1985
DOI: 10.1007/bf02109033
|View full text |Cite
|
Sign up to set email alerts
|

Bottom currents in Nankai Trough and Sagami Trough

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

0
6
0

Year Published

1986
1986
2022
2022

Publication Types

Select...
7
1

Relationship

1
7

Authors

Journals

citations
Cited by 18 publications
(6 citation statements)
references
References 7 publications
0
6
0
Order By: Relevance
“…The first survey around the islands (K6 and K7) also showed higher densities in the immediate and eastern regions, especially in the lower epipelagic layer ( Figure 3b). As it is known that one of the branches of Oyashio, the western boundary current of the western subarctic gyre, reaches Sagami Bay or flows westward from the Izu Islands (Marumo, 1966;Sekine & Uchiyama, 2002;Senjyu, Asano, Matsuyama, & Ishimaru, 1998;Taira & Teramoto, 1985;Yang, Nagata, Taira, & Kawabe, 1993a, 1993b, the higher densities are attributed to the influence of Oyashio water. In the Kuroshio Extension area, the highest water density (lowest temperature and salinity) was shown north of the axis (Oyashio side) on the eastern side of…”
Section: Characteristics Of the Water Massmentioning
confidence: 99%
“…The first survey around the islands (K6 and K7) also showed higher densities in the immediate and eastern regions, especially in the lower epipelagic layer ( Figure 3b). As it is known that one of the branches of Oyashio, the western boundary current of the western subarctic gyre, reaches Sagami Bay or flows westward from the Izu Islands (Marumo, 1966;Sekine & Uchiyama, 2002;Senjyu, Asano, Matsuyama, & Ishimaru, 1998;Taira & Teramoto, 1985;Yang, Nagata, Taira, & Kawabe, 1993a, 1993b, the higher densities are attributed to the influence of Oyashio water. In the Kuroshio Extension area, the highest water density (lowest temperature and salinity) was shown north of the axis (Oyashio side) on the eastern side of…”
Section: Characteristics Of the Water Massmentioning
confidence: 99%
“…The variance between I 0 and 30 hours periods, occupied mainly by tidal current energy, are shown to be 42-82% of the total variance. Although no detailed analysis associated with the tidal periods have been made by Taira and Teramoto (1985), the strong tidal currents are likely to exist even near the sea bottom south of the Suruga Trough.…”
Section: Summary and Discussionmentioning
confidence: 98%
“…The strong tidal currents were actually experienced in the axial floor of Suruga Bay during submersible dives (Otsuka and Niitsuma, 1985;Midorikawa et al, 1988). Taira and Teramoto (1985) carried out long-term current measurements near the sea bottom south of the Suruga Trough for about one year. The current meters were set at 7 m above the sea bottom at Stn.…”
Section: Summary and Discussionmentioning
confidence: 99%
“…Significantly different clusters formed during different seasons at 100 m depths (clusters 1, 3 and 4 for eukaryotic community and clusters 1 and 4-3 for bacterial community). Upwelling of deep seawater supplies rich nutrients to the coastal areas from Sagami Trough (more than 1000 m deep), located in the centre of the Bay (Takahashi et al 1980;Taira and Teramoto 1985;Kawabe and Yoneo 1987). In our study, deep-waters, rich in nutrients, were supplied to deeper layers (100 m) when vertical mixing weakened.…”
Section: Overall Plankton Community and Diversity Dynamicsmentioning
confidence: 99%