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Journal articles on the topic 'Marine meteorology'

Author: Grafiati
Published: 4 June 2021
Last updated: 29 July 2024

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1

Xie, Lian, Bin Liu, John Morrison, Huiwang Gao, and Jianhong Wang. "Air-Sea Interactions and Marine Meteorology." Advances in Meteorology 2013 (2013): 1–3. http://dx.doi.org/10.1155/2013/162475.

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2

Yoon, Hong-Joo. "Development of Contents on the Marine Meteorology Service by Meteorology and Climate Big Data." Journal of the Korea institute of electronic communication sciences 11, no. 2 (February 25, 2016): 125–38. http://dx.doi.org/10.13067/jkiecs.2016.11.2.125.

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3

A., Balagiu. "Marine Meteorology - English versus Romanian Terminology in the 18th -19th centuries." Scientific Bulletin of Naval Academy XXI, no. 2 (December 15, 2018): 139–45. http://dx.doi.org/10.21279/1454-864x-18-i2-017.

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The marine meteorology, as a branch of meteorology, a science developed in the 18th and 19th century, has certain characteristics and its own terminology. Although words denoting natural phenomenon existed long before the science, a comparison between English and Romanian terminology in the 18th and 19th century is to establish the similarities and differences between words with the same meaning that entered the scientific vocabulary or were formed in the period mentioned.
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4

Popović, Ružica, Mirsad Kulović, and Tatjana Stanivuk. "Meteorological Safety of Entering Eastern Adriatic Ports." Transactions on Maritime Science 3, no. 1 (April 20, 2014): 53–60. http://dx.doi.org/10.7225/toms.v03.n01.006.

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Traffic and sea shipping industry are perhaps the most important economic activities in modern economic and social development of the world. Basic features and the meaning of sea shipping industry, as one of the constituent parts of multimodal transport, emerge primarily from special characteristics of the sea as a transportation way. Ports represent a great economic power; they play an essential role in the international and national economies, as well as in the global commodity exchange. They are of special importance because they are primary starting points for marine economy development. Numerous factors are relevant for the role and development of ports and port systems, and the most important ones include natural characteristics of ports, such as the depth and spatiality of the port maritime zone, shelter from winds, waves, sea currents and tides, and climate features. The recognition of the importance of meteorology for maritime activities has even changed the schooling of seamen; educational programme have been adjusted according to WMO recommendations, ships have been equipped with the state-of-the-art meteorological and navigational devices, and once the satellites were introduced the meteorological service has reached a high level of development and forecast accuracy. Therefore, marine meteorology should not be neglected; it should be given as much importance so as to become a constituent part of the skill for choosing the best and optimal shipping route. Marine meteorology (which includes the river meteorology as well) provides weather information to various maritime and river transportation activities. First of all, it refers to information on the state of wind and sea. Considering the importance of understanding the weather and climate of the area where a port is located, this paper provides a detailed overview of the climatological elements, including wind roses, for each of the presented ports: Rijeka, Zadar (Gaženica), Split (North Port), Ploče and Dubrovnik (Gruž).
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5

Kusch, Wolfgang, Reinhold Zöllner, and Frank-Ulrich Dentler. "Georg von Neumayer: his influence on marine meteorology in the German Meteorological Service." Proceedings of the Royal Society of Victoria 123, no. 1 (2011): 27. http://dx.doi.org/10.1071/rs11027.

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Georg von Neumayer achieved outstanding scientific results and created the organisational framework for the successful completion of scientific tasks. Returning from Australia, Neumayer aimed to set up in Germany a state-owned centre for marine meteorology, hydrography, navigation, marine instruments and geomagnetism, with an emphasis on scientific research with practical application of the findings. Since 1868, a successfully operating private institute, Norddeutsche Seewarte, had existed in Hamburg. This institute provided instructions for sailing routes and the optimal use of favourable winds and currents. In 1875, the institute was transformed into an imperial institution, the ‘Deutsche Seewarte’ (German Marine Observatory), with a broad spectrum of marine responsibilities including meteorological forecasts and warnings, data acquisition and management, and climatology. Its first director was Georg von Neumayer, who led it to worldwide recognition. In 1903, he retired but the Deutsche Seewarte continued in his spirit. At the end of World War II, the institute was destroyed by bombs and ceased to exist. Today, the tasks are shared between Marine Meteorological Office of the Deutscher Wetterdienst specialising in the marine meteorological and related topics and the Federal Maritime and Hydrographic Agency.
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6

Wang, Dongxiao, Yan Zhang, Lili Zeng, and Lin Luo. "Marine meteorology research progress of China from 2003 to 2006." Advances in Atmospheric Sciences 26, no. 1 (January 2009): 17–30. http://dx.doi.org/10.1007/s00376-009-0017-0.

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7

Dongxiao, Wang, Qin Zenghao, and Shi Ping. "Progress in marine meteorology studies in China during 1999–2002." Advances in Atmospheric Sciences 21, no. 3 (June 2004): 485–96. http://dx.doi.org/10.1007/bf02915575.

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8

Xu, Peng, and Ren Yuan Li. "On Cross-Strait Cooperation for Environmental Preservation at the South China Sea - An Angle of Rescue and Salvage at the Sea." Advanced Materials Research 781-784 (September 2013): 2277–82. http://dx.doi.org/10.4028/www.scientific.net/amr.781-784.2277.

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Complex geographical position and meteorology make the SCS become high-risk area of accident. In order to prevent from accident to avoid marine pollution or minimize pollution as soon as possible in the SCS, strengthening rescue and salvage is necessary. Because of characteristics of the Marine pollution and special situation in the SCS, cross-strait cooperation for marine environmental preservation in the SCS should be strengthened. In this case, cross-strait cooperation on establishing a salvage company for rescue and prevention of pollution in the SCS can integrate cross-strait salvage power to promote marine environmental preservation.
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9

Agnew, D. C. "Robert Fitzroy and the myth of the ‘Marsden Square’: Transatlantic rivalries in early marine meteorology." Notes and Records of the Royal Society of London 58, no. 1 (January 22, 2004): 21–46. http://dx.doi.org/10.1098/rsnr.2003.0223.

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Marine data (especially in meteorology) are often grouped geographically using a set of numbered 10° latitude–longitude squares known as Marsden squares, which are usually attributed to William Marsden, Secretary of the Admiralty (and Vice–President of The Royal Society), who supposedly invented them early in the nineteenth century. Available records suggest that this system was in fact probably invented by Robert FitzRoy soon after his appointment as head of the British Meteorological Office in 1854. FitzRoy felt that early English work in marine meteorology was being ignored, notably by the American Matthew Fontaine Maury, who had pioneered the collecting of marine meteorological data from ship's logs. A desire to undo this wrong led FitzRoy to emphasize earlier (though abortive) British projects by A.B. Becher (in 1831) and by Marsden (probably in the 1780s), both of which involved grouping marine data geographically, though only over limited areas. FitzRoy's treatment of this earlier work seems to have created, much later, the belief that Marsden had invented the system of 10° squares. Given both Maury's and FitzRoy's desire to demonstrate priority in this field, it is ironic that the first clear proposal to collect and group data from ship's logs was made by the American (and British) natural philosopher Isaac Greenwood in 1728.
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10

Hsu, S. A. "Some Value-Added Met-Ocean Products to the RAMMB’s TC Surface Analysis for Marine Meteorological Applications." Advances in Environmental and Engineering Research 04, no. 04 (December 20, 2023): 1–20. http://dx.doi.org/10.21926/aeer.2304054.

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In the realm of air-sea interaction and marine meteorology, during a tropical cyclone (TC) worldwide since 2006, the Regional and Mesoscale Meteorological Branch (RAMMB) has issued surface wind analysis. Based on this TC’s isotach (line of equal wind speed) analysis, in this paper, much more meteorological-oceanographic (met-ocean) products are developed and value-added to these isotachs. They are, for marine meteorology, overwater friction velocity, wind stress, atmospheric vorticity and the mean vertical velocity, and for oceanography, significant wave height, drift-current velocity, wind-stress tide and wave set-up. Furthermore, in order to estimate the wind-stress induced storm surges, two case studies are presented. They are the Extremely Severe Cyclonic Storm<strong> </strong>Nargis which devastated Myanmar in May 2008 from the Bay of Bengal and in August 2023 Hurricane Idalia which impacted northeastern Gulf of Mexico coastal region of Florida.
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11

Schulz, Eric W., Jeffrey D. Kepert, and Diana J. M. Greenslade. "An Assessment of Marine Surface Winds from the Australian Bureau of Meteorology Numerical Weather Prediction Systems." Weather and Forecasting 22, no. 3 (June 1, 2007): 613–36. http://dx.doi.org/10.1175/waf996.1.

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Abstract A method for routinely verifying numerical weather prediction surface marine winds with satellite scatterometer winds is introduced. The marine surface winds from the Australian Bureau of Meteorology’s operational global and regional numerical weather prediction systems are evaluated. The model marine surface layer is described. Marine surface winds from the global and limited-area models are compared with observations, both in situ (anemometer) and remote (scatterometer). A 2-yr verification shows that wind speeds from the regional model are typically underestimated by approximately 5%, with a greater bias in the meridional direction than the zonal direction. The global model also underestimates the surface winds by around 5%–10%. A case study of a significant marine storm shows that where larger errors occur, they are due to an underestimation of the storm intensity, rather than to biases in the boundary layer parameterizations.
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12

Füllekrug, M., C. Price, Y. Yair, and E. R. Williams. "<i>Letter to the Editor</i> Intense oceanic lightning." Annales Geophysicae 20, no. 1 (January 31, 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 morning hours, probably associated with the resurgence of oceanic mesoscale convection in coastal areas. The day-to-day variability of intense negative oceanic lightning discharges exhibits a five day periodicity, possibly related to planetary waves.Key words. Meteorology and atmospheric dynamics (lightning; ocean-atmosphere interactions) – Oceanography - general (marine meteorology)
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13

Schiano, M. E., M. Borghini, S. Castellari, and C. Luttazzi. "Climatic features of the Mediterranean Sea detected by the analysis of the longwave radiative bulk formulae." Annales Geophysicae 18, no. 11 (November 30, 2000): 1482–87. http://dx.doi.org/10.1007/s00585-000-1482-z.

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Abstract. Some important climatic features of the Mediterranean Sea stand out from an analysis of the systematic discrepancies between direct measurements of longwave radiation budget and predictions obtained by the most widely used bulk formulae. In particular, under clear-sky conditions the results show that the surface values of both air temperature and humidity over the Mediterranean Sea are larger than those expected over an open ocean with the same amount of net longwave radiation. Furthermore, the twofold climatic regime of the Mediterranean region strongly affects the downwelling clear-sky radiation. This study suggests that a single bulk formula with constant numerical coefficients is unable to reproduce the fluxes at the surface for all the seasons.Key words: Meteorology and Atmospheric dynamics (radiative processes) – Oceanography: general (marginal and semienclosed seas; marine meteorology)
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14

Poenaru, Valentina, Valerian Novac, and Razvan Bazaitu. "Methods in maritime education for analysis of factors influencing shipping and marine environment in the western part of the Black Sea." Technium Social Sciences Journal 6 (April 15, 2020): 36–40. http://dx.doi.org/10.47577/tssj.v6i1.361.

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The marine environment is a complex environment that includes both the water and the area of ​​air moving through the vessel. Depending on its mode of expression, its status parameter value, it produces direct effects, favorable and unfavorable, on navigation. Modern Meteorology and Oceanography operating methods and procedures for obtaining data for education, necessary for determining regularities that lead to phenomena and processes which occur in interdependent layers, in the marine environment and the atmosphere above the ocean (waves, storms, rain, currents, the impact on the safety of life, activities and maritime navigation challenges - in terms of visibility, stability, and immovability of the ship
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15

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 39, no. 8 (August 1992): 639–47. http://dx.doi.org/10.1016/s0198-0254(05)80003-2.

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16

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 37, no. 1 (January 1990): 17–25. http://dx.doi.org/10.1016/s0198-0254(05)80010-x.

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17

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 37, no. 5 (January 1990): 410–19. http://dx.doi.org/10.1016/s0198-0254(05)80022-6.

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18

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 4 (January 1991): 286–94. http://dx.doi.org/10.1016/s0198-0254(05)80089-5.

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19

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 2 (January 1991): 110–17. http://dx.doi.org/10.1016/s0198-0254(05)80100-1.

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20

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 1 (January 1991): 21–30. http://dx.doi.org/10.1016/s0198-0254(05)80111-6.

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21

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 7 (January 1991): 539–50. http://dx.doi.org/10.1016/s0198-0254(05)80122-0.

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22

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 12 (January 1991): 1009–14. http://dx.doi.org/10.1016/s0198-0254(05)80129-3.

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23

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 37, no. 2 (January 1990): 124–29. http://dx.doi.org/10.1016/s0198-0254(05)80139-6.

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24

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 3 (January 1991): 210–16. http://dx.doi.org/10.1016/s0198-0254(05)80146-3.

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25

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 6 (January 1991): 467–73. http://dx.doi.org/10.1016/s0198-0254(05)80156-6.

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26

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 39, no. 2 (February 1992): 117–25. http://dx.doi.org/10.1016/s0198-0254(06)80003-8.

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27

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 39, no. 3 (March 1992): 203–13. http://dx.doi.org/10.1016/s0198-0254(06)80010-5.

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28

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 39, no. 4 (April 1992): 310–20. http://dx.doi.org/10.1016/s0198-0254(06)80017-8.

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29

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 39, no. 7 (July 1992): 554–63. http://dx.doi.org/10.1016/s0198-0254(06)80024-5.

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30

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 37, no. 4 (January 1990): 296–305. http://dx.doi.org/10.1016/s0198-0254(06)80076-2.

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31

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 5 (January 1991): 370–78. http://dx.doi.org/10.1016/s0198-0254(06)80087-7.

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32

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 10 (January 1991): 827–40. http://dx.doi.org/10.1016/s0198-0254(06)80094-4.

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33

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 37, no. 3 (January 1990): 227–35. http://dx.doi.org/10.1016/s0198-0254(06)80101-9.

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34

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 39, no. 1 (January 1992): 20–27. http://dx.doi.org/10.1016/s0198-0254(06)80126-3.

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35

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 11 (January 1991): 920–30. http://dx.doi.org/10.1016/s0198-0254(06)80152-4.

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36

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 39, no. 6 (June 1992): 484–87. http://dx.doi.org/10.1016/s0198-0254(06)80159-7.

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37

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 39, no. 9 (January 1992): 734–44. http://dx.doi.org/10.1016/s0198-0254(06)80594-7.

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38

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 39, no. 5 (May 1992): 410–20. http://dx.doi.org/10.1016/s0198-0254(06)80633-3.

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39

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 8 (January 1991): 635–46. http://dx.doi.org/10.1016/s0198-0254(06)80676-x.

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40

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 39, no. 11 (November 1992): 923–32. http://dx.doi.org/10.1016/s0198-0254(06)80693-x.

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41

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 39, no. 12 (December 1992): 1003–10. http://dx.doi.org/10.1016/s0198-0254(09)90016-4.

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42

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 37, no. 11 (January 1990): 994–1005. http://dx.doi.org/10.1016/s0198-0254(09)90026-7.

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43

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 37, no. 9 (January 1990): 791–800. http://dx.doi.org/10.1016/s0198-0254(09)90034-6.

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44

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 37, no. 7 (January 1990): 586–98. http://dx.doi.org/10.1016/s0198-0254(09)90044-9.

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45

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 9 (January 1991): 725–41. http://dx.doi.org/10.1016/s0198-0254(09)90052-8.

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46

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 32, no. 10 (January 1985): 799–806. http://dx.doi.org/10.1016/0198-0254(85)90023-8.

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47

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 32, no. 11 (January 1985): 911–17. http://dx.doi.org/10.1016/0198-0254(85)90037-8.

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48

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 32, no. 3 (January 1985): 174–78. http://dx.doi.org/10.1016/0198-0254(85)90087-1.

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49

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 32, no. 7 (January 1985): 514–20. http://dx.doi.org/10.1016/0198-0254(85)90105-0.

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50

"Marine meteorology." Deep Sea Research Part B. Oceanographic Literature Review 36, no. 7 (January 1989): 556–63. http://dx.doi.org/10.1016/0198-0254(89)92629-0.

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