(PDF) Kuroshio And Oyashio Currents (2001) | Bo Qiu | 187 Citations (2024)

Book ChapterDOI

Bo QiuUniversity of Hawaii at Manoa

- pp 1413-1425

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187Citations

TL;DR: In this paper, the importance of euphausiids in marine food webs throughout the world’s oceans has been discussed, and they are potentially important indicator species for detecting and understanding climate change effects.

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Abstract:Salps compete with krill for phytoplankton } in poor sea ice years salp numbers are increased and krill recruitment is reduced. Further north in their range, E. superba abundance is dependent on the transport of krill in the ocean currents as well as Suctuations in the strength of particular cohorts. Given the importance of euphausiids in marine food webs throughout the world’s oceans, they are potentially important indicator species for detecting and understanding climate change effects. Changes in ocean circulation or environmental regimes will be reSected in changes in growth, development, recruitment success, and distribution. These effects may be most notable at the extremes of their distribution where any change in the pattern of variation will result in major changes in food web structure. Given their signiRcance as prey to many commercially exploited species, this may also have a major impact on harvesting activities. A greater understanding of the large-scale biology of the euphausiids and the factors generating the observed variability is crucial. Obtaining good long-term and large-scale biological and physical data will be fundamental to this process.

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Citations

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Open Access

Journal Article

DOI

The Kuroshio Extension Bifurcation Region: A pelagic hotspot for juvenile loggerhead sea turtles

Jeffrey J. Polovina, +5 moreDole Food Company,Joint Institute for Marine and Atmospheric Research,National Oceanic and Atmospheric Administration

- 01 Feb

2006-

Deep-sea Research Part Ii-topical Studie...

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Abstract: Satellite telemetry of 43 juvenile loggerhead sea turtles (Caretta caretta) in the western North Pacific together with satellite-remotely sensed oceanographic data identified the Kuroshio Extension Bifurcation Region (KEBR) as a forage hotspot for these turtles. In the KEBR juvenile loggerheads resided in Kuroshio Extension Current (KEC) meanders and the associated anti-cyclonic (warm core) and cyclonic (cold core) eddies during the fall, winter, and spring when the KEC water contains high surface chlorophyll. Turtles often remained at a specific feature for several months. However, in the summer when the KEC waters become vertically stratified and surface chlorophyll levels are low, the turtles moved north up to 600 km from the main axis of KEC to the Transition Zone Chlorophyll Front (TZCF). In some instances, the loggerheads swam against geostrophic currents, and seasonally all turtles moved north and south across the strong zonal flow. Loggerhead turtles traveling westward in the KEBR had their directed westward movement reduced 50% by the opposing current, while those traveling eastward exhibited an increase in directed zonal movement. It appears, therefore, that these relatively weak-swimming juvenile loggerheads are not passive drifters in a major ocean current but are able to move east, west, north, and south through this very energetic and complex habitat. These results indicate that oceanic regions, specifically the KEBR, represent an important juvenile forage habitat for this threatened species. Interannual and decadal changes in productivity of the KEBR may be important to the species’s population dynamics. Further, conservation efforts should focus on identifying and reducing threats to the survival of loggerhead turtles in the KEBR. r 2006 Elsevier Ltd. All rights reserved.

172

Journal Article

DOI

The Pliocene to recent history of the Kuroshio and Tsushima Currents: a multi-proxy approach

Stephen J. Gallagher, +5 moreUniversity of Melbourne,Shizuoka University,Tohoku University,National Institute of Advanced Industrial Science and Technology,Hokkaido University

- 27 Jun

2015-

Progress in Earth and Planetary Science

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TL;DR: Foraminiferal proxy data suggests eastward deflection of the Kuroshio Current from its present path at 24 °N into the Pacific Ocean due to East Taiwan Channel restriction during the Last Glacial Maximum.

131

Journal Article

DOI

An overview of the Oyashio ecosystem

Yasunori SakuraiHokkaido University

- 01 Nov

2007-

Deep-sea Research Part Ii-topical Studie...

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TL;DR: The Oyashio shelf region and the seasonally ice-covered areas north of Hokkaido are highly productive, supporting a wide range of species including marine mammals, seabirds and commercially important species in the western subarctic Pacific as discussed by the authors.

109

Journal Article

DOI

Dissolved and labile particulate Zr, Hf, Nb, Ta, Mo and W in the western North Pacific Ocean

M. Lutfi Firdaus, +4 moreKyoto University

- 01 Apr

2008-

Journal of Oceanography

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TL;DR: In this paper, a portion of seawater for dissolved species (D) was passed through a 0.2 µm Nuclepore filter and acidified to pH 2.2 with HCl and HF.

90

Journal Article

DOI

Sediment core record of global fallout and Bikini close-in fallout Pu in Sagami Bay, western Northwest Pacific margin

Jian Zheng, +1 moreNational Institute of Radiological Sciences

- 01 Jul

2004-

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TL;DR: To the best of the knowledge, this is the first report that Pu contamination, which originated from Bikini and Enewetak nuclear weapon test series in the 1950s, has extended westwards as far as the Japanese coast.

83

References

PDF

Open Access

Book

Regional Oceanography: An Introduction

Matthias Tomczak, +1 more

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TL;DR: In this article, what drives the ocean currents? temperature, salinity, density and the oceanic pressure field the Coriolis force, geostropy, Rossby waves and the westwood intensification Ekman layer transports, Ekman pumping and the Sverdrup balance water mass formation, subduction and oceanic heat budget Antarctic oceanography Arctic oceanography.

1,261

Book

Descriptive Physical Oceanography : An Introduction

George L. Pickard

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TL;DR: In this paper, the authors describe ocean dimensions, shapes and bottom materials Physical properties of sea-water Typical distributions of water characteristics in the oceans Water, salt and heat budgets of the oceans Instruments and methods Circulation and water masses of oceans Coastal oceanography Some directions for future work Appendix Bibliography Index.

925

Beginning of the Kuroshio

H. Nitani

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592

Journal Article

DOI

Annual and Interannual Variability in the Kuroshio Current System

Keisuke Mizuno, +1 moreScripps Institution of Oceanography

- 01 Oct

1983-

Journal of Physical Oceanography

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TL;DR: In this article, a composite of the paths of the Kuroshio (i.e., the 12°C isotherm) from the individual seasonal maps, and the total variance map, finds nodes (minima) and anti-nodes (e.g., maxima) of variability to have existed along the mean Kuroshia path.

315

Journal Article

DOI

Variations of Current Path, Velocity, and Volume Transport of the Kuroshio in Relation with the Large Meander

Masaki KawabeUniversity of Tokyo

- 01 Dec

1995-

Journal of Physical Oceanography

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TL;DR: In this paper, the variations of the Kuroshio current path and their relations with current velocity, volume transport, and upstream position were examined using sea level data, and it was shown that the formation and decay of the large meander are associated with the velocity and position of the kokara Strait south of Kyushu.

302

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(PDF) Kuroshio And Oyashio Currents (2001) | Bo Qiu | 187 Citations (2024)

FAQs

What is the answer to the Kuroshio Current? ›

Explanation: The Kuroshio is a north-flowing, warm ocean current on the west side of the North Pacific Ocean.

What are the Oyashio and Kuroshio currents? ›

The Kuroshio and Oyashio currents are the western boundary currents in the wind-driven, subtropical, and subarctic circulations of the North Pacific Ocean. Translated from Japanese, Kuroshio literally means black (“kuro”) stream (“shio”) owing to the blackish— ultramarine to cobalt blue—color of its water.

How do Oyashio Current and Kuroshio Current affect the northeastern part and southern part of Japan? ›

Cold Oyashio currents affects: - the cold oyashio current lowers the temperature in northeast Asia drastic as it moves southeast from the Bering Strait. On the other hand, the warm Kuroshio 6Current, of East coast of Japan, raises its coastal temperature considerably.

Where is the Kuroshio Current in the ocean basin? ›

The Kuroshio Current is one of the major ocean currents. It begins east of the Philippines then flows in a northeastward direction past Taiwan and Japan. It forms the western side of the clockwise North Pacific Ocean gyre.

What does Kuroshio mean in Japanese? ›

It is called Kuroshio (“Black Current”) because it appears a deeper blue than does the sea through which it flows. The Editors of Encyclopaedia Britannica.

What do you mean by Oyashio? ›

noun. a cold ocean current flowing southwest from the Bering Sea, east of the Kuril Islands, along the east coast of Japan where it meets the Japan Current.

Why is the Kuroshio Current important? ›

The Kuroshio Current plays an important role in influencing regional climate and weather patterns mainly through the input of warm waters from lower latitudes northward into the western edge of the Pacific basin.

How does the Oyashio Current affect the climate? ›

Thus, a northward shift in the current location of the Kuroshio Current would result in a decrease of organic carbon and carbonate abundances. Conversely, a southward shift of the Oyashio Current would cause increased productivity and would likely be associated with colder climates.

How deep is the Oyashio Current? ›

The Oyashio Current is strongest in spring, and the presence of cold current water in Volcano Bay continues till June (Ohtani et al, 1971). This bowl-shaped bay is about 2,300 km2 with a mean depth of 59 m. Surface temperature of Oyashio water varies seasonally from about 0°C in early spring to 20°C in the summer.

Is the Kuroshio Current cold or warm? ›

The Kuroshio Current (黒潮, Kuroshio, literally “Black Current”, named after the deeper blue colour of its waters), and is also known as the Japan Current. The Kuroshio is a warm water, north-flowing current, which transports warm, and tropical water northward toward the polar region.

Is the Kuroshio Current fast or slow? ›

The Kuroshio current is a strong ocean current in the western North Pacific Ocean. The current flow is approximately 500 m deep and 100 km wide with a flow speed of 1–1.5 m/s [4–6].

What marine life is in the Kuroshio Current? ›

Various species of tuna, sardine and anchovy, mackerel, squid and many other commercially important species are each found in specific zones in and near the Kuroshio. For example, fronts where coastal and offshore waters meet are often good fishing grounds.

What is the fact about the Kuroshio Current? ›

EVERY second the Kuroshio current carries some 50 million tonnes of sea water past Japan's southeast coast-a flow equal in volume to about 6000 rivers the size of the Danube or Volga. But even this massive current would take some 250 years to equal the total volume of the north Pacific.

Why is Kuroshio Current called black current? ›

The Japanese named it Kuroshio, or black current, for its dark, cobalt blue waters. Physical oceanographer Steven Jayne said, “The Kuroshio is the strongest current in the Pacific Ocean, and is also one of the most intense air-sea heat exchange regions on the globe. It influences climate as far as North America.”

How do the Kamchatka Current and Kuroshio Current? ›

Answer: Explanation: The Kamchatka current acts like a conveyor belt that brings cold water to the Northeastern part of Japan which makes the temperature low (colder). The Kuroshio current on the other hand brings warm water to the Southern part of Japan which makes the temperature high (warmer).

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