influence the hydrosphere, pedosphere, biosphere, and atmosphere.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Hochella, Michael F Jr -- Lower, Steven K -- Maurice, Patricia A -- Penn, R Lee -- Sahai, Nita -- Sparks, Donald L -- Twining, Benjamin S -- New York, N.Y. -- Science. 2008 Mar 21;319(5870):1631-5. doi: 10.1126/science.1141134.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Center for NanoBioEarth, Department of Geosciences, Virginia Polytechnic Institute and State University (Virginia Tech), Blacksburg, VA 24061-0420, USA. hochella@vt.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18356515" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere ; Biology ; Geologic Sediments/chemistry ; Humans ; *Minerals/chemistry/metabolism ; *Nanoparticles ; Oceans and Seas ; Particle Size ; Solubility ; Thermodynamics
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 85
    Publication Date: 2008-07-05
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Schaefer, Mark -- Baker, D James -- Gibbons, John H -- Groat, Charles G -- Kennedy, Donald -- Kennel, Charles F -- Rejeski, David -- New York, N.Y. -- Science. 2008 Jul 4;321(5885):44-5. doi: 10.1126/science.1160192.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18599760" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Atmosphere ; Biodiversity ; Conservation of Natural Resources ; Ecology ; Fresh Water ; Geological Phenomena ; Geology ; Oceanography ; Oceans and Seas ; *Public Policy ; United States ; United States Government Agencies/*organization & administration
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 86
    Publication Date: 2018-06-11
    Description: We demonstrate that sea ice motion in summer can be derived reliably from the 18GHz channel of the AMSR-E instrument on the EOS Aqua platform. The improved spatial resolution of this channel with its lower sensitivity to atmospheric moisture seems to have alleviated various issues that have plagued summer motion retrievals from shorter wavelength observations. Two spatial filters improve retrieval quality: one reduces some of the microwave signatures associated with synoptic-scale weather systems and the other removes outliers. Compared with daily buoy drifts, uncertainties in motion are approx.3-4 km/day. Using the daily motion fields, we examine five years of summer ice area exchange between the Pacific and Atlantic sectors of the Arctic Ocean. With the sea-level pressure patterns during the summer of 2006 and 2007 favoring the export of sea ice into the Atlantic Sector, the regional outflow is approx.21% and approx.15% of the total sea ice retreat in the Pacific sector.
    Keywords: Oceanography
    Type: Geophysical Research Letters; Volume 35
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  • 87
    Publication Date: 2018-06-12
    Description: High- and low-resolution sea surface temperature (SST) analysis products are used to initialize the Weather Research and Forecasting (WRF) Model for May 2004 for short-term forecasts over Florida and surrounding waters. Initial and boundary conditions for the simulations were provided by a combination of observations, large-scale model output, and analysis products. The impact of using a 1-km Moderate Resolution Imaging Spectroradiometer (MODIS) SST composite on subsequent evolution of the marine atmospheric boundary layer (MABL) is assessed through simulation comparisons and limited validation. Model results are presented for individual simulations, as well as for aggregates of easterly- and westerly-dominated low-level flows. The simulation comparisons show that the use of MODIS SST composites results in enhanced convergence zones. earlier and more intense horizontal convective rolls. and an increase in precipitation as well as a change in precipitation location. Validation of 10-m winds with buoys shows a slight improvement in wind speed. The most significant results of this study are that 1) vertical wind stress divergence and pressure gradient accelerations across the Florida Current region vary in importance as a function of flow direction and stability and 2) the warmer Florida Current in the MODIS product transports heat vertically and downwind of this heat source, modifying the thermal structure and the MABL wind field primarily through pressure gradient adjustments.
    Keywords: Oceanography
    Type: Monthly Weather Review; Volume 136; Issue 4; 1349-1372
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  • 88
    Publication Date: 2018-06-06
    Description: Analysis of Arctic sea ice extents derived from satellite passive-microwave data for the 28 years, 1979-2006 yields an overall negative trend of -45,100 +/- 4,600 km2/yr (-3.7 +/- 0.4%/decade) in the yearly averages, with negative ice-extent trends also occurring for each of the four seasons and each of the 12 months. For the yearly averages the largest decreases occur in the Kara and Barents Seas and the Arctic Ocean, with linear least squares slopes of -10,600 +/- 2,800 km2/yr (-7.4 +/- 2.0%/decade) and -10,100 +/- 2,200 km2/yr (-1.5 +/- 0.3%/decade), respectively, followed by Baffin Bay/Labrador Sea, with a slope of -8,000 +/- 2,000 km2/yr) -9.0 +/- 2.3%/decade), the Greenland Sea, with a slope of -7,000 +/- 1,400 km2/yr (-9.3 +/- 1.9%/decade), and Hudson Bay, with a slope of -4,500 +/- 900 km2/yr (-5.3 +/- 1.1%/decade). These are all statistically significant decreases at a 99% confidence level. The Seas of Okhotsk and Japan also have a statistically significant ice decrease, although at a 95% confidence level, and the three remaining regions, the Bering Sea, Canadian Archipelago, and Gulf of St. Lawrence, have negative slopes that are not statistically significant. The 28-year trends in ice areas for the Northern Hemisphere total are also statistically significant and negative in each season, each month, and for the yearly averages.
    Keywords: Oceanography
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  • 89
    Publication Date: 2018-06-06
    Description: There is growing recognition that rigorous skill assessment is required to understand the ability of ocean biological models to represent ocean processes and distributions. Statistical analysis of model results with observations represents the most quantitative form of skill assessment, and this principle serves as well for data assimilation models. However, skill assessment for data assimilation requires special consideration. This is because there are three sets of information in the free-run model, data, and the assimilation model, which uses Data assimilation information from both the flee-run model and the data. Intercom parison of results among the three sets of information is important and useful for assessment, but is not conclusive since the three information sets are intertwined. An independent data set is necessary for an objective determination. Other useful measures of ocean biological data assimilation assessment include responses of unassimilated variables to the data assimilation, performance outside the prescribed region/time of interest, forecasting, and trend analysis. Examples of each approach from the literature are provided. A comprehensive list of ocean biological data assimilation and their applications of skill assessment, in both ecosystem/biogeochemical and fisheries efforts, is summarized.
    Keywords: Oceanography
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  • 90
    Publication Date: 2018-06-06
    Description: The dynamical state of the ocean and atmosphere is taken to be a large dimensional random vector in a range of large-scale computational applications, including data assimilation, ensemble prediction, sensitivity analysis, and predictability studies. In each of these applications, numerical evolution of the covariance matrix of the random state plays a central role, because this matrix is used to quantify uncertainty in the state of the dynamical system. Since atmospheric and ocean dynamics are nonlinear, there is no closed evolution equation for the covariance matrix, nor for the mean state. Therefore approximate evolution equations must be used. This article studies theoretical properties of the evolution equations for the mean state and covariance matrix that arise in the second-moment closure approximation (third- and higher-order moment discard). This approximation was introduced by EPSTEIN [1969] in an early effort to introduce a stochastic element into deterministic weather forecasting, and was studied further by FLEMING [1971a,b], EPSTEIN and PITCHER [1972], and PITCHER [1977], also in the context of atmospheric predictability. It has since fallen into disuse, with a simpler one being used in current large-scale applications. The theoretical results of this article make a case that this approximation should be reconsidered for use in large-scale applications, however, because the second moment closure equations possess a property of energetic consistency that the approximate equations now in common use do not possess. A number of properties of solutions of the second-moment closure equations that result from this energetic consistency will be established.
    Keywords: Oceanography
    Type: Prepared for Handbook of Numerical Analysis: Special Volume on Computational Methods for the Ocean and the Atmosphere, R. Temam and J. Tribbia, eds., Elsevier
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  • 91
    Publication Date: 2018-06-11
    Description: A three-dimensional variational data assimilation scheme for the Regional Ocean Modeling System (ROMS), named ROMS3DVAR, has been described in the work of Li et al. (2008). In this paper, ROMS3DVAR is applied to the central California coastal region, an area characterized by inhomogeneity and anisotropy, as well as by dynamically unbalanced flows. A method for estimating the model error variances from limited observations is presented, and the construction of the inhomogeneous and anisotropic error correlations based on the Kronecker product is demonstrated. A set of single observation experiments illustrates the inhomogeneous and anisotropic error correlations and weak dynamic constraints used. Results are presented from the assimilation of data gathered during the Autonomous Ocean Sampling Network (AOSN) experiment during August 2003. The results show that ROMS3DVAR is capable of reproducing complex flows associated with upwelling and relaxation, as well as the rapid transitions between them. Some difficulties encountered during the experiment are also discussed.
    Keywords: Oceanography
    Type: Journal Of Geophysical Research; Volume 113
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  • 92
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    Unknown
    In:  Other Sources
    Publication Date: 2019-07-19
    Description: In situ time series observations have provided a multi-decadal view of long-term changes in ocean biology. These observations are sufficiently reliable to enable discernment of even relatively small changes, and provide continuous information on a host of variables. Their key drawback is their limited domain. Satellite observations from ocean color sensors do not suffer the drawback of domain, and simultaneously view the global oceans. This attribute lends credence to their use in global and regional model validation and data assimilation. We focus on these applications using the NASA Ocean Biogeochemical Model. The enhancement of the satellite data using data assimilation is featured and the limitation of tongterm satellite data sets is also discussed.
    Keywords: Oceanography
    Type: Ocean Carbon and Biogeochemistry Summer Science Workshop; Jul 21, 2008 - Jul 24, 2008; Massachusetts; United States
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  • 93
    Publication Date: 2019-07-19
    Description: The Rapid Prototyping Capability (RPC) node at NASA Stennis Space Center, MS, was used to simulate NASA next-generation sensor imagery over well-known coral reef areas: Looe Key, FL, and Kaneohe Bay, HI. The objective was to assess the degree to which next-generation sensor systems-the Visible/Infrared Imager/Radiometer Suite (VIIRS) and the Landsat Data Continuity Mission (LDCM)- might provide key input to the National Oceanographic and Atmospheric Administration (NOAA) Integrated Coral Observing Network (ICON)/Coral Reef Early Warning System (CREWS) Decision Support Tool (DST). The DST data layers produced from the simulated imagery concerned water quality and benthic classification map layers. The water optical parameters of interest were chlorophyll (Chl) and the absorption coefficient (a). The input imagery used by the RPC for simulation included spaceborne (Hyperion) and airborne (AVIRIS) hyperspectral data. Specific field data to complement and aid in validation of the overflight data was used when available. The results of the experiment show that the next-generation sensor systems are capable of providing valuable data layer resources to NOAA s ICON/CREWS DST.
    Keywords: Oceanography
    Type: SSTI-2220-0128 , 2008 Ocean Sciences Meeting; Mar 02, 2008 - Mar 07, 2008; Orlando, Fl; United States
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  • 94
    Publication Date: 2019-07-19
    Description: The Ocean Color component of the Aerosol Robotic Network (AERONET-OC) has been implemented to support long-term satellite ocean color investigations through cross-site consistent and accurate measurements collected by autonomous radiometer systems deployed on offshore fixed platforms. The ultimate purpose of AERONET-OC is the production of standardized measurements performed at different sites with identical measuring systems and protocols, calibrated using a single reference source and method, and processed with the same code. The AERONET-OC primary data product is the normalized water leaving radiance determined at center-wavelengths of interest for satellite ocean color applications, with an uncertainty lower than 5% in the blue-green spectral regions and higher than 8% in the red. Measurements collected at 6 sites counting the northern Adriatic Sea, the Baltic Proper, the Gulf of Finland, the Persian Gulf, and, the northern and southern margins of the Middle Atlantic Bay, have shown the capability of producing quality assured data over a wide range of bio-optical conditions including Case-2 yellow substance- and sedimentdominated waters. This work briefly introduces network elements like: deployment sites, measurement method, instrument calibration, processing scheme, quality-assurance, uncertainties, data archive and products accessibility. Emphases is given to those elements which underline the network strengths (i.e., mostly standardization of any network element) and its weaknesses (i.e., the use of consolidated, but old-fashioned technology). The work also addresses the application of AERONET-OC data to the validation of primary satellite radiometric products over a variety of complex coastal waters and finally provides elements for the identification of new deployment sites most suitable to support satellite ocean color missions.
    Keywords: Oceanography
    Type: Ocean Optics 19th; Oct 06, 2008 - Oct 10, 2008; Tuscany; Italy
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  • 95
    Publication Date: 2019-07-19
    Description: Ocean surface turbulent and radiative fluxes are critical links in the climate system since they mediate energy exchange between the two fluid systems (ocean and atmosphere) whose combined heat transport determines the basic character of Earth's climate. Moreover, interannual to decadal climate variability depends crucially on the nature of these exchange processes. For example, addressing the question of the degree to which the global hydrologic cycle is changing depends on our ability to observe and model these fluxes accurately. In this work we investigate the interannual to decadal variation of fluxes over the global tropics, especially the tropical oceans. Recent versions of satellite-derived fresh water flux estimates as well as some reanalyses (e.g. products from Remote Sensing Systems, the Woods Hole Oceanographic Institute, and Global Precipitation Climatology Project) suggest that increases in evaporation and precipitation over the past 20 years exceed those expected on the basis of climate model projected responses to greenhouse gas forcing. At the same time, it is well known that E1 Nino / Southern Oscillation behavior in the Pacific exhibits significant variability at scales longer than interannual. We examine here the degree to which surface fluxes attending these interannual to decadal fluctuations are related to ENSO. We examine consistency between these data sets and explore relationships between SST variations, flux changes and modulation of tropical Walker and Hadley circulations.
    Keywords: Oceanography
    Type: Spring American Geophysical Union Meeting; May 27, 2008 - May 30, 2008; Fort Lauderdale, Fl; United States
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  • 96
    Publication Date: 2019-08-26
    Description: The authors investigate the nature of the interannual variability of the meridional overturning circulation (MOC) of the North Atlantic Ocean using an Estimating the Circulation and Climate of the Ocean (ECCO) assimilation product for the period of 1993-2003. The time series of the first empirical orthogonal function of the MOC is found to be correlated with the North Atlantic Oscillation (NAO) index, while the associated circulation anomalies correspond to cells extending over the full ocean depth. Model sensitivity experiments suggest that the wind is responsible for most of this interannual variability, at least south of 40(deg)N. A dynamical decomposition of the meridional streamfunction allows a further look into the mechanisms. In particular, the contributions associated with 1) the Ekman flow and its depth-independent compensation, 2) the vertical shear flow, and 3) the barotropic gyre flowing over zonally varying topography are examined. Ekman processes are found to dominate the shorter time scales (1.5-3 yr), while for longer time scales (3-10 yr) the MOC variations associated with vertical shear flow are of greater importance. The latter is primarily caused by heaving of the pycnocline in the western subtropics associated with the stronger wind forcing. Finally, how these changes in the MOC affect the meridional heat transport (MHT) is examined. It is found that overall, Ekman processes explain a larger part of interannual variability (3-10 yr) for MHT (57%) than for the MOC (33%).
    Keywords: Oceanography
    Type: Journal of Physical Oceanography; 38; 2; 467-480
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  • 97
    Publication Date: 2019-07-13
    Description: Coral reefs are some of the most biologically rich and economically important ecosystems on Earth. Coral reefs are Earth's largest biological structures and have taken thousands of years to form. Coral reefs not only provide important habitat for many marine animals and plants, but they also provide humanity with food, jobs, chemicals, protection against storms, and life-saving pharmaceuticals. Severe bleaching events have occurred that have dramatic long-term ecological impacts to corals, including loss of reef-building corals, changes in benthic habitat, and, in some cases, changes in larval fish populations (Holden and Ledrew, 1998). Some researchers suggest that 10 percent of Earth s coral reefs have already been destroyed and that another 60 percent are in danger. Scientists have proposed that as much as 95 percent of Jamaica's reefs are dying or dead. This poster reports on a Rapid Prototyping Capability (RPC) experiment done to determine whether future NASA sensors - the Visible/Infrared Imager/Radiometer Suite (VIIRS) and Landsat Data Continuity Mission (LDCM) - could generate key data products for the Integrated Coral Reef Observation Network (ICON)/Coral Reef Early Warning System (CREWS) Decision Support Tool (DST) operated by the National Oceanic and Atmospheric Administration (NOAA).
    Keywords: Oceanography
    Type: SSTI-2220-0137 , 11th International Coral Reef Symposium (Poster); Jul 07, 2008 - Jul 11, 2008; Fort Lauderdale, FL; United States
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  • 98
    Publication Date: 2019-07-13
    Description: Knowledge of global oceanic tides has markedly advanced over the last two decades, in no small part because of the near-global measurements provided by satellite altimeters, and especially the long and precise Topex/Poseidon time series e.g. [2]. Satellite altimetry in turn places very severe demands on the accuracy of tidal models. The reason is clear: tides are by far the largest contributor to the variance of sea-surface elevation, so any study of non-tidal ocean signals requires removal of this dominant tidal component. Efforts toward improving models for altimetric tide corrections have understandably focused on deep-water, open-ocean regions. These efforts have produced models thought to be generally accurate to about 2 cm rms. Corresponding tide predictions in shelf and near-coastal regions, however, are far less accurate. This paper discusses the status of our current abilities to provide near-global tidal predictions in shelf and near-coastal waters, highlights some of the difficulties that must be overcome, and attempts to divine a path toward some degree of progress. There are, of course, many groups worldwide who model tides over fairly localized shallow-water regions, and such work is extremely valuable for any altimeter study limited to those regions, but this paper considers the more global models necessary for the general user. There have indeed been efforts to patch local and global models together, but such work is difficult to maintain over many updates and can often encounter problems of proprietary or political nature. Such a path, however, might yet prove the most fruitful, and there are now new plans afoot to try again. As is well known, tides in shallow waters tend to be large, possibly nonlinear, and high wavenumber. The short spatial scales mean that current mapping capabilities with (multiple) nadir-oriented altimeters often yield inadequate coverage. This necessitates added reliance on numerical hydrodynamic models and data assimilation, which in turn necessitates very accurate bathymetry with high spatial resolution. Nonlinearity means that many additional compound tides and overtides must be accounted for in our predictions, which increases the degree of modeling effort and increases the amounts of data required to disentangle closely aliased tides.
    Keywords: Oceanography
    Type: IGARRS 2008; Jul 09, 2008; Boston, MA; United States
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  • 99
    Publication Date: 2019-07-13
    Description: Forecasting atmospheric and oceanic circulations accurately over the Eastern Mediterranean has proved to be an exceptional challenge. The existence of fine-scale topographic variability (land/sea coverage) and seasonal dynamics variations can create strong spatial gradients in temperature, wind and other state variables, which numerical models may have difficulty capturing. The Hellenic Center for Marine Research (HCMR) is one of the main operational centers for wave forecasting in the eastern Mediterranean. Currently, HCMR's operational numerical weather/ocean prediction model is based on the coupled Eta/Princeton Ocean Model (POM). Since 1999, HCMR has also operated the POSEIDON floating buoys as a means of state-of-the-art, real-time observations of several oceanic and surface atmospheric variables. This study attempts a first assessment at improving both atmospheric and oceanic prediction by initializing a regional Numerical Weather Prediction (NWP) model with high-resolution sea surface temperatures (SST) from remotely sensed platforms in order to capture the small-scale characteristics.
    Keywords: Oceanography
    Type: AMS 88th Annual Meeting; Jan 20, 2008 - Jan 24, 2008; New Orleans, LA; United States
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  • 100
    Publication Date: 2019-07-12
    Description: An apparatus is being developed for sampling water for signs of microbial life in an ocean hydrothermal vent at a depth of as much as 6.5 km. Heretofore, evidence of microbial life in deep-sea hydrothermal vents has been elusive and difficult to validate. Because of the extreme conditions in these environments (high pressures and temperatures often in excess of 300 C), deep-sea hydrothermal- vent samplers must be robust. Because of the presumed low density of biomass of these environments, samplers must be capable of collecting water samples of significant volume. It is also essential to prevent contamination of samples by microbes entrained from surrounding waters. Prior to the development of the present apparatus, no sampling device was capable of satisfying these requirements. The apparatus (see figure) includes an intake equipped with a temperature probe, plus several other temperature probes located away from the intake. The readings from the temperature probes are utilized in conjunction with readings from flowmeters to determine the position of the intake relative to the hydrothermal plume and, thereby, to position the intake to sample directly from the plume. Because it is necessary to collect large samples of water in order to obtain sufficient microbial biomass but it is not practical to retain all the water from the samples, four filter arrays are used to concentrate the microbial biomass (which is assumed to consist of particles larger than 0.2 m) into smaller volumes. The apparatus can collect multiple samples per dive and is designed to process a total volume of 10 L of vent fluid, of which most passes through the filters, leaving a total possibly-microbe-containing sample volume of 200 mL remaining in filters. A rigid titanium nose at the intake is used for cooling the sample water before it enters a flexible inlet hose connected to a pump. As the water passes through the titanium nose, it must be cooled to a temperature that is above a mineral-precipitation temperature of 100 C but below the upper working temperature (230 C) of switching valves and tubes in the apparatus. The sample water then passes into a manifold tube, from whence the switching valves can direct the water through either a bypass tube or any one of the filter arrays, without contamination from a previous sample. Each filter array consists of series of filters having pore sizes decreasing in the direction of flow: 90-, 60-, 15-, and 7-micron prefilters and a large-surface-area 0.2-micron collection filter. All the filter taps are located between the intake and the bypass tube so that each time the bypass tube is used, the entire manifold tube is flushed as well.
    Keywords: Oceanography
    Type: NPO-42617 , NASA Tech Briefs, November 2008; 23
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