scholarly journals Robert C. Stern, Scratch One Flattop: The First Carrier Air Campaign and the Battle of the Coral Sea (Lisle A. Rose)

2021 ◽  
Vol 30 (1) ◽  
pp. 105-106
Author(s):  
Lisle A. Rose
Keyword(s):  
2002 ◽  
Vol 54 (4) ◽  
pp. 655-668 ◽  
Author(s):  
R. Brinkman ◽  
E. Wolanski ◽  
E. Deleersnijder ◽  
F. McAllister ◽  
W. Skirving

2012 ◽  
Vol Special2012 (7) ◽  
pp. 45-57 ◽  
Author(s):  
Jason Coughran ◽  
Kathryn L. Dawkins ◽  
Rod Hobson ◽  
James M. Furse
Keyword(s):  

Author(s):  
Daniela M. Ceccarelli
Keyword(s):  

1980 ◽  
Vol 31 (4) ◽  
pp. 415 ◽  
Author(s):  
E Wolanski ◽  
M Jones

Weather and currents at eight sites were measured and drogue trajectories obtained in July 1979 at Britomart Reef, a middle reef located at 18�16'S.,146� 38'E. in the central region of the Great Barrier Reef province. The longest current records (3 weeks) were obtained at two sites in passes between the Coral Sea and the Great Barrier Reef Lagoon where westerly currents modulated by tides were observed. Analysis of residuals also showed the importance of wind-driven secondary circulation. Non-tidal sea-level oscillations were very small. Shorter current records (1-10 days) at six sites in the lagoon and on the reef flat showed a predominant northerly flow, also modulated by tides and wind. A residual anticlockwise water circulation existed in the lagoon where flushing was controlled more by winds than by tides. The rise in sea level over the reef flat as a result of waves breaking was negligible. Temperature differences between air and water accounted for the cooling of the water column during the expedition. Constant south-east trade winds were experienced at the reef, while on land the wind was weaker. more variable, and often dominated by land-sea breezes.


1978 ◽  
Vol 9 (3) ◽  
pp. 82-87 ◽  
Author(s):  
John C. Mutter ◽  
Garry Karner
Keyword(s):  

1998 ◽  
Vol 49 (6) ◽  
pp. 475 ◽  
Author(s):  
John Hampton ◽  
John Gunn

Yellowfin tuna (Thunnus albacares) and bigeye tuna (T. obesus) were tagged and released in the north-western Coral Sea off northern Queensland in 1991 and 1992. Over the next five years, recaptures were reported by Australian longline vessels based in Cairns and fishing in the release area, and by industrial tuna fleets fishing in the adjacent western Pacific region, thus demonstrating clear links between the tuna stocks in these areas. Some southerly movements of yellowfin, in particular, further suggested links with stocks supporting the longline fishery in the south-eastern Australian Fishing Zone. Bigeye tuna tag returns and catch per unit effort by Cairns-based longliners showed a strong seasonal signal, peaking in mid year. Yellowfin tag-return data displayed a similar, but weaker, seasonal pattern. The data were analysed by use of tag-attrition models with seasonally variable catchability and with two assumptions regarding changes in targeting of the two species by longliners during the study. Under both assumptions, the local exploitation rates for yellowfin are low: about 0.07 in 1996. For bigeye, the local exploitation rate in 1996 may have been as high as 0.30, warranting a cautious approach to further fishery expansion in this area.


2018 ◽  
Author(s):  
François Carlotti ◽  
Marc Pagano ◽  
Loïc Guilloux ◽  
Katty Donoso ◽  
Valentina Valdés ◽  
...  

Abstract. This paper presents results on the spatial and temporal distribution patterns of mesozooplankton in the western tropical South Pacific along the 20 °S south visited during austral summer (February–April 2015). By contributing to the interdisciplinary OUTPACE (Oligotrophy to UlTra-oligotrophy PACific Experiment) project (Moutin et al., 2017), the specific aims of this study dedicated to mesozooplankton observations were (1) to document the responses of zooplankton in terms of species diversity, density and biomass along the transect, and (2) to characterize the trophic pathways from primary production to large mesozooplanktonic organisms. Along a West-East transect of 4000 km from New Caledonia to the French Polynesia, 15 short-duration stations (SD-1 to SD-15, 8 hours each) dedicated to a large-scale description, and three long-duration stations (LD-A to LD-C, 5days each), respectively positioned (1) in offshore northern waters of New Caledonia, (2) near Niue Island, and (3) in the subtropical Pacific gyre near the Cook Islands, were sampled with a Bongo Net with 120 μm mesh size net for quantifying mesozooplankton abundance, biomass, community taxonomy and size structure, and size fractionated content of δ15N. Subsequently, the contribution of Diazotroph Derived Nitrogen (DDN (%) to zooplankton δ15N (ZDDN) values at each station was calculated, as well as an estimation of zooplankton carbon demand and grazing impact and of zooplankton excretion rates. The mesozooplankton community showed a general decreasing trend in abundance and biomass from West to East, with a clear drop in the ultra-oligotrophic waters of the subtropical Pacific gyre (LD-C, SD-14 and SD-15). Higher abundance and biomass corresponded to higher primary production of more or less ephemeral blooms linked to complex mesoscale circulation in the Coral Sea and between the longitudes 170–180 °W. Copepods were the most abundant group (68 to 86 % of total abundance), slightly increasing in contribution from west to east while, in parallel, gelatinous plankton decreased (dominated by appendicularians) and other holoplankton. Detritus in the net tow samples represented 20–50 % of the biomass, the lowest and the highest values being obtained in the subtropical Pacific gyre and in the Coral Sea, respectively, linked to the local primary production and the biomass and growth rates of zooplanktonic populations. Taxonomic compositions showed a high degree of similarity across the whole region, however, with a moderate difference in subtropical Pacific gyre. Several copepod taxa, known to have trophic links with Trichodesmium, presented positive relationships with Trichodesmium abundance, such as the Harpacticoids Macrosetella, Microsetella and Miracia, and the Poecilostomatoids Corycaeus and Oncaea. At the LD stations, the populations initially responded to local spring blooms with a large production of larval forms, reflected in increasing abundances but with limited (station LD-A) or no (station LD-A) biomass changes. Diazotrophs contributed up to 67 and 75 % to zooplankton biomass in the western and central Melanesian Archipelago regions respectively, but strongly decreased to an average of 22 % in the subtropical Pacific gyre (GY) and down to 7 % occurring in the most eastern station (SD-15). Using allometric relationships, specific zooplankton ingestion rates were estimated between 0.55 and 0.64 d−1 with the highest mean value at the bloom station (LD-B) and the lowest in GY, whereas estimated weight specific excretion rates ranged between 0.1 and 0.15 d−1 for NH4 and between 0.09 and 9.12 d−1 for PO4. Daily grazing pressure on phytoplankton stocks and daily regeneration by zooplankton were as well estimated for the different regions showing contrasted impacts between MA and GY regions. For the 3 LD stations, it was not possible to find any relationship between the abundance and biomass in the water column and swimmers found in sediment traps. Diel vertical migration of zooplankton, which obviously occurs from observed differences in day and night samples, might strongly influence the community of swimmers in traps.


PLoS ONE ◽  
2011 ◽  
Vol 6 (2) ◽  
pp. e16312 ◽  
Author(s):  
Andrew J. Dunstan ◽  
Peter D. Ward ◽  
N. Justin Marshall

1970 ◽  
Vol 8 (3-4) ◽  
pp. 229-244 ◽  
Author(s):  
Edward L. Winterer
Keyword(s):  

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