Deep convection and brine rejection in the Japan Sea

Talley, Lynne D.; Лобанов, В. Б.; Пономарев, В. И.; Salyuk, A.; Tishchenko, P. Ya.; Zhabin, I. A.; Riser, Stephen C.

doi:10.1029/2002gl016451

Cited by 156 publications

(157 citation statements)

References 17 publications

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“…Another similarity is the existence of sea ice in the northern East Sea (the Sea of Japan). Sea ice in Peter the Great Bay and its role in deepwater formation through brine rejection has been addressed by Talley et al [2003]. However, little attention has been paid to sea ice in the Tatar Strait although this strait has the most extensive ice coverage in the East Sea (the Sea of Japan).…”

Section: Introductionmentioning

confidence: 99%

Relationship between satellite‐observed cold water along the Primorye coast and sea ice in the East Sea (the Sea of Japan)

Park

Kim

Cornillon

et al. 2006

Geophysical Research Letters

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The relationship between cold surface water along the Primorye coast and sea ice in the Tatar Strait of the northern East Sea (the Sea of Japan) is examined by analyzing sea surface temperatures (SST) from NOAA/AVHRR, sea ice concentrations from SSM/I, wind vectors from QuikSCAT, and position data from satellite‐tracked drifting buoys. Relatively low SSTs along the Primorye coast in spring and early summer are attributed to sea ice melted water advected to the southwest as the Liman Cold Current (LCC). Monthly to year‐to‐year variations of SSTs along the Primorye coast in spring and early summer are negatively correlated with those of the sea ice concentration in the Tatar Strait during the previous winter. Translational speeds from the surface drifter and SST anomalies demonstrate that the LCC significantly varies by 2–18 km/day both in space and time.

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Section: Introductionmentioning

confidence: 99%

Relationship between satellite‐observed cold water along the Primorye coast and sea ice in the East Sea (the Sea of Japan)

Park

Kim

Cornillon

et al. 2006

Geophysical Research Letters

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“…The location of Site U1422 was selected specifically to identify the timing of the onset of IRD events and to reconstruct temporal variations in its intensity and frequency. Because sea ice formation in this region occurred along the northwestern margin as a result of the strong winter cooling (Talley et al, 2003) that is closely related to the intensity of Siberian High (e.g., Tada, 2004), we expect the intensity of the IRD events to reflect the strength of the EAWM. Therefore, at Site U1422 we hoped to reconstruct the winter monsoon intensity through examination of IRD abundance and distribution along the northern latitudinal transect.…”

Section: Site Summaries Site U1422mentioning

confidence: 99%

“…The location of Site U1423 was selected to identify the spatial extent of IRD events and their temporal variations. Because sea ice formation in the northwestern margin of the Japan Basin occurred as a result of strong winter cooling by EAWM wind (Talley et al, 2003), we expect the intensity of the IRD events to reflect the strength of the EAWM. At Site U1423, we hoped to reconstruct EAWM intensity through examination of IRD abundance and distribution along the northern latitudinal transect in the marginal sea.…”

Section: Site U1423mentioning

confidence: 99%

“…At Site U1423, we hoped to reconstruct EAWM intensity through examination of IRD abundance and distribution along the northern latitudinal transect in the marginal sea. Because stronger EAWM wind produces deep water (JSPW) through sea ice formation in the northwestern part of the Japan Basin (Talley et al, 2003), sea ice formation and deepwater ventilation could also reflect EAWM intensity.…”

Section: Site U1423mentioning

confidence: 99%

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Expedition 346 summary

Tada¹,

Murray²,

Zarikian³

et al. 2015

Proceedings of the IODP

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Integrated Ocean Drilling Program (IODP) Expedition 346 (29 July-27 September 2013) drilled seven sites covering a wide latitudinal range in the body of water bordered by the Eurasian continent, the Korean Peninsula, and the Japanese Islands, as well as two closely spaced sites in the East China Sea. This expedition recovered 6135.3 m of core with an average recovery of 101%-a record amount of core recovered during any single IODP expedition. Expedition 346 was the first scientific drilling expedition ever to focus exclusively on the climate system in this region, which is at once so critical yet potentially vulnerable to the challenges society faces in the coming years of global climate change. With the East Asian Monsoon directly affecting the water supply of one-third of the global population, the expedition scientific results and postexpedition research that will follow have direct bearing on society's understanding of this complex atmosphereocean climate system. The high quality of materials recovered and the complete documentation of their geological, geochemical, and geophysical context will lead to an unparalleled series of future studies by the expedition Science Party as well as many other scientists over the coming decades. Cores obtained during this expedition will be used to test the hypothesis that Pliocene-Pleistocene uplift of the Himalaya and Tibetan Plateau, and the consequent emergence of the two discrete modes of Westerly Jet circulation, caused the amplification of millennial-scale variability of the East Asian summer monsoon and East Asian winter monsoon and provided teleconnection mechanism(s) for Dansgaard-Oeschger cycles.Recent and novel advances in drilling technology and newly developed analytical tools enabled collection and examination of sediment records that were impossible to acquire even a few years ago. The newly engineered half advanced piston corer enabled recovery of the deepest piston core in Deep Sea Drilling Project/ Ocean Drilling Program/IODP history (490.4 m in IODP Hole U1427A); that achievement was also the deepest continuously recovered piston cored sequence, initiated at the mudline and penetrating to ~500 m core depth below seafloor, Method A (CSF-A). Technological advances delivered a series of "new surprises" (e.g., pristine dark-light laminae from ~12 Ma sediment recovered by piston core from 410 m CSF-A at IODP Site U1425 and from 210 m CSF-A at IODP Site U1430) that will stimulate new scientific in-

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“…1 Tada et al, 1999;Tada, 2004Gamo et al, 1986Talley et al, 2003Yasuda, 1997Shcherbina et al, 200319701980Manabe and Terpstra, 1974Hahn and Manabe, 1975;Kutzubach et al, 1989;Ruddiman and Kutzbach, 1989;Kutzbach, 1992 Kutzubach et al, 1993;Prell, 1997 CO CO Raymo et al, 1988;Raymo andRuddiman, 1992 1980 e.g., Kukla and An, 1989;Ding et al, 1992;Zhang and Chen, 1995;Guo et al, 1998;Tada et al, 1999;Tada, 2004 , 62-66. Arnold, E., Merrill, J., Leinen, M. and King, J., 1995 …”

mentioning

confidence: 99%

Evolution and variability of Asian Monsoon

隆治¹

2005

Jour. Geol. Soc. Japan

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The idea that uplift of Himalaya and Tibet caused onset and enhancement of Asian Monsoon is not new, but it has never been tested because the knowledge on the timing and mode of onset and evolution of the Asian Monsoon as well as those of Himalaya and Tibet uplift has not been sufficient. Situation changed recently due to the drastic progress in reconstruction of Asian Monsoon evolution through intensive studies of loess in China as well as of hemipelagic sediments of the Japan Sea. The knowledge on the timing and process of Himalaya-Tibet uplift has also been accumulated. In addition, climate model, which is necessary to examine the linkage between Himalaya-Tibet uplift and monsoon onset and evolution, has improved drastically.In this synthesis, I summarized recent advances in our knowledge on the onset, evolution, and variability of Asian Monsoon, and reconstructed probable process of its evolution based on compilation of the paleoclimate data.

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Deep convection and brine rejection in the Japan Sea

Cited by 156 publications

References 17 publications

Relationship between satellite‐observed cold water along the Primorye coast and sea ice in the East Sea (the Sea of Japan)

Relationship between satellite‐observed cold water along the Primorye coast and sea ice in the East Sea (the Sea of Japan)

Expedition 346 summary

Evolution and variability of Asian Monsoon

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