Enhanced chlorophyll associated with island-induced cyclonic eddies in the eastern channel of the Tsushima Straits

2009 ◽  
Vol 81 (3) ◽  
pp. 401-408 ◽  
Author(s):  
Goh Onitsuka ◽  
Akihiko Morimoto ◽  
Tetsutaro Takikawa ◽  
Atsushi Watanabe ◽  
Masatoshi Moku ◽  
...  
2009 ◽  
Vol 65 (1) ◽  
pp. 61-71 ◽  
Author(s):  
Akihiko Morimoto ◽  
Tetsutaro Takikawa ◽  
Goh Onitsuka ◽  
Atsushi Watanabe ◽  
Masatoshi Moku ◽  
...  

2005 ◽  
Vol 35 (6) ◽  
pp. 1154-1168 ◽  
Author(s):  
Tetsutaro Takikawa ◽  
Jong-Hwan Yoon ◽  
Kyu-Dae Cho

Abstract Current structures across the Tsushima Straits are studied using results from long-term acoustic Doppler current profiler (ADCP) observations by a ferryboat between Hakata and Pusan conducted since February 1997. Two maxima of the northeastward current are observed in the central parts of the eastern and western channels, and the maximum velocity in the western channel is stronger than that of the eastern channel. Downstream of the Tsushima Islands, a southwestward countercurrent is observed associated with a pair of cyclonic and anticyclonic eddies. In the western channel, the deep countercurrent is observed pronouncedly on the bottom slope of the Korean side from summer to winter. The volume transport of the Tsushima Warm Current through the straits has strong seasonal variation with a minimum in January and two maxima from spring to autumn (double peaks). The spring peak of the volume transport through the eastern channel is more pronounced than the autumn peak, and the autumn peak of the western channel is more pronounced than the spring peak. The inflow volume transport into the Japan Sea through the western channel significantly increases in autumn because of an incrementation of the freshwater transport. The total volume transport averaged over the observation period (5.5 yr) is 2.64 Sv (Sv ≡ 106 m3 s−1). The average volume transports through the eastern and western channels are 1.10 and 1.54 Sv, respectively.


1965 ◽  
Vol 5 (41) ◽  
pp. 651-660 ◽  
Author(s):  
N. A. Ostenso ◽  
P. V. Sellmann ◽  
T. L. Péwé

AbstractAs an extension of an intensive study of Gulkana Glacier a 42 station gravimeter survey was made to gain some insight into its third dimension. This survey showed that the glacier’s main tongue occupies a complex valley composed essentially of two parallel channels separated by a medial ridge which extends southward from rock bastions in the accumulation zone. At mid-glacier the ice thickness in the larger eastern channel is 225 m., in contrast to 130 m. in the western channel. The medial ridge degenerates down-glacier probably disappearing within 2 km. of the glacier terminus. The basic surface flow pattern of the glacier described by Moores can be adequately explained by this basal topography. Seasonal velocity variations are possibly caused by melt-water basal lubrication with one channel being favored over the other at different times of the year, in agreement with observations by Elliston on the Gorner-Gletscher, Switzerland, and with the glacier sliding theory of Weertman.


Author(s):  
N. A. Holme

The brittle-star Ophiothrix fragilis forms dense aggregations on the sea bed off Plymouth, as well as in other parts of the English Channel. From about 1970 there was a marked decline in populations off Plymouth, and study of previous records suggests that there have from time to time been considerable fluctuations in abundance of this species — since beds were first reported by E. J. Allen in the 1890s. The decline did not extend to populations in the southern and eastern parts of the Channel. The distribution of Ophiocomina nigra, which sometimes occurs in mixed populations with Ophiothrix, is also described. This species is more or less limited to the western Channel, and populations, which are nowhere very dense, showed no decline comparable to that of Ophiothrix.Predation by the starfish Luidia ciliaris and L. sarsi is thought to be a likely cause of the disappearance of Ophiothrix. Luidia spp. are active predators on ophiuroids and other echinoderms, and numbers of L. ciliaris were observed in the vicinity of the Ophiothrix beds at the time of the decline. Both species of Luidia have a ’western’ distribution in the Channel, and showed an increase in density off Plymouth after the late 1960s, which is probably related to a changeover from a Sagitta setosa to a 5. elegans plankton community from 1968 on. The distribution of these Luidia is confined to stratified waters in the western Channel, surviving stocks of Ophiothrix being limited to mixed waters in the southern and eastern Channel where Luidia does not occur.


1957 ◽  
Vol 65 (4) ◽  
pp. 433-441 ◽  
Author(s):  
Shannon R. Torphy ◽  
John M. Zeigler

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