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419 results for “offshoring”
Dataset from Annual Acoustic Presence of Fin Whale (Balaenoptera physalus) Offshore Eastern Sicily, Central Mediterranean Sea
<p>This dataset is form the study: </p> <p>Sciacca V., Caruso F.,Beranzoli L., Chierici F., De Domenico E., Embriaco D., Favali P., Giovanetti G., Larosa G., Marinaro G., Papale E., Pavan G., Pellegrino C., Pulvirenti S., Simeone F., Viola S., and G. Riccobene. "Annual Acoustic Presence of Fin Whale (<em>Balaenoptera physalus</em>) Offshore Eastern Sicily, Central Mediterranean Sea." PLoS ONE 10(11): e0141838. doi:10.1371/journal.pone.0141838</p> <p>The archives labeled YYYYMM_Spectrograms.zip contain the data from each month of passive acoustic recording -MM- of the years -YYYY- 2012 and 2013. Data consist of the spectrograms (1-50 Hz) of 10-min audio recordings, in PNG format files. These data were used in the cited study to verify the presence of fin whale calls.</p> <p>The archive labeled "NoiseData.zip" consists of two matrix (ASCII format) containing the recorded values of acoustic noise within the fin whale call frequency band.</p> <p> </p> <p> </p>
Source data for "Halving the North Sea's offshore wind energy carbon footprint"
<p>This dataset provides source data for the paper "Halving the North Sea’s offshore wind energy carbon footprint". It contains basic geographical factors, including wind speed, water depth, and distance from shore, and environmental impact intensities, including steel, Cu, and Al use, climate change, marine ecotoxicity, and marine eutrophication impacts. For more details, please refer to https://pubs.acs.org/doi/full/10.1021/acs.est.2c02183 and https://www.sciencedirect.com/science/article/pii/S1364032122004993. </p>
Hexametafosfato de Sodio (SHMP) como Inhibidor de Incrustaciones de Carbonato de Calcio en la Producción de Petróleo Offshore
<p>La investigación propone el uso de hexametafosfato de sodio (SHMP) para inhibir la formación de incrustaciones de carbonato de calcio en líneas de producción de petróleo offshore. Se realizaron experimentos en un sistema en loop, en presencia y ausencia de SHMP y asi comparar la cantidad de incrustación acumulada en un cuerpo de prueba. Los resultados de masa depositada fueron comparados a su vez con predicciones de incrustación. Además, el proceso de incrustación fue seguido a través de cambios de temperatura e imágenes infrarrojas. Finalmente, los resultados arrojaron que la presencia de SHMP si afecta la formación de incrustaciones de carbonato de calcio.</p>
Exploring Gaussian processes for short-term forecasting in offshore energy systems: Supplementary material
<p>Two supplementary videos are provided. The first video analyses the performance of wave excitation force forecasting across different horizons in a noise-free case. The second video examines the impact of noise on the forecast. Both videos include results from a Gaussian-based forecaster, an AR forecaster, and show the uncertainty bounds provided by the Gaussian forecaster. The variable analysed and forecasted in these videos is the wave excitation force.</p>
Imaging the sediment cover offshore central Chile with surface-wave dispersion and P-wave conversion using DAS
<p>This repository contains codes and data used to reproduce the figures in the paper <em>Vernet, C. et al, "Imaging the sediment cover offshore central Chile with surface-wave dispersion and P-wave conversion using distributed acoustic sensing", 2025, (<a href="https://doi.org/10.1029/2024JB030507">https://doi.org/10.1029/2024JB030507</a>).</em></p>
Side scan sonar backscatter mosaic offshore Thailand, Andaman Sea
<p>The attached mosaics of side scan sonar data were recorded during 3 field campaigns in 2007, 2008 and 2010. High backscatter values are represented by darker colours. The mosaic is georeferenced in EPSG:32647 - WGS 84 / UTM zone 47N.</p> <p>Please refer to Feldens, P.; Schwarzer, K.; Sakuna, D.; Szczuciński, W.; Sompongchaiyakul, P. Sediment distribution on the inner continental shelf off Khao Lak (Thailand) after the 2004 Indian Ocean tsunami. <em>Earth, Planets and Space,</em> 2012, 64, 875-887; DOI:10.5047/eps.2011.09.001 and Sakuna-Schwartz, D.; Feldens, P.; Schwarzer, K.; Khokiattiwong, S.; Stattegger, K. Internal structure of event layers preserved on the Andaman Sea continental shelf, Thailand: tsunami vs. storm and flash-flood deposits. <em>Natural Hazards and Earth System Sciences,</em> 2015, 15, 1181-1199; DOI:10.5194/nhess-15-1181-201 and Feldens, P., Schwarzer K., Sakuna-Schwartz, D., Khokiattiwong, S. (in prep) Offshore geomorphological evolution in Phang Nga province (Thailand) during the Holocene: An example for a sediment starving shelf and references therein for further information on the dataset. </p> <p>The research was funded by Deutsche Forschungsgemeinschaft (DFG) grant No. SCHW 572/11-1 and National Research Council of Thailand (NRCT)</p>
Balancing profitability of energy production, societal impacts and biodiversity in offshore wind farm design
<p>Dataset related to the article: Virtanen, E.A., Lappalainen, J., Nurmi, M., Viitasalo, M., Tikanmäki, M., Heinonen, J., Atlaskin, E., Kallasvuo, M., Tikkanen, H., Moilanen, A. (2022) Balancing profitability of energy production, societal impacts and biodiversity in offshore wind farm design. Renewable and Sustainable Energy Reviews 158, 112087.</p> <p>Dataset includes suitability maps for offshore windfarms, where priority values are scaled between 0-1 (note the reversed value scale): analysis solution (A) economy, (B) society, (C) biodiversity, (D) restrictions, (E) A+B+C without restrictions and (F) A+B+C with restrictions. Dataset includes also the conflict map (and R script), where each three main solutions (A, B, C) are mapped onto an RGB color composite map. </p> <p>Additional details can be found from the published article: <a href="https://doi.org/10.1016/j.rser.2022.112087">https://doi.org/10.1016/j.rser.2022.112087</a></p>
Reef effect of offshore structures on the occurrence and foraging activity of harbour porpoises
<p class="MsoNormal">With increasing numbers of offshore structures to be decommissioned, a better understanding of their effect on marine predators is timely. There is some evidence that oil and gas platforms may attract marine mammals acting as artificial reefs. However, it is unclear whether different man-made structure designs have similar effects. Further, due to the lack of baseline data prior to installation, it is unknown whether artificial structures modify the diel patterns of occurrence and foraging behaviour of marine mammals. Here, we used passive acoustics to investigate the occurrence and foraging activity of harbour porpoises (<em>Phocoena phocoena</em>) around three artificial structures of different age and complexity. We deployed an array of echolocation click detectors (CPODs) in 2021, along a gradient of distances to these structures and assessed the extent to which porpoises were attracted to them. We also investigated the effect of these structures on the diel patterns of occurrence and foraging activity of porpoises. The probability of porpoise occurrence and foraging activity decreased with distance from offshore structures. A significant increase in porpoise occurrence and foraging was detected during night-time compared to daytime around all three offshore structures (< 200 m). Comparing pre- and post-installation porpoise detections, the daily patterns of occurrence and foraging activity shifted from a weak <a>diel</a><span class="MsoCommentReference"><span> </span></span>pattern before the structure was installed, to a strong nocturnal pattern when the structure was present. These findings provide evidence that marine mammals are attracted to man-made structures and that porpoises modify their diel patterns of occurrence and foraging activity around them. This research suggests that offshore structures play an important role as foraging areas for marine mammals and provides key information for the decommissioning process.</p>
Greigite formation modulated by turbidites and bioturbation in deep-sea sediments offshore Sumatra
<p>This repository contains the rock magnetic and paleomagnetic data, TOC and TN data, and XRD spectra data associated with the research paper titled "Greigite formation modulated by turbidites and bioturbation in deep-sea sediments offshore Sumatra" by Yang et al. published in Journal of Geophysical Research: Solid Earth, Volume127, Issue11, e2022JB024734, https://doi.org/10.1029/2022JB024734</p>
Wind shadows from U.S. east coast offshore wind energy lease areas.
<p>Georeferenced data layers describing whole wind farm wakes (wind shadows) for use in planning and development along the U.S. east coast based on WRF simulations performed using the accompanying namelist. Full details of the analysis are provided in: Pryor and Barthelmie: Wind shadows impact planning of large offshore wind farms</p> <p> </p> <p>This work is supported by the U.S. Department of Energy (DoE) (DE-SC0016605). The research used computing resources from the National Science Foundation: Extreme Science and Engineering Discovery Environment (XSEDE) (allocation award to SCP is TG-ATM170024) and National Energy Research Scientific Computing Center, a DOE Office of Science User Facility supported by the Office of Science of the U.S. Department of Energy under Contract No. DE-AC02-05CH11231.</p>
FIGURE 2. Offshore Operations. A in Deep-Sea Octocoral Biodiversity Surveys in Central California
FIGURE 2. Offshore Operations. A. Scientific staff on board FSV Bell M. Shimada with the MARE ROV, "Beagle", August 2018. B. The ROV "Hercules" on board E/V Nautilus. C. The manipulator arm of the ROV "Hercules" on the E/V Nautilus, collecting branches of the bamboo coral, Keratosis sp. D. The E/V Nautilus at harbor, San Francisco. E. Bow of the E/V Nautilus approaching the Golden Gate. F. The CBNMS ROV on board R/V Fulmar. Photograph 2C courtesy OET and NOAA.
Fig. 7 in A new neolepadid cirripede from a Pleistocene cold seep, Krishna-Godavari Basin, offshore India
Fig. 7. Cladogram of relationships between Neolepadidae, Pedupycnolepas and Etcheslepas, using heuristic unconstrained analysis optimised to deltran and based on characters listed in Table 1. Values are for Bremer support/bootstrap.
Fig. 6 in A new neolepadid cirripede from a Pleistocene cold seep, Krishna-Godavari Basin, offshore India
Fig. 6. Comparative morphology (capitula in lateral view) of neolepadids and other genera of pedunculated thoracicans. A. Etcheslepas durotrigensis Gale, 2014; Tithonian (Upper Jurassic), UK. B. Pedupycnolepas articulata (Collins, 1980); Aptian (Lower Cretacous), Antarctica. C. Ashinkailepas seepiophila Yamaguchi, Newman, and Hashimoto, 2004; Recent, Japan. D. Leucolepas longa Southward and Jones, 2003; Recent, Pacific. E. Neolepas zevinae Newman, 1979; Recent, Pacific. F. Vulcanolepas osheai Buckeridge, 2000; Recent, New Zealand. G. Litholepas klausreschi Nagler, Haug, Glenner, and Buckeridge, 2017; Tithonian (Upper Jurassic), Germany. H. Pycnolepas rigida (Sowerby, 1836); Albian (Lower Cretaceous), UK. I. Stipilepas molerensis Carriol in Carriol et al., 2016; Eocene of Denmark.
Fig. 5 in A new neolepadid cirripede from a Pleistocene cold seep, Krishna-Godavari Basin, offshore India
Fig. 5. Comparative morphology of neolepadid cirripede Ashinkailepas indica Gale sp. nov. (A, D, G) from Late Pleistocene, Krishna-Godavari Basin, off shore India, and other cirripedes. A. NHMUK IC 1412, paratype, scutum. D. NHMUK IC 1410, paratype, tergum. G. NHMUK IC 1404, paratype, upper latus. B, C, F. Brachylepadid Pycnolepas rígida (J. de C. Sowerby, 1836) from Gault Clay, Upper Albian (Lower Cretaceous), Naccolt, Kent, UK (based on B, Gale 2014b: fig. 4S; C, Gale 2014b: fig. 4Q; F, Gale 2014b: fig. 4R). B. NHMUK IC 1034, scutum. C. NHMUK IC 1032, tergum. F. NHMUK IC 1033, upper latus. E. Brachylepadid Faxelepas bruennichi (Withers, 1914) from Paleocene, Danian, Faxe, Denmark (based on Gale 2014b: fig. 6A). NHMUK IC 1019, scutum. H. Brachylepadid Pedupycnolepas pulcher Gale, 2019 from Endemoceras amblygonium Zone, Hauterivian (Lower Cretaceous), Engelbostel, near Hannover, Germany (based on Gale 2019b: fig. 11B). NHMUK IC 1397, holotype, tergum. I–K. Zeugmatolepadid capitula of Etcheslepas durotrigensis Gale, 2014 from Pectinatites pectinatus Zone, Tithonian (Upper Jurassic), Freshwater Steps, Kimmeridge, Dorset, UK. I, J. MIJML coll. unnumbered (based on Gale 2019a: fig. 2C, D). K. MIJML K1261, holotype (based on Gale 2014a: fig. 1). All in external view. Abbreviations: r, rostrum; s, scutum; rl, rostrolatus; ul, upper latus.
Fig. 3 in A new neolepadid cirripede from a Pleistocene cold seep, Krishna-Godavari Basin, offshore India
Fig. 3. Capitular plates of neolepadid cirripede Ashinkailepas indica Gale sp. nov. from Late Pleistocene (52.6 ka), Krishna-Godavari Basin, offshore India (A–G) and living species of the genus (H, I). A–F. Capitular plates of paratypes. A. NHMUK IC 1402, tergum in external (A1) and internal (A2) views. B. NHMUK IC 1403 small tergum in external view. C. NHMUK IC 1404, upper latus in external view. D. NHMUK IC 1405, carina in dorsal (D1) and lateral (D2) views. E. NHMUK IC 1406, small scutum in internal (E1) and external (E2) views. F. NHMUK IC1407, rostrum in ventral view. G. Recent Ashinkailepas seepiophila Yamaguchi, Newman, and Hashimoto, 2004 from near Sagami Bay, Japan. USNM 1018131, paratype in lateral (right side) view (based on Yamaguchi et al. 2004: fig. 4). H. Recent Ashinkailepas kermadecensis Buckeridge, 2009 from Kermadec Ridge, northeast of North Island, New Zealand. NIWA 44722, holotype in lateral view (based on Buckeridge 2009: pl. 1: 5).
Fig. 4 in A new neolepadid cirripede from a Pleistocene cold seep, Krishna-Godavari Basin, offshore India
Fig. 4. Plates of neolepadid cirripede Ashinkailepas indica Gale sp. nov. from Late Pleistocene, 52.6 ka) Krishna-Godavari Basin, offshore India. A–C. External views of terga. A. NHMUK IC 1408. B. NHMUK IC 1409, holotype. C. NHMUK IC 1410. D. NHMUK IC 1411, carina in dorsal view. E. NHMUK IC 1412, scutum external (E1) and internal (E2) views. F. NHMUK IC 1413, small scutum in external view, with predatory gastropod drillhole Oichnus paraboloides Bromley, 1981. I. NHMUK IC 1416, upper latus in external view, with predatory boring made by gastropod. J. NHMUK IC 1417, rostrum in ventral view. G, H, K–M. NHMUK IC 1414, 1415, 1417–1419, respectively, peduncular plates in external (G, L, K) and internal (H, M) views.
Fig. 2 in A new neolepadid cirripede from a Pleistocene cold seep, Krishna-Godavari Basin, offshore India
Fig. 2. Fossil taxa assigned to Neolepadidae. A, B.?Neolepas augurata Buckeridge and Grant-Mackie, 1885 (original of Buckeridge and Grant-Mackie 1985: figs. 2, 3); Sinemurian–Pliensbachian (Lower Jurassic), New Caledonia. A. University of Auckland Geology Department UoA A291a, b, external mould of tergum. B. University of Auckland Geology Department UoA A292a, b, external mould of scutum. This is here tentatively interpreted as an eolepadid. C. Toarcolepas mutans Gale and Schweigert, 2015 (SMNS 26029); Toarcian (Jurassic), Harpoceras falciferum Zone, Zell u. Aichelberg, Germany; reconstruction based upon type material (Gale and Schweigert 2015: fig. 5). D. Litholepas klausreschi Nagler, Haug, Glenner, and Buckeridge, 2017; Tithonian (Upper Jurassic), Hybernoticeras hybernotum Zone, Eichstatt, Germany; D2, SMNS 70388/5 (decolourised original of Nagler et al. 2017: fig. 5B). I am unable to identify the upper latus, marked "l" in their figure; D1, reconstruction (mirrored for comparison with C). E. Concinnalepas costata (Withers, 1928) (NHMUK IC 1103); Kimmeridge Clay, 2 m beneath Freshwater Stone Band, Pectinatites pectinatus Zone, Tithonian (Upper Jurassic), Kimmeridge, Dorset, UK; fragmentary capitulum, showing scutum, tergum, and two lateral plates (based on original of Gale 2014: fig. 6l). Abbreviations: c, carina; l, upper latus; p, peduncle; r, rostrum; s, scutum;; t, tergum.
Fig. 1. NGHP-01 in A new neolepadid cirripede from a Pleistocene cold seep, Krishna-Godavari Basin, offshore India
Fig. 1. NGHP-01 core sites (circles) and logging sites (stars) in the offshore Krishna-Godavari Basin, modified from Lorenson and Collett (2018). Site 12 is co-located with sites 10 and 21 (red circle). Inset shows the study area in Krishna-Godavari Basin is located on the eastern margin of peninsular India in the western Bay of Bengal.
Fig. A4 in Trace metal concentrations in the offshore surficial sediments of Heraklion Gulf (Crete Island, East Mediterranean Sea) Abstract
Fig. A4: Cr (total, nlh and %nlh) per transect [transects are presented from west to east, (•) the outlier value symbol and numbers refer to the isobaths].
Fig. A3 in Trace metal concentrations in the offshore surficial sediments of Heraklion Gulf (Crete Island, East Mediterranean Sea) Abstract
Fig. A3: Mn (total, nlh and %nlh) per transect [transects are presented from west to east, (•) the outlier value symbol and numbers refer to the isobaths].
ScienceDex guides
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These curated guides explain access requirements, typical timelines, costs, and reuse considerations for widely used research datasets.
Allen Brain Atlas
Allen Brain Atlas is an Allen Institute collection of brain map atlases, datasets, APIs, and analysis tools covering mouse, human, and non-human primate brain resources.
Annotated Behaviour and Observability Dataset (ABODe)
ABODe is a University of Edinburgh DataShare dataset for behavior classification in group-housed mice using home-cage video, identities, bounding boxes, ground-plate positions, and annotator labels.
DANDI Archive for NWB datasets
DANDI is a BRAIN Initiative archive for publishing and sharing neurophysiology data, including electrophysiology, optophysiology, and behavioral data packaged as NWB and related standards.
International Brain Laboratory public data
The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.
OpenNeuro
OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.