Feeding methods and diving rates of migrating larids off Deer Island, New Brunswick

1982 ◽  
Vol 60 (9) ◽  
pp. 2190-2197 ◽  
Author(s):  
B. M. Braune ◽  
D. E. Gaskin

A study of three species of migrating larids was undertaken off Deer Island, New Brunswick, to compare feeding methods and diving rates of birds exploiting various prey types. Bonaparte's Gulls (Larus Philadelphia) fed mainly by diving (dipping and plunging) and surface seizing, whereas Common and Arctic Terns (Sterna hirundo and S. paradisaea) acquired food by diving only. Common and Arctic Terns foraged from greater heights than Bonaparte's Gulls, and both the gulls and the terns maintained a higher foraging height while feeding on small fish than while feeding on euphausiids or, in the case of the gulls, insects. Common and Arctic Terns had a steeper dive angle than Bonaparte's Gulls, and both the gulls and the terns dove more steeply when feeding on small fish than on euphausiids. The highest diving rate occurred when Bonaparte's Gulls were dipping for insects trapped in the water surface layer. There was no significant difference in mean dipping or plunging rates between the gulls and the terns feeding on euphausiids or small fish. Bonaparte's Gulls had a lower mean rate of incomplete dives than did terns, probably because of the gulls' lesser aerial manoeuverability reducing the likelihood of altering course after dive initiation. The mean dipping rate was higher than the mean plunging rate for both the gulls and the terns since most food was taken at the surface, and plunges were necessary only for deeper prey (usually small fish). Intervals between hovering and diving were similar for both the gulls and the terns.

1982 ◽  
Vol 104 (1) ◽  
pp. 34-39 ◽  
Author(s):  
B. M. Howe ◽  
A. J. Chambers ◽  
S. P. Klotz ◽  
T. K. Cheung ◽  
R. L. Street

The velocity and temperature fields on both sides of an air-water interface were examined experimentally in order to understand better the physical processes of momentum and heat transfer through the surface layers about the interface. An examination of temperature and velocity profiles plotted in “law-of-the-wall” coordinates leads to the conclusion that, both in the air and in the water, the mechanism of momentum transfer is affected by surface roughness changes, but the mechanism of heat transfer is not. In the water surface layer the velocity fluctuations due to the wave-related motions are of the same order as the purely turbulent motions. The turbulent components closely resemble those found in boundary layers over solid walls. The measured total energy flux from the interface agrees well with the measured single-phase, vertical heat transport through the water surface layer.


2010 ◽  
Vol 41 (2) ◽  
pp. 411-419 ◽  
Author(s):  
Ana Fernández Scavino ◽  
Javier Menes ◽  
Lucía Ferrando ◽  
Silvana Tarlera

2003 ◽  
Vol 83 (22) ◽  
pp. 4506-4508 ◽  
Author(s):  
N. T. Cherpak ◽  
A. A. Barannik ◽  
Yu. V. Prokopenko ◽  
T. A. Smirnova ◽  
Yu. F. Filipov

2018 ◽  
Author(s):  
Ye Tian ◽  
Chao Xue ◽  
Chun-Ying Liu ◽  
Gui-Peng Yang ◽  
Pei-Feng Li ◽  
...  

Abstract. Nitric oxide (NO) is a short-lived compound of the marine nitrogen cycle; however, our knowledge about its oceanic distribution and pathways is rudimentary. Here we present the measurements of dissolved NO in the surface and bottom layers at 75 stations in the Bohai Sea (BS) and Yellow Sea (YS) in June 2011. Moreover, NO photoproduction rates were determined at 27 stations in both seas. The NO concentrations in the surface and bottom layers were highly variable and ranged from below the detection limit (i.e. 32 pmol L−1) to 616 pmol L−1 in the surface layer and to 482 pmol L−1 in the bottom layer. There was no significant difference between the mean NO concentrations in the surface (186 ± 108 pmol L−1) and bottom (174 ± 123 pmol L−1) layers. A decreasing trend of NO bottom layer concentrations salinity indicates a NO input by submarine groundwater discharge. NO in the surface layer was supersaturated at all stations during both day and night and therefore the BS and YS were a persistent source of NO to the atmosphere at the time of our measurements. The accumulation of NO during daytime was resulting from photochemical production and photoprodcution rates were correlated to illuminance. The persistent nighttime NO supersaturation pointed to a, so far unknown, NO dark production. NO sea-to-air flux densities were much lower than the NO photoproduction rates. Therefore, we conclude that the bulk of the NO produced in the mixed layer was rapidly consumed before its release to the atmosphere. Overall, the oceanic NO emissions to the atmosphere were negligible compared to anthropogenic NOx sources such as emissions from ships.


2018 ◽  
Vol 478 (2) ◽  
pp. 268-273
Author(s):  
A. P. Lisitzin ◽  
V. N. Lukashin ◽  
A. N. Novigatsky ◽  
A. A. Klyuvitkin ◽  
O. M. Dara ◽  
...  

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