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Journal articles on the topic 'Oceanic dynamics'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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1

Li, Futian, Yaping Wu, David A. Hutchins, Feixue Fu, and Kunshan Gao. "Physiological responses of coastal and oceanic diatoms to diurnal fluctuations in seawater carbonate chemistry under two CO<sub>2</sub> concentrations." Biogeosciences 13, no. 22 (2016): 6247–59. http://dx.doi.org/10.5194/bg-13-6247-2016.

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Abstract. Diel and seasonal fluctuations in seawater carbonate chemistry are common in coastal waters, while in the open-ocean carbonate chemistry is much less variable. In both of these environments, ongoing ocean acidification is being superimposed on the natural dynamics of the carbonate buffer system to influence the physiology of phytoplankton. Here, we show that a coastal Thalassiosira weissflogii isolate and an oceanic diatom, Thalassiosira oceanica, respond differentially to diurnal fluctuating carbonate chemistry in current and ocean acidification (OA) scenarios. A fluctuating carbona

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2

Marshall, John C., and A. J. George Nurser. "Fluid Dynamics of Oceanic Thermocline Ventilation." Journal of Physical Oceanography 22, no. 6 (1992): 583–95. http://dx.doi.org/10.1175/1520-0485(1992)022<0583:fdootv>2.0.co;2.

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3

Giachini Tosetto, Everton, Arnaud Bertrand, Sigrid Neumann-Leitão, Alex Costa da Silva, and Miodeli Nogueira Júnior. "Planktonic cnidarian responses to contrasting thermohaline and circulation seasonal scenarios in a tropical western boundary current system." Ocean Science 18, no. 6 (2022): 1763–79. http://dx.doi.org/10.5194/os-18-1763-2022.

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Abstract. In western boundary current systems (WBCSs), strong currents flow coastward carrying oceanic water masses and their associated planktonic fauna. Variation in the intensity of these currents and in the continental runoff may affect the dynamic interplay between oceanic and coastal communities. In addition, changes in the continental runoff and the thermohaline structure modulate the primary production, adding complexity to the dynamics of these oligotrophic systems. These dynamics likely shape the planktonic cnidarian communities. To further understand such relationships, we used a co

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4

Seip, Knut L., and Øyvind Grøn. "Atmospheric and Ocean Dynamics May Explain Cycles in Oceanic Oscillations." Climate 7, no. 6 (2019): 77. http://dx.doi.org/10.3390/cli7060077.

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What causes cycles in oceanic oscillations, and is there a change in the characteristics of oscillations in around 1950? Characteristics of oceanic cycles and their sources are important for climate predictability. We here compare cycles generated in a simple model with observed oceanic cycles in the great oceans: The North Atlantic Oscillation (NAO), El Niño, the Southern Oscillation Index (SOI), and the Pacific Decadal Oscillation (PDO). In the model, we let a stochastic movement in one oceanic oscillation cause a similar but lagging movement in another oceanic oscillation. The two interacti

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Rhines, P. B. "Vorticity Dynamics of the Oceanic General Circulation." Annual Review of Fluid Mechanics 18, no. 1 (1986): 433–97. http://dx.doi.org/10.1146/annurev.fl.18.010186.002245.

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6

Pedlosky, J. "The Dynamics of the Oceanic Subtropical Gyres." Science 248, no. 4953 (1990): 316–22. http://dx.doi.org/10.1126/science.248.4953.316.

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7

Roberts, Nicholas P. "Oceanic Wahhabism." Journal of World History 36, no. 1 (2025): 21–49. https://doi.org/10.1353/jwh.2025.a950279.

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Abstract: At some point around 1810, a leading Wahhabi theologian in the capital of the First Saudi State fielded an intriguing question: Although Wahhabi leaders preached the ideals of enmity and violence toward non-Wahhabi peoples, could Wahhabi merchants travel to non-Wahhabi lands, do business with non-Wahhabi persons, and reside among them while pursuing commercial agendas? The theologian answered yes. I argue that this question and its answer reveal a lived reality in Najd that historians have yet to fully uncover. The theologian’s answer reveals how Arabia’s interior where Wahhabism eme

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8

Gayen, Bishakhdatta, and Andreas Klocker. "Deep convection drives oceanic overturning." Physics Today 77, no. 6 (2024): 44–50. http://dx.doi.org/10.1063/pt.uvlg.jjol.

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Research that combines fluid dynamics and climate science is uncovering the inner workings of the North Atlantic’s overturning circulation. Future changes to that circulation system could trigger major disruptions to global weather patterns.

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Woodward, J. R., J. W. Pitchford, and M. A. Bees. "Physical flow effects can dictate plankton population dynamics." Journal of The Royal Society Interface 16, no. 157 (2019): 20190247. http://dx.doi.org/10.1098/rsif.2019.0247.

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Oceanic flows do not necessarily mix planktonic species. Differences in individual organisms’ physical and hydrodynamic properties can cause changes in drift normal to the mean flow, leading to segregation between species. This physically driven heterogeneity may have important consequences at the scale of population dynamics. Here, we describe how one form of physical forcing, circulating flows with different inertia effects between phytoplankton and zooplankton, can dramatically alter excitable plankton bloom dynamics. This may impact our understanding of the initiation and development of ha

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Greene, Charles, Peter Wiebe, and Jeanneatte Zamon. "Acoustic Visualization of Patch Dynamics in Oceanic Ecosystems." Oceanography 7, no. 1 (1994): 4–12. http://dx.doi.org/10.5670/oceanog.1994.09.

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11

Wang, Yang, Avi Gozolchiani, Yosef Ashkenazy, and Shlomo Havlin. "Oceanic El-Niño wave dynamics and climate networks." New Journal of Physics 18, no. 3 (2016): 033021. http://dx.doi.org/10.1088/1367-2630/18/3/033021.

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12

Lapeyre, Guillaume, Patrice Klein, and Bach Lien Hua. "Oceanic Restratification Forced by Surface Frontogenesis." Journal of Physical Oceanography 36, no. 8 (2006): 1577–90. http://dx.doi.org/10.1175/jpo2923.1.

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Abstract Potential vorticity (PV) conservation implies a strong constraint on the time evolution of the mean density at a given depth. The authors show that, on an f plane and in the absence of sources and sinks of PV, it only depends on two terms, namely, the time evolution of the product between density anomaly and relative vorticity and the vertical PV flux. This primitive equation result, which applies at any depth, suggests that the ageostrophic dynamics induced by baroclinic eddies strongly affect the mean oceanic stratification profile. This result is illustrated for two simple initial-

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Sultanov, Ogabek, Safarali Bobojonov, Muntadher MuhssanAlmusawi, Ayyappan V, Dilorom Bobojonova, and Ashu Nayak. "Phytoplankton dynamics and their role in carbon sequestration across different oceanic zones." International Journal of Aquatic Research and Environmental Studies 5, S1 (2025): 132–42. https://doi.org/10.70102/ijares/v5s1/5-s1-14.

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Phytoplankton are key elements in the oceanic carbon cycle. They assist with roughly fifty percent of global productivity and enable carbon storage through the biological pump. This study shows phytoplankton carbon sequestration across spatially discrete oceanic zones: the coastal shelves, the oligotrophic open ocean, and the upwelling systems. To evaluate spatial-temporal variability during 2010-2020, satellite-derived chlorophyll-a concentrations (MODIS-AQUA), other datasets, and in-situ observations were integrated with a coupled physical-biogeochemical model. The analysis results display s

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14

Heron, Philip J. "Mantle plumes and mantle dynamics in the Wilson cycle." Geological Society, London, Special Publications 470, no. 1 (2019): 87–103. http://dx.doi.org/10.1144/sp470-2018-97.

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AbstractThis review discusses the thermal evolution of the mantle following large-scale tectonic activities such as continental collision and continental rifting. About 300 myr ago, continental material amalgamated through the large-scale subduction of oceanic seafloor, marking the termination of one or more oceanic basins (e.g. Wilson cycles) and the formation of the supercontinent Pangaea. The present day location of the continents is due to the rifting apart of Pangaea, with the dispersal of the supercontinent being characterized by increased volcanic activity linked to the generation of de

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Füllekrug, M., C. Price, Y. Yair, and E. R. Williams. "<i>Letter to the Editor</i> Intense oceanic lightning." Annales Geophysicae 20, no. 1 (2002): 133–37. http://dx.doi.org/10.5194/angeo-20-133-2002.

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Abstract. The electrodynamic properties of intense oceanic lightning discharges are compared to intense continental lightning discharges. Particularly intense negative lightning discharges with absolute charge moments > 2 kC · km occur more often over the oceans than over the continents during April 1998. Intense continental lightning discharges, with negative and positive polarity, and intense positive oceanic lightning discharges primarily occur associated with mesoscale convection in the late evening. The number of intense negative oceanic lightning discharges increases in the early morn

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Park, W., and M. Latif. "Ocean Dynamics and the Nature of Air–Sea Interactions over the North Atlantic at Decadal Time Scales." Journal of Climate 18, no. 7 (2005): 982–95. http://dx.doi.org/10.1175/jcli-3307.1.

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Abstract The dependence of the air–sea interactions over the North Atlantic on the ocean dynamics is explored by analyzing multicentury integrations with two different coupled ocean–atmosphere models. One is a coupled general circulation model (CGCM), in which both the atmospheric and the oceanic components are represented by general circulation models (GCMs). The second coupled model employs the same atmospheric GCM, but the oceanic GCM is replaced by a fixed-depth mixed layer model, so that variations of the ocean dynamics are excluded. The coupled model including active ocean dynamics simul

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Chapman, Christopher C., Andrew McC Hogg, Andrew E. Kiss, and Stephen R. Rintoul. "The Dynamics of Southern Ocean Storm Tracks." Journal of Physical Oceanography 45, no. 3 (2015): 884–903. http://dx.doi.org/10.1175/jpo-d-14-0075.1.

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AbstractThe mechanisms that initiate and maintain oceanic “storm tracks” (regions of anomalously high eddy kinetic energy) are studied in a wind-driven, isopycnal, primitive equation model with idealized bottom topography. Storm tracks are found downstream of the topography in regions strongly influenced by a large-scale stationary meander that is generated by the interaction between the background mean flow and the topography. In oceanic storm tracks the length scale of the stationary meander differs from that of the transient eddies, a point of distinction from the atmospheric storm tracks.

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18

Juewei Shi and Sioh Yang Tan. "Flows of Innovation in Fo Guang Shan Oceania: Transregional dynamics behind the Buddha’s Birthday Festival." Journal of Global Buddhism 23, no. 2 (2022): 185–202. http://dx.doi.org/10.26034/lu.jgb.2022.1998.

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Fo Guang Shan (FGS), a transnational Buddhist movement in the Chinese Mahāyāna tradition, has grown rapidly in the last fifty years to become a global network of close to 180 branch temples. For almost thirty years, FGS Oceania has invested heavily in the Buddha’s Birthday Festival annually in the form of weekend-long festivals in public spaces across Australia and New Zealand, involving months of planning and thousands of volunteers to welcome tens of thousands of visitors. FGS Oceania served as an incubator, exporter, and importer of innovations to make the Buddha, Dharma, and Sangha accessi

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Petereit, Johannes, Jan Saynisch, Christopher Irrgang, Tobias Weber, and Maik Thomas. "Electromagnetic characteristics of ENSO." Ocean Science 14, no. 3 (2018): 515–24. http://dx.doi.org/10.5194/os-14-515-2018.

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Abstract. The motion of electrically conducting sea water through Earth's magnetic field induces secondary electromagnetic fields. Due to its periodicity, the oceanic tidally induced magnetic field is easily distinguishable in magnetic field measurements and therefore detectable. These tidally induced signatures in the electromagnetic fields are also sensitive to changes in oceanic temperature and salinity distributions. We investigate the impact of oceanic heat and salinity changes related to the El Niño–Southern Oscillation (ENSO) on oceanic tidally induced magnetic fields. Synthetic hydrogr

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20

Chen, Xingchao, Robert G. Nystrom, Christopher A. Davis, and Colin M. Zarzycki. "Dynamical Structures of Cross-Domain Forecast Error Covariance of a Simulated Tropical Cyclone in a Convection-Permitting Coupled Atmosphere–Ocean Model." Monthly Weather Review 149, no. 1 (2021): 41–63. http://dx.doi.org/10.1175/mwr-d-20-0116.1.

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AbstractUnderstanding the dynamics of the flow-dependent forecast error covariance across the air–sea interface is beneficial toward revealing the potential influences of strongly coupled data assimilation on tropical cyclone (TC) initialization in coupled models, and the fundamental dynamics associated with TC air–sea interactions. A 200-member ensemble of convection-permitting forecasts from a coupled atmosphere–ocean regional model is used to investigate the forecast error covariance across the oceanic and atmospheric domains during the rapid intensification of Hurricane Florence (2018). Fo

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21

Guo, Laodong, Peter H. Santschi, and Kent W. Warnken. "Dynamics of dissolved organic carbon (DOC) in oceanic environments." Limnology and Oceanography 40, no. 8 (1995): 1392–403. http://dx.doi.org/10.4319/lo.1995.40.8.1392.

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22

Barajas‐Barbosa, Martha Paola, Patrick Weigelt, Michael Krabbe Borregaard, Gunnar Keppel, and Holger Kreft. "Environmental heterogeneity dynamics drive plant diversity on oceanic islands." Journal of Biogeography 47, no. 10 (2020): 2248–60. http://dx.doi.org/10.1111/jbi.13925.

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23

Zatman, Stephen, Richard G. Gordon, and Kartik Mutnuri. "Dynamics of diffuse oceanic plate boundaries: insensitivity to rheology." Geophysical Journal International 162, no. 1 (2005): 239–48. http://dx.doi.org/10.1111/j.1365-246x.2005.02622.x.

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24

Richards, Fred, Mark Hoggard, Alistair Crosby, Siavash Ghelichkhan, and Nicky White. "Structure and dynamics of the oceanic lithosphere-asthenosphere system." Physics of the Earth and Planetary Interiors 309 (December 2020): 106559. http://dx.doi.org/10.1016/j.pepi.2020.106559.

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25

Bye, John A. T. "The Dynamics of the Oceanic Air-Sea Boundary Layer." Advances in Environmental and Engineering Research 04, no. 01 (2023): 1–16. http://dx.doi.org/10.21926/aeer.2301018.

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This paper presents a model for the similarity structure of the velocity profiles in air and water in the wave boundary layer, which provides predictions in terms of two parameters, F and R, of all its important properties, including the Charnock parameter, the surface drift velocity and the condition for the cancellation of the surface Stokes velocity by the surface current. The parameter, F, arises from the fetch variability of the wave field, and the parameter, R, arises from the duration variability of the wave field. In the analysis two regimes emerge, namely the Ekman regime and the Hass

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Alves, José M. R., Rui M. A. Caldeira, and Pedro M. A. Miranda. "Dynamics and oceanic response of the Madeira tip‐jets." Quarterly Journal of the Royal Meteorological Society 146, no. 732 (2020): 3048–63. http://dx.doi.org/10.1002/qj.3825.

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27

Déruelle, B., G. Dreibus, and A. Jambon. "Iodine abundances in oceanic basalts: implications for Earth dynamics." Earth and Planetary Science Letters 108, no. 4 (1992): 217–27. http://dx.doi.org/10.1016/0012-821x(92)90024-p.

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28

Pötter, Stephan, Katharina Seeger, Christiane Richter, et al. "Pleniglacial dynamics in an oceanic central European loess landscape." E&G Quaternary Science Journal 72, no. 1 (2023): 77–94. http://dx.doi.org/10.5194/egqsj-72-77-2023.

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Abstract. Loess–palaeosol sequences (LPSs) of the oceanic-influenced European loess belt underwent frequent post-depositional processes induced by surface runoff or periglacial processes. The interpretation of such atypical LPSs is not straightforward, and they cannot be easily used for regional to continental correlations. Within the last few years, however, such sequences gained increased attention, as they are valuable archives for regional landscape dynamics. In this study, the Siersdorf LPS was analysed using a multi-proxy approach using sedimentological, geochemical, and spectrophotometr

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Wirth, A. "Laminar and weakly turbulent oceanic gravity currents performing inertial oscillations." Ocean Science 8, no. 3 (2012): 301–17. http://dx.doi.org/10.5194/os-8-301-2012.

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Abstract. The small scale dynamics of a weakly turbulent oceanic gravity current is determined. The gravity current considered is initially at rest and adjusts by performing inertial oscillations to a geostrophic mean flow. The dynamics is explored with a hierarchy of mathematical models. The most involved are the fully 3-D Navier-Stokes equations subject to the Boussinesq approximation. A 1-D and 0-D mathematical model of the same gravity current dynamics are systematically derived. Using this hierarchy and the numerical solutions of the mathematical models, the turbulent dynamics at the bott

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Wirth, A. "Laminar and weakly turbulent oceanic gravity currents performing inertial oscillations." Ocean Science Discussions 8, no. 5 (2011): 2001–45. http://dx.doi.org/10.5194/osd-8-2001-2011.

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Abstract. The small scale dynamics of a weakly turbulent oceanic gravity current is determined. The gravity current considered is initially at rest and adjusts by performing inertial oscillations to a geostrophic mean flow. The dynamics is explored with a hierarchy of mathematical models. The most involved are the fully 3-D Navier-Stokes equations subject to the Boussinesq approximation. A 1-D and 0-D mathematical model of the same gravity current dynamics are systematically derived. Using this hierarchy and the numerical solutions of the mathematical models, the turbulent dynamics at the bott

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Ozaki, Kazumi, Devon B. Cole, Christopher T. Reinhard, and Eiichi Tajika. "CANOPS-GRB v1.0: a new Earth system model for simulating the evolution of ocean–atmosphere chemistry over geologic timescales." Geoscientific Model Development 15, no. 20 (2022): 7593–639. http://dx.doi.org/10.5194/gmd-15-7593-2022.

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Abstract. A new Earth system model of intermediate complexity – CANOPS-GRB v1.0 – is presented for use in quantitatively assessing the dynamics and stability of atmospheric and oceanic chemistry on Earth and Earth-like planets over geologic timescales. The new release is designed to represent the coupled major element cycles of C, N, P, O, and S, as well as the global redox budget (GRB) in Earth's exogenic (ocean–atmosphere–crust) system, using a process-based approach. This framework provides a mechanistic model of the evolution of atmospheric and oceanic O2 levels on geologic timescales and

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Gao, Yu, Igor Kamenkovich, and Natalie Perlin. "Origins of mesoscale mixed-layer depth variability in the Southern Ocean." Ocean Science 19, no. 3 (2023): 615–27. http://dx.doi.org/10.5194/os-19-615-2023.

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Abstract. Mixed-layer depth (MLD) exhibits significant variability, which is important for atmosphere–ocean exchanges of heat and atmospheric gases. The origins of the mesoscale MLD variability in the Southern Ocean are studied here in an idealised regional ocean–atmosphere model (ROAM). The main conclusion from the analysis of the upper-ocean buoyancy budget is that, while the atmospheric forcing and oceanic vertical mixing, on average, induce the mesoscale variability of MLD, the three-dimensional oceanic advection of buoyancy counteracts and partially balances these atmosphere-induced verti

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Hibler, W. D., and Jinlun Zhang. "On the effect of sea-ice dynamics on oceanic thermohaline circulation." Annals of Glaciology 21 (1995): 361–68. http://dx.doi.org/10.3189/s0260305500016074.

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An idealized planetary flat-bottom geostrophic ice–ocean model is constructed with boundaries at latitudes 5° and 65° N and longitudes 50° W and 10° E in order to approximate the North Atlantic. The model is driven by fixed zonally averaged wind, surface air temperatures and surface ocean salinity. A dynamic thermodynamic sea-ice model is coupled to the ocean model. Only the thermodynamic insulating effects of the sea ice are considered, and no salt fluxes due to melting and freezing are included. Four equilibrium simulations of about 5000 years each are performed: two with interactive sea ice

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Hibler, W. D., and Jinlun Zhang. "On the effect of sea-ice dynamics on oceanic thermohaline circulation." Annals of Glaciology 21 (1995): 361–68. http://dx.doi.org/10.1017/s0260305500016074.

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An idealized planetary flat-bottom geostrophic ice–ocean model is constructed with boundaries at latitudes 5° and 65° N and longitudes 50° W and 10° E in order to approximate the North Atlantic. The model is driven by fixed zonally averaged wind, surface air temperatures and surface ocean salinity. A dynamic thermodynamic sea-ice model is coupled to the ocean model. Only the thermodynamic insulating effects of the sea ice are considered, and no salt fluxes due to melting and freezing are included. Four equilibrium simulations of about 5000 years each are performed: two with interactive sea ice

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35

Börger, Lara, Michael Schindelegger, Mengnan Zhao, et al. "Chaotic oceanic excitation of low-frequency polar motion variability." Earth System Dynamics 16, no. 1 (2025): 75–90. https://doi.org/10.5194/esd-16-75-2025.

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Abstract. Studies of Earth rotation variations generally assume that changes in non-tidal oceanic angular momentum (OAM) manifest the ocean's direct response to atmospheric forces. However, fluctuations in OAM may also arise from chaotic intrinsic ocean processes that originate in local nonlinear (e.g., mesoscale) dynamics and can map into motions and mass variations at basin scales. To examine whether such random mass redistributions effectively excite polar motion, we compute monthly OAM anomalies from a 50-member ensemble of eddy-permitting global ocean/sea ice simulations that sample intri

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36

Berloff, P., W. Dewar, S. Kravtsov, and J. McWilliams. "Ocean Eddy Dynamics in a Coupled Ocean–Atmosphere Model*." Journal of Physical Oceanography 37, no. 5 (2007): 1103–21. http://dx.doi.org/10.1175/jpo3041.1.

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Abstract The role of mesoscale oceanic eddies is analyzed in a quasigeostrophic coupled ocean–atmosphere model operating at a large Reynolds number. The model dynamics are characterized by decadal variability that involves nonlinear adjustment of the ocean to coherent north–south shifts of the atmosphere. The oceanic eddy effects are diagnosed by the dynamical decomposition method adapted for nonstationary external forcing. The main effects of the eddies are an enhancement of the oceanic eastward jet separating the subpolar and subtropical gyres and a weakening of the gyres. The flow-enhancing

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Li, Lianwei, Cunjin Xue, Yangfeng Xu, Chengbin Wu, and Chaoran Niu. "PoSDMS: A Mining System for Oceanic Dynamics with Time Series of Raster-Formatted Datasets." Remote Sensing 14, no. 13 (2022): 2991. http://dx.doi.org/10.3390/rs14132991.

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Many effective and advanced methods have been developed to explore oceanic dynamics using time series of raster-formatted datasets; however, they have generally been designed at a scale suitable for data observation and used independently of each other, despite the potential advantages of combining different modules into an integrated system at a scale suited for dynamic evolution. From raster-formatted datasets to marine knowledge, we developed and integrated several mining algorithms at a dynamic evolutionary scale and combined them into six modules: a module of raster-formatted dataset pret

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Behr, Whitney M., Adam F. Holt, Thorsten W. Becker, and Claudio Faccenna. "The effects of plate interface rheology on subduction kinematics and dynamics." Geophysical Journal International 230, no. 2 (2022): 796–812. http://dx.doi.org/10.1093/gji/ggac075.

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SUMMARY Tectonic plate motions predominantly result from a balance between the potential energy change of the subducting slab and viscous dissipation in the mantle, bending lithosphere and slab–upper plate interface. A wide range of observations from active subduction zones and exhumed rocks suggest that subduction interface shear zone rheology is sensitive to the composition of subducting crustal material—for example, sediments versus mafic igneous oceanic crust. Here we use 2-D numerical models of dynamically consistent subduction to systematically investigate how subduction interface viscos

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Lu, Xiaojie, Guoqing Han, Yifan Lin, et al. "Application of Large-Scale Rotating Platforms in the Study of Complex Oceanic Dynamic Processes." Journal of Marine Science and Engineering 13, no. 6 (2025): 1187. https://doi.org/10.3390/jmse13061187.

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As the core components of geophysical dynamic system, oceans and atmospheres are dominated by the Coriolis force, which governs complex dynamic phenomena such as internal waves, gravity currents, vortices, and others involving multi-scale spatiotemporal coupling. Due to the limitations of in situ observations, large-scale rotating tanks have emerged as critical experimental platforms for simulating Earth’s rotational effects. This review summarizes recent advancements in rotating tank applications for studying oceanic flow phenomena, including mesoscale eddies, internal waves, Ekman flows, Ros

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Zatman, Stephen, Richard G. Gordon, and Mark A. Richards. "Analytic models for the dynamics of diffuse oceanic plate boundaries." Geophysical Journal International 145, no. 1 (2001): 145–56. http://dx.doi.org/10.1111/j.1365-246x.2001.00357.x.

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Noh, Yign. "Dynamics of Diurnal Thermocline Formation in the Oceanic Mixed Layer." Journal of Physical Oceanography 26, no. 10 (1996): 2183–95. http://dx.doi.org/10.1175/1520-0485(1996)026<2183:dodtfi>2.0.co;2.

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Azeria, Ermias T., Allan Carlson, Tomas Pärt, and Christer G. Wiklund. "Temporal dynamics and nestedness of an oceanic island bird fauna." Global Ecology and Biogeography 15, no. 4 (2006): 328–38. http://dx.doi.org/10.1111/j.1466-822x.2006.00227.x.

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Afonso, Pedro, Niall McGinty, and Miguel Machete. "Dynamics of Whale Shark Occurrence at Their Fringe Oceanic Habitat." PLoS ONE 9, no. 7 (2014): e102060. http://dx.doi.org/10.1371/journal.pone.0102060.

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Dachs, Jordi, Rainer Lohmann, Wendy A. Ockenden, Laurence Méjanelle, Steven J. Eisenreich, and Kevin C. Jones. "Oceanic Biogeochemical Controls on Global Dynamics of Persistent Organic Pollutants." Environmental Science & Technology 36, no. 20 (2002): 4229–37. http://dx.doi.org/10.1021/es025724k.

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Dusenberry, J. A., R. J. Olson, and S. W. Chisholm. "Field observations of oceanic mixed layer dynamics and picophytoplankton photoacclimation." Journal of Marine Systems 24, no. 3-4 (2000): 221–32. http://dx.doi.org/10.1016/s0924-7963(99)00087-1.

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Thibon, Fanny, Janne Blichert-Toft, Harilaos Tsikos, John Foden, Emmanuelle Albalat, and Francis Albarede. "Dynamics of oceanic iron prior to the Great Oxygenation Event." Earth and Planetary Science Letters 506 (January 2019): 360–70. http://dx.doi.org/10.1016/j.epsl.2018.11.016.

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Kiene, Ronald P. "Dynamics of dimethyl sulfide and dimethylsulfoniopropionate in oceanic water samples." Marine Chemistry 37, no. 1-2 (1992): 29–52. http://dx.doi.org/10.1016/0304-4203(92)90055-f.

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Auer, Ludwig, Thorsten W. Becker, Lapo Boschi, and Nicholas Schmerr. "Thermal structure, radial anisotropy, and dynamics of oceanic boundary layers." Geophysical Research Letters 42, no. 22 (2015): 9740–49. http://dx.doi.org/10.1002/2015gl066246.

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Naliboff, John B., Magali I. Billen, Taras Gerya, and Jessie Saunders. "Dynamics of outer-rise faulting in oceanic-continental subduction systems." Geochemistry, Geophysics, Geosystems 14, no. 7 (2013): 2310–27. http://dx.doi.org/10.1002/ggge.20155.

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Lavín, Alicia, Xabier Moreno-Ventas, Victoria Ortiz de Zárate, Pablo Abaunza, and José Manuel Cabanas. "Environmental variability in the North Atlantic and Iberian waters and its influence on horse mackerel (Trachurus trachurus) and albacore (Thunnus alalunga) dynamics." ICES Journal of Marine Science 64, no. 3 (2007): 425–38. http://dx.doi.org/10.1093/icesjms/fsl042.

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Abstract:

Abstract Lavín, A., Moreno-Ventas, X., Ortiz de Zárate, V., Abaunza, P., and Cabanas, J. M. 2007. Environmental variability in the North Atlantic and Iberian waters and its influence on horse mackerel (Trachurus trachurus) and albacore (Thunnus alalunga) dynamics. – ICES Journal of Marine Science, 64: 425–438. We explore the potential impact of climatic and oceanic variables on the dynamics of horse mackerel Trachurus trachurus (coastal distribution) and albacore Thunnus alalunga (oceanic distribution). Principal components analysis of a set of environmental parameters for the years 1966–2000

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