Literatura académica sobre el tema "Surface geostrophic currents"
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Artículos de revistas sobre el tema "Surface geostrophic currents"
Armitage, Thomas W. K., Sheldon Bacon, Andy L. Ridout, Alek A. Petty, Steven Wolbach y Michel Tsamados. "Arctic Ocean surface geostrophic circulation 2003–2014". Cryosphere 11, n.º 4 (26 de julio de 2017): 1767–80. http://dx.doi.org/10.5194/tc-11-1767-2017.
Texto completoRio, M. H., R. Santoleri, R. Bourdalle-Badie, A. Griffa, L. Piterbarg y G. Taburet. "Improving the Altimeter-Derived Surface Currents Using High-Resolution Sea Surface Temperature Data: A Feasability Study Based on Model Outputs". Journal of Atmospheric and Oceanic Technology 33, n.º 12 (diciembre de 2016): 2769–84. http://dx.doi.org/10.1175/jtech-d-16-0017.1.
Texto completoBerta, Maristella, Lucio Bellomo, Annalisa Griffa, Marcello G. Magaldi, Anne Molcard, Carlo Mantovani, Gian Pietro Gasparini et al. "Wind-induced variability in the Northern Current (northwestern Mediterranean Sea) as depicted by a multi-platform observing system". Ocean Science 14, n.º 4 (25 de julio de 2018): 689–710. http://dx.doi.org/10.5194/os-14-689-2018.
Texto completoCenturioni, L. R., J. C. Ohlmann y P. P. Niiler. "Permanent Meanders in the California Current System". Journal of Physical Oceanography 38, n.º 8 (1 de agosto de 2008): 1690–710. http://dx.doi.org/10.1175/2008jpo3746.1.
Texto completoChaudhary, A., N. Agarwal y R. Sharma. "Estimation of currents using SARAL/AltiKa in the coastal regions of India". ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XL-8 (23 de diciembre de 2014): 1365–67. http://dx.doi.org/10.5194/isprsarchives-xl-8-1365-2014.
Texto completoOllitrault, Michel y Alain Colin de Verdière. "The Ocean General Circulation near 1000-m Depth". Journal of Physical Oceanography 44, n.º 1 (1 de enero de 2014): 384–409. http://dx.doi.org/10.1175/jpo-d-13-030.1.
Texto completoCadden, Dara D. H., Richard Styles y Bulusu Subrahmanyam. "Estimates of Geostrophic Surface Currents in the South Atlantic Bight". Marine Geodesy 32, n.º 3 (11 de agosto de 2009): 334–41. http://dx.doi.org/10.1080/01490410903094908.
Texto completoSudre, Joël, Christophe Maes y Véronique Garçon. "On the global estimates of geostrophic and Ekman surface currents". Limnology and Oceanography: Fluids and Environments 3, n.º 1 (febrero de 2013): 1–20. http://dx.doi.org/10.1215/21573689-2071927.
Texto completoZhang, ZiZhan, Yang Lu y HouTse Hsu. "Detecting surface geostrophic currents using wavelet filter from satellite geodesy". Science in China Series D: Earth Sciences 50, n.º 6 (junio de 2007): 918–26. http://dx.doi.org/10.1007/s11430-007-0038-4.
Texto completoPoulain, Pierre-Marie, Milena Menna y Elena Mauri. "Surface Geostrophic Circulation of the Mediterranean Sea Derived from Drifter and Satellite Altimeter Data". Journal of Physical Oceanography 42, n.º 6 (1 de junio de 2012): 973–90. http://dx.doi.org/10.1175/jpo-d-11-0159.1.
Texto completoTesis sobre el tema "Surface geostrophic currents"
Müller, Felix Lucian [Verfasser], Florian [Akademischer Betreuer] Seitz, Per [Gutachter] Knudsen, Martin [Gutachter] Horwath y Florian [Gutachter] Seitz. "Improved polar geostrophic surface currents from satellite altimetry / Felix Lucian Müller ; Gutachter: Per Knudsen, Martin Horwath, Florian Seitz ; Betreuer: Florian Seitz". München : Universitätsbibliothek der TU München, 2021. http://d-nb.info/122758055X/34.
Texto completoChi-HungChang y 張繼鴻. "Analysis of Surface and Subsurface Geostrophic Currents Derived from Satellite Altimetry and In-situ Hydrographical Data". Thesis, 2015. http://ndltd.ncl.edu.tw/handle/42066379829858480894.
Texto completo國立成功大學
測量及空間資訊學系
103
Studies have shown that ocean circulations are highly important for the climate stability and human life. Their variations are also highly connected to potential natural hazards; therefore, continuous monitoring of ocean circulations has been a highly respected issue over the past centuries. The research uses multiple satellite altimetry data, satellite-only geoid model (GOCE or GRACE), in-situ hydrographical data to determine mesoscale geostrophic current velocities globally. To reduce the errors remain in ADT, the research adopts conventional pointwise approach, spectral approach, and profile approach to process Sea Surface Height (SSH) and geoid models. In-situ current meter observations at 23 stations fixed at 10m depth from TAO/TRITON and PIRATA were taken as ground truth. Results show that when adopting the spectral approach, around 70%~90% of stations gives Root Mean Square (RMS) smaller than or at same accuracy level (within 1 cm/s) compared with the pointwise approach and the averaged RMS is about 10~15 cm/s, while there are over 90% of stations giving RMS smaller than or at same accuracy level with pointwise approach and averaged RMS is around 8~10 cm/s when adopting profile approach, which better improves the conventional pointwise approach. GOCE geoid model was also proved to perform better than GRACE geoid in determining geostrophic currents from time-variant perspective with 60%~80% of stations giving smaller RMS. On the other hand, the average correlation coefficients are all around 0.6~0.7 and 0.3~0.4 in zonal and meridional direction, respectively, with no significant discrepancy when adopting different approach or geoid model (average difference within 0.1). The correlation coefficients between geostrophic current velocities, volume transports through the Gulf Stream (GS), Labrador Current (LC) and wintertime North Atlantic Oscillation (NAO) were estimated, while the correlations of Kuroshio Current (KC) and El Niño/Southern Oscillation (ENSO) were evaluated by using Multivariate ENSO Index (MEI). Results show the correlation coefficient of 0.7 with 1-year lag between GS and wintertime NAO in zonal direction which may relate to the north-southward shift of GS pathway, while LC velocities show the correlation coefficient of 0.5 in meridional direction with zero-lag. The meridional volume transport through the transect also shows the same maximum correlation coefficient and lag time. Such fast response may due to the barotropic nature of LC variability. In the North Pacific Ocean, transects through the Bashi Channel, the northeast of Taiwan, and Kuroshio Extension were chosen. Comparatively higher correlations with MEI are in the meridional currents through the Kuroshio Extension and near-surface zonal currents through the Bashi Channel with maximum negative correlation coefficient of -0.4 and -0.3~ -0.4 for volume transports; Zonal currents through Kuroshio Extension shows maximum positive correlation coefficient of 0.4 and 0.3 for volume transports. Results indicate that correlations in the transect through Bashi Channel and Kuroshio Extension are all higher than those in the transect of the northeast of Taiwan where only gives correlation coefficient of 0.1~0.2.
Zheng, Zhe-Wen y 鄭志文. "Seasonal and interannual variability of multi-satellite derived Sea Surface Heights and Geostrophic Currents in the South China Sea". Thesis, 2006. http://ndltd.ncl.edu.tw/handle/08316759647731497673.
Texto completoYu, Yunyue. "Sea surface temperature, geostrophic current and surface heat advection in the western tropical Pacific". 1996. http://catalog.hathitrust.org/api/volumes/oclc/37356621.html.
Texto completoActas de conferencias sobre el tema "Surface geostrophic currents"
Storie, Jill, Rafael Ramos, Michael Leber, Heather Nowak, Michelle Young y Bruce Magnell. "Evaluation of Loop Current/Loop Current Eddy Fronts to Guide Offshore Oil & Gas Operations". En Offshore Technology Conference. OTC, 2023. http://dx.doi.org/10.4043/32643-ms.
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