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Journal articles on the topic 'Deep water flow'

Author: Grafiati

Published: 4 June 2021

Last updated: 11 February 2022

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1

Timmermans, M.-L., P. Winsor, and J. A. Whitehead. "Deep-Water Flow over the Lomonosov Ridge in the Arctic Ocean." Journal of Physical Oceanography 35, no. 8 (2005): 1489–93. http://dx.doi.org/10.1175/jpo2765.1.

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Abstract The Arctic Ocean likely impacts global climate through its effect on the rate of deep-water formation and the subsequent influence on global thermohaline circulation. Here, the renewal of the deep waters in the isolated Canadian Basin is quanitified. Using hydraulic theory and hydrographic observations, the authors calculate the magnitude of this renewal where circumstances have thus far prevented direct measurements. A volume flow rate of Q = 0.25 ± 0.15 Sv (Sv ≡ 106 m3 s−1) from the Eurasian Basin to the Canadian Basin via a deep gap in the dividing Lomonosov Ridge is estimated. Dee

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2

Bensi, Manuel, Vedrana Kovačević, Leonardo Langone, et al. "Deep Flow Variability Offshore South-West Svalbard (Fram Strait)." Water 11, no. 4 (2019): 683. http://dx.doi.org/10.3390/w11040683.

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Water mass generation and mixing in the eastern Fram Strait are strongly influenced by the interaction between Atlantic and Arctic waters and by the local atmospheric forcing, which produce dense water that substantially contributes to maintaining the global thermohaline circulation. The West Spitsbergen margin is an ideal area to study such processes. Hence, in order to investigate the deep flow variability on short-term, seasonal, and multiannual timescales, two moorings were deployed at ~1040 m depth on the southwest Spitsbergen continental slope. We present and discuss time series data col

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3

Dong, Changming, James C. McWilliams, and Alexander F. Shchepetkin. "Island Wakes in Deep Water." Journal of Physical Oceanography 37, no. 4 (2007): 962–81. http://dx.doi.org/10.1175/jpo3047.1.

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Abstract Density stratification and planetary rotation distinguish three-dimensional island wakes significantly from a classical fluid dynamical flow around an obstacle. A numerical model is used to study the formation and evolution of flow around an idealized island in deep water (i.e., with vertical island sides and surface-intensified stratification and upstream flow), focusing on wake instability, coherent vortex formation, and mesoscale and submesoscale eddy activity. In a baseline experiment with strong vorticity generation at the island, three types of instability are evident: centrifug

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4

Fieux, M., and J. C. Swallow. "Flow of deep water into the Somali Basin." Deep Sea Research Part A. Oceanographic Research Papers 35, no. 2 (1988): 303–9. http://dx.doi.org/10.1016/0198-0149(88)90041-6.

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5

张, 雨晴. "Flume Experiment Research Progress of Deep Water Gravity Flow." Advances in Geosciences 10, no. 11 (2020): 1062–74. http://dx.doi.org/10.12677/ag.2020.1011105.

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6

Liu, Ko-Fei. "Tide-Induced Ground-Water Flow in Deep Confined Aquifer." Journal of Hydraulic Engineering 122, no. 2 (1996): 104–10. http://dx.doi.org/10.1061/(asce)0733-9429(1996)122:2(104).

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7

Siedler, Gerold, Jürgen Holfort, Walter Zenk, Thomas J. Müller, and Tiberiu Csernok. "Deep-Water Flow in the Mariana and Caroline Basins*." Journal of Physical Oceanography 34, no. 3 (2004): 566–81. http://dx.doi.org/10.1175/2511.1.

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Abstract Two major water masses dominate the deep layers in the Mariana and Caroline Basins: the Lower Circumpolar Water (LCPW), arriving from the Southern Ocean along the slopes north of the Marshall Islands, and the North Pacific Deep Water (NPDW) reaching the region from the northeastern Pacific Ocean. Hydrographic and moored observations and multibeam echosounding were performed in the East Mariana and the East Caroline Basins to detail watermass distributions and flow paths in the area. The LCPW enters the East Mariana Basin from the east. At about 13°N, however, in the southern part of t

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8

Kouskoulas, David M., and Yaron Toledo. "Deep water gravity wave triad resonances on uniform flow." Physics of Fluids 32, no. 7 (2020): 076603. http://dx.doi.org/10.1063/5.0012631.

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9

McCave, I. N., T. Kiefer, D. J. R. Thornalley, and H. Elderfield. "Deep flow in the Madagascar–Mascarene Basin over the last 150000 years." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 363, no. 1826 (2005): 81–99. http://dx.doi.org/10.1098/rsta.2004.1480.

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The SW Indian Ocean contains at least four layers of water masses with different sources: deep Antarctic (Lower Circumpolar Deep Water) flow to the north, midwater North Indian Deep Water flow to the south and Upper Circumpolar Deep Water to the north, meridional convergence of intermediate waters at 500–1500 m, and the shallow South Equatorial Current flowing west. Sedimentation rates in the area are rather low, being less than 1 cm ka −1 on Madagascar Ridge, but up to 4 cm ka −1 at Amirante Passage. Bottom flow through the Madagascar–Mascarene Basin into Amirante Passage varies slightly on g

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10

Burckel, Pierre, Claire Waelbroeck, Yiming Luo, et al. "Changes in the geometry and strength of the Atlantic meridional overturning circulation during the last glacial (20–50 ka)." Climate of the Past 12, no. 11 (2016): 2061–75. http://dx.doi.org/10.5194/cp-12-2061-2016.

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Abstract. We reconstruct the geometry and strength of the Atlantic meridional overturning circulation during the Heinrich stadial 2 and three Greenland interstadials of the 20–50 ka period based on the comparison of new and published sedimentary 231Pa / 230Th data with simulated sedimentary 231Pa / 230Th. We show that the deep Atlantic circulation during these interstadials was very different from that of the Holocene. Northern-sourced waters likely circulated above 2500 m depth, with a flow rate lower than that of the present-day North Atlantic deep water (NADW). Southern-sourced deep waters

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11

Hurynovich, Anatoly, and Valiantsin Ramanouski. "Artifisial replenishment of the deep aquifers." E3S Web of Conferences 45 (2018): 00025. http://dx.doi.org/10.1051/e3sconf/20184500025.

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On the basis of the analysis, laboratory and pilot studies that have been conducted, schemes of artificial replenishment of deep aquifers are proposed. These schemes allow a groundwater recharge in order to water intake with generate electricity using the energy of the water flow and provide clear water, which serves to replenish underground water. Experimental section of this technological scheme was designed and built in the region of water intake in Brest (Belarus), on which were carried out hydrogeological surveys. Based on the above results, it was suggested to use the energy of the water

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12

Zhang, Zhiqiang, Bingcheng Si, Huijie Li, and Min Li. "Quantify Piston and Preferential Water Flow in Deep Soil Using Cl− and Soil Water Profiles in Deforested Apple Orchards on the Loess Plateau, China." Water 11, no. 10 (2019): 2183. http://dx.doi.org/10.3390/w11102183.

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Piston and preferential water flow are viewed as the two dominant water transport mechanisms regulating terrestrial water and solute cycles. However, it is difficult to accurately separate the two water flow patterns because preferential flow is not easy to capture directly in field environments. In this study, we take advantage of the afforestation induced desiccated deep soil, and directly quantify piston and preferential water flow using chloride ions (Cl−) and soil water profiles, in four deforested apple orchards on the Loess Plateau. The deforestation time ranged from 3 to 15 years. In e

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13

Borenäs, Karin M., and Peter A. Lundberg. "On the deep-water flow through the Faroe Bank Channel." Journal of Geophysical Research 93, no. C2 (1988): 1281. http://dx.doi.org/10.1029/jc093ic02p01281.

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14

Røy, Hans, Jae Seong Lee, Stefan Jansen, and Dirk de Beer. "Tide-driven deep pore-water flow in intertidal sand flats." Limnology and Oceanography 53, no. 4 (2008): 1521–30. http://dx.doi.org/10.4319/lo.2008.53.4.1521.

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15

Smethie, William M., Rana A. Fine, Alfred Putzka, and E. Peter Jones. "Tracing the flow of North Atlantic Deep Water using chlorofluorocarbons." Journal of Geophysical Research: Oceans 105, no. C6 (2000): 14297–323. http://dx.doi.org/10.1029/1999jc900274.

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16

Dutykh, D., D. Clamond, and M. Chhay. "Serre-type Equations in Deep Water." Mathematical Modelling of Natural Phenomena 12, no. 1 (2017): 23–40. http://dx.doi.org/10.1051/mmnp/201712103.

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This manuscript is devoted to the modelling of water waves in the deep water regime with some emphasis on the underlying variational structures. The present article should be considered as a review of some existing models and modelling approaches even if new results are presented as well. Namely, we derive the deep water analogue of the celebrated SERRE–GREEN–NAGHDI equations which have become the standard model in shallow water environments. The relation to existing models is discussed. Moreover, the multi-symplectic structure of these equations is reported as well. The results of this work c

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17

Abrashkin, A. A. "Standing vortex waves in deep water." Fluid Dynamics 31, no. 3 (1996): 470–73. http://dx.doi.org/10.1007/bf02030232.

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18

Moreira, R. M., and J. T. A. Chacaltana. "Vorticity effects on nonlinear wave–current interactions in deep water." Journal of Fluid Mechanics 778 (July 31, 2015): 314–34. http://dx.doi.org/10.1017/jfm.2015.385.

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The effects of uniform vorticity on a train of ‘gentle’ and ‘steep’ deep-water waves interacting with underlying flows are investigated through a fully nonlinear boundary integral method. It is shown that wave blocking and breaking can be more prominent depending on the magnitude and direction of the shear flow. Reflection continues to occur when sufficiently strong adverse currents are imposed on ‘gentle’ deep-water waves, though now affected by vorticity. For increasingly positive values of vorticity, the induced shear flow reduces the speed of right-going progressive waves, introducing sign

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19

Williams, Dara, Annette Harte, and Frank Grealish. "Development of an Analytical Tool for the Design of Deep Water Riser/Flow Line Thermal Insulation Systems." Journal of Offshore Mechanics and Arctic Engineering 127, no. 2 (2004): 96–103. http://dx.doi.org/10.1115/1.1894403.

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The offshore oil and gas industry is predicting the discovery of more and more deep water reservoirs. Increased water depths create a requirement for reliable pipelines to economically recover these deep water fields and also to minimize flow assurance problems. Increased flow assurance problems in deeper waters increase the need for thermally insulated pipelines. In this paper we present an overview of the key issues in the analysis and design of thermal insulation systems, identify and discuss how these are addressed by the design tools developed within the DeFRIS project and present results

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20

Dola, Shahpara Sheikh, Khairul Bahsar, Mazeda Islam, and Md Mizanur Rahman Sarker. "Hydrogeological Classification and the Correlation of Groundwater Chemistry with Basin Flow in the South-Western Part of Bangladesh." Journal of Bangladesh Academy of Sciences 42, no. 1 (2018): 41–54. http://dx.doi.org/10.3329/jbas.v42i1.37831.

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Attempt has been made to find the relationship between the basin groundwater flow and the current water chemistry of south-western part of Bangladesh considering their lithological distribution and aquifer condition. The correlation of water chemistry and basin groundwater flow is depicted in the conceptual model. The water-types of shallow groundwater are predominantly Mg-Na-HCO3 and Ca- Mg-Na-HCO3 type. In the deep aquifer of upper delta plain is predominately Na-Cl, Ca-HCO3 and Mg- HCO3 type. In the lower delta plain Na-Cl type of water mainly occurs in the shallow aquifer and occasionally

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21

Goderniaux, Pascal, Philippe Davy, Etienne Bresciani, Jean-Raynald de Dreuzy, and Tanguy Le Borgne. "Partitioning a regional groundwater flow system into shallow local and deep regional flow compartments." Water Resources Research 49, no. 4 (2013): 2274–86. http://dx.doi.org/10.1002/wrcr.20186.

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22

Cherian, Deepak A., and K. H. Brink. "Shelf Flows Forced by Deep-Ocean Anticyclonic Eddies at the Shelf Break." Journal of Physical Oceanography 48, no. 5 (2018): 1117–38. http://dx.doi.org/10.1175/jpo-d-17-0237.1.

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AbstractIsolated monopolar eddies in the ocean tend to move westward. Those shed by western boundary currents may then interact with the continental margin. This simple picture is complicated by the presence of other flow features, but satellite observations show that many western boundary continental shelves experience cross-shelfbreak exchange flows forced by mesoscale eddies translating near the shelf break. Here we extend our previous study of eddy interaction with a flat shelf to that with a sloping shelf. Using a set of primitive equation numerical simulations, we address the vertical st

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23

Rahmstorf, Stefan, and Matthew H. England. "Influence of Southern Hemisphere Winds on North Atlantic Deep Water Flow." Journal of Physical Oceanography 27, no. 9 (1997): 2040–54. http://dx.doi.org/10.1175/1520-0485(1997)027<2040:ioshwo>2.0.co;2.

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24

Tian, YANG, CAO Yingchang, WANG Yanzhong, LI Ya, and ZHANG ShaoMin. "Status and Trends in Research on Deep-Water Gravity Flow Deposits." Acta Geologica Sinica - English Edition 89, no. 2 (2015): 610–31. http://dx.doi.org/10.1111/1755-6724.12451.

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25

Negre, César, Rainer Zahn, Alexander L. Thomas, et al. "Reversed flow of Atlantic deep water during the Last Glacial Maximum." Nature 468, no. 7320 (2010): 84–88. http://dx.doi.org/10.1038/nature09508.

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26

Maciel, Guilherme M., Vinicius Albuquerque Cabral, Andre Luis Marques Marcato, Ivo C. Silva Junior, and Leonardo De M. Honorio. "Daily Water Flow Forecasting via Coupling Between SMAP and Deep Learning." IEEE Access 8 (2020): 204660–75. http://dx.doi.org/10.1109/access.2020.3036487.

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27

GIDHAGEN, LARS, and BERTIL HAKANSSON. "A model of the deep water flow into the Baltic Sea." Tellus A 44, no. 5 (1992): 414–24. http://dx.doi.org/10.1034/j.1600-0870.1992.t01-4-00005.x.

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28

Gidhagen, Lars, and Bertil HÅKansson. "A model of the deep water flow into the Baltic Sea." Tellus A: Dynamic Meteorology and Oceanography 44, no. 5 (1992): 414–24. http://dx.doi.org/10.3402/tellusa.v44i5.14971.

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29

Serié, Christophe, Mads Huuse, Niels H. Schødt, James M. Brooks, and Alan Williams. "Subsurface fluid flow in the deep-water Kwanza Basin, offshore Angola." Basin Research 29, no. 2 (2016): 149–79. http://dx.doi.org/10.1111/bre.12169.

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30

Sanli, Bengi Gozmen, and Huseyin Akilli. "Effects of Permeable Cylinder on the Flow Structure in Deep Water." Fluid Dynamics 53, no. 5 (2018): 711–21. http://dx.doi.org/10.1134/s0015462818050130.

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31

Chang, Tsang-Jung, Yu-Sheng Chang, Wei-Ting Lee, and Shang-Shu Shih. "Flow uniformity and hydraulic efficiency improvement of deep-water constructed wetlands." Ecological Engineering 92 (July 2016): 28–36. http://dx.doi.org/10.1016/j.ecoleng.2016.03.028.

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32

Bodmer, Ph, and L. Rybach. "Heat flow maps and deep ground water circulation: Examples from Switzerland." Journal of Geodynamics 4, no. 1-4 (1985): 233–45. http://dx.doi.org/10.1016/0264-3707(85)90062-6.

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33

Zhu, Hong Jun, Zhi Peng Ou, Yuan Hua Lin, and Fang Fang Hu. "Large Eddy Simulations of Unsteady Wakes behind Riser in Offshore Deep Water." Advanced Materials Research 268-270 (July 2011): 787–92. http://dx.doi.org/10.4028/www.scientific.net/amr.268-270.787.

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Riser vortex-induced vibration (VIV) has been the outstanding problem affecting the normal safe operation in offshore oil exploitation. In this paper, based on computational fluid dynamics, a three-dimensional large eddy simulation (LES) numerical model was used to calculate the flow fields of unsteady flow around marine riser with different approaching flow velocities. Then streamlines, velocity and vorticity contours, drag and lift coefficients in different conditions were obtained. Simulation results indicate that the flow properties in different depth display obvious difference, which pres

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34

Kondapi, Phaneendra. "Flow Assurance." Mechanical Engineering 137, no. 03 (2015): S13—S15. http://dx.doi.org/10.1115/1.2015-mar-8.

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This article explores various aspects of flow assurance in subsea developments. Flow assurance is an understanding of multiphase flow fluid dynamics and analyses, an ability to identify flow-related problems using state-of-the-art prediction tools, and the knowledge to develop solutions that eliminate, mitigate or remediate flow-related issues encountered in subsea systems. Flow assurance is reliable, safe and cost-efficient management of hydrocarbons from reservoir to export without any flow-related issues over the life cycle of the oil field. Subsea developments continue to escalate in quant

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35

Ledwell, James R. "Comment on “Abyssal Upwelling and Downwelling Driven by Near-Boundary Mixing”." Journal of Physical Oceanography 48, no. 3 (2018): 739–48. http://dx.doi.org/10.1175/jpo-d-17-0089.1.

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AbstractMcDougall and Ferrari have estimated the global deep upward diapycnal flow in the boundary layer overlying continental slopes that must balance both downward diapycnal flow in the deep interior and the formation of bottom water around Antarctica. The decrease of perimeter of isopycnal surfaces with depth and the observed decay with height above bottom of turbulent dissipation in the deep ocean play a key role in their estimate. They argue that because the perimeter of seamounts increases with depth, the net effect of mixing around seamounts is to produce net downward diapycnal flow. Wh

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36

Pizzo, N. E., Luc Deike, and W. Kendall Melville. "Current generation by deep-water breaking waves." Journal of Fluid Mechanics 803 (August 22, 2016): 275–91. http://dx.doi.org/10.1017/jfm.2016.469.

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We examine the partitioning of the energy transferred to the water column by deep-water wave breaking; in this case between the turbulent and mean flow. It is found that more than 95 % of the energy lost by the wave field is dissipated in the first four wave periods after the breaking event. The remaining energy is in the coherent vortex generated by breaking. A scaling argument shows that the ratio between the energy in this breaking generated mean current and the total energy lost from the wave field to the water column due to breaking scales as $(hk)^{1/2}$, where $hk$ is the local slope at

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37

Wang, Nanzhe, Dongxiao Zhang, Haibin Chang, and Heng Li. "Deep learning of subsurface flow via theory-guided neural network." Journal of Hydrology 584 (May 2020): 124700. http://dx.doi.org/10.1016/j.jhydrol.2020.124700.

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38

Ju, Yong Tao, Hao Liu, Hui Yong Li, and Yu Han Shi. "Depositional Characteristics and Distribution of Lake-Floor Fan of Paleogene Lower Member 3 of Shahejie Formation in Northwestern Part of Huanghekou Sag, Bohai Bay Basin." Advanced Materials Research 347-353 (October 2011): 1299–305. http://dx.doi.org/10.4028/www.scientific.net/amr.347-353.1299.

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The lake-floor fan, as an important deposition of Paleogene in Huanghekou Sag, is characterized with both good physical character of reservoir and oil-bearing property, thus it has higher values for petroleum exploration. The lower Member 3 of Shahejie Formation, rich in sandstone, can be divided into lowstand system tract, extensive system tract and highstand system tracts based on seismic reflection signature, and core and logging data clearly. The sand bodies in the study area belonged to two kinds of lake-floor fan deposition formed under semi-deep-lake to deep-lake environment: deposition

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39

Schlitzer, Reiner. "14C in the Deep Water of the East Atlantic." Radiocarbon 28, no. 2A (1986): 391–96. http://dx.doi.org/10.1017/s0033822200007505.

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The renewal of east Atlantic deep water and its large-scale circulation and mixing have been studied in observed distributions of temperature, silicate, ΣCO2, and 14C. 14C variations in northeast Atlantic deep water below 3500m depth are small. Δ14C values range from − 100‰ to −125‰. 14C bottom water concentrations decrease from Δ14C =−117‰ in the Sierra Leone Basin to Δ14C = − 123‰ in the Iberian Basin and are consistent with a mean northward bottom water flow. The characteristic of the water that flows from the west Atlantic through the Romanche Trench into the east Atlantic was determined b

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40

Long, Xiting, Keneng Zhang, Ruiqiang Yuan, Liang Zhang, and Zhenling Liu. "Hydrogeochemical and Isotopic Constraints on the Pattern of a Deep Circulation Groundwater Flow System." Energies 12, no. 3 (2019): 404. http://dx.doi.org/10.3390/en12030404.

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Characterization of a deep circulation groundwater flow system is a big challenge, because the flow field and aqueous chemistry of deep circulation groundwater is significantly influenced by the geothermal reservoir. In this field study, we employed a geochemical approach to recognize a deep circulation groundwater pattern by combined the geochemistry analysis with isotopic measurements. The water samples were collected from the outlet of the Reshui River Basin which has a hot spring with a temperature of 88 °C. Experimental results reveal a fault-controlled deep circulation geothermal groundw

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41

Liao, Jianbo, Aihua Xi, Sujuan Liang, et al. "Genetic mechanisms of deep-water massive sandstones in continental lake basins and their significance in micro–nano reservoir storage systems: A case study of the Yanchang formation in the Ordos Basin." Nanotechnology Reviews 9, no. 1 (2020): 489–503. http://dx.doi.org/10.1515/ntrev-2020-0040.

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AbstractBased on field geological surveys of two deep-water sedimentary outcrops in the Yanchang formation of the Ordos Basin, X-ray diffraction analysis, elemental geochemical analysis, and polarizing microscope observations were conducted to investigate the causes of various sedimentary structures inside the massive sand bodies from deep-water debris flow. A genesis model of deep-water debris-flow sandstone is established: during the handling of the mass transport complexes in the basin slope, the soft sandy sedimentary layer with relatively strong shear resistance tears the soft muddy sedim

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42

Brady, Patrick, Carlos Lopez, and Dave Sassani. "Granite Hydrolysis to Form Deep Brines." Energies 12, no. 11 (2019): 2180. http://dx.doi.org/10.3390/en12112180.

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Reaction path calculations suggest that water fixation by zeolite and chlorite formation can account for much of the high salinity of deep brines in contact with deep granites, as well as their Ca/Na ratios, which reflect the rock-dominated chemistry of such brines. Resultant brines, undiluted by the influx of shallower fresher waters, are likely to be at equilibrium with laumontite, chlorite, calcite, dolomite, anhydrite/gypsum, K-feldspar, quartz, plagioclase, and possibly halite. The growth of laumontite and chlorite consumes water, causing the concentration of residual salts to increase du

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43

Lv, Xiao-fang, Jiang-wei Zuo, Yang Liu, et al. "Experimental study of growth kinetics of CO2 hydrates and multiphase flow properties of slurries in high pressure flow systems." RSC Advances 9, no. 56 (2019): 32873–88. http://dx.doi.org/10.1039/c9ra06445a.

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44

Ren, Shaoran, Yanmin Liu, Zhiwu Gong, et al. "Numerical simulation of water and sand blowouts when penetrating through shallow water flow formations in deep water drilling." Journal of Ocean University of China 17, no. 1 (2018): 17–24. http://dx.doi.org/10.1007/s11802-018-3454-5.

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45

Egorov, Alexander V., Robert I. Nigmatulin, and Aleksey N. Rozhkov. "Temperature effects in deep-water gas hydrate foam." Heat and Mass Transfer 55, no. 2 (2018): 235–46. http://dx.doi.org/10.1007/s00231-018-2403-6.

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46

Haynes, Shannon J., Kenneth G. MacLeod, Jean-Baptiste Ladant, et al. "Constraining sources and relative flow rates of bottom waters in the Late Cretaceous Pacific Ocean." Geology 48, no. 5 (2020): 509–13. http://dx.doi.org/10.1130/g47197.1.

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Abstract Geochemical data suggest that ocean circulation patterns changed over a period of long-term cooling during the last 10 m.y. of the Cretaceous (late Campanian–Maastrichtian). Proposed changes include enhanced deep-water formation in the South Atlantic and/or Indian sectors of the Southern Ocean, initiation or enhanced deep-water formation in the North Atlantic, and alternating regions of deep convection in the North and South Pacific. Existing geochemical data do not allow simple confirmation or rejection of any of these scenarios. To test Pacific circulation during the Maastrichtian,

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47

Zhang, Xiaoyuan, Shipeng Li, Baoyu Yang, and Ningfei Wang. "Flow structures of over-expanded supersonic gaseous jets for deep-water propulsion." Ocean Engineering 213 (October 2020): 107611. http://dx.doi.org/10.1016/j.oceaneng.2020.107611.

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48

Hwang, Hajung, Jinho Woo, Won-Bae Na, and Hyeon-Ju Kim. "Three-Dimensional Flow Response Analysis of Subsea Riser Transporting Deep Ocean Water." Journal of Korean Society of Coastal and Ocean Engineers 27, no. 2 (2015): 113–17. http://dx.doi.org/10.9765/kscoe.2015.27.2.113.

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49

Wenzel, Arne, Dennis Bünte, and Norbert P. Hoffmann. "Potential flow simulations of Peregrine-type deep water surface gravity wave packets." PAMM 15, no. 1 (2015): 537–38. http://dx.doi.org/10.1002/pamm.201510259.

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50

Fu, Jianhong, Yu Su, Wei Jiang, Xingyun Xiang, and Bin Li. "Multiphase flow behavior in deep water drilling: The influence of gas hydrate." Energy Science & Engineering 8, no. 4 (2020): 1386–403. http://dx.doi.org/10.1002/ese3.600.

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