Weakened pacific overturning circulation, winter monsoon dominance and tectonism re-organized Japan Sea paleoceanography during the Late Miocene global cooling

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Location: Deutsche Nationalbibliothek Frankfurt am Main

ISSN: 2045-2322

Extent: Online-Ressource

Language: Englisch

Notes: online resource.

Bibliographic citation: Weakened pacific overturning circulation, winter monsoon dominance and tectonism re-organized Japan Sea paleoceanography during the Late Miocene global cooling ; volume:12 ; number:1 ; day:20 ; month:7 ; year:2022 ; pages:1-12 ; date:12.2022
Scientific reports ; 12, Heft 1 (20.7.2022), 1-12, 12.2022

Creator: Matsuzaki, Kenji M.
Ikeda, Masayuki
Tada, Ryuji

Contributor: SpringerLink (Online service)

DOI: 10.1038/s41598-022-15441-x

URN: urn:nbn:de:101:1-2022082520513917728425

Rights: Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.

Last update: 15.08.2025, 7:34 AM CEST

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Matsuzaki, Kenji M.
Ikeda, Masayuki
Tada, Ryuji
SpringerLink (Online service)

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Weakened pacific overturning circulation, winter monsoon dominance and tectonism re-organized Japan Sea paleoceanography during the Late Miocene global cooling

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Other Objects (12)

Re-organization of Pacific overturning circulation across the Miocene Climate Optimum

Late Miocene climate cooling and intensification of southeast Asian winter monsoon

Regional climate model experiments to investigate the Asian monsoon in the Late Miocene

Regional climate model experiments to investigate the Asian monsoon in the Late Miocene

South Asian summer monsoon enhanced by the uplift of Iranian Plateau in Middle Miocene

South Asian summer monsoon enhanced by the uplift of Iranian Plateau in Middle Miocene

Late Miocene Tarim desert wetting linked with eccentricity minimum and East Asian monsoon weakening

Dominance of climate warming effects on recent drying trends over wet monsoon regions

South Asian summer monsoon enhanced by the uplift of the Iranian Plateau in Middle Miocene

Strong winter monsoon wind causes surface cooling over India and China in the Late Miocene

Secular and orbital-scale variability of equatorial Indian Ocean summer monsoon winds during the late Miocene

Secular and orbital-scale variability of equatorial Indian Ocean summer monsoon winds during the late Miocene

Re-organization of Pacific overturning circulation across the Miocene Climate Optimum

Late Miocene climate cooling and intensification of southeast Asian winter monsoon

Regional climate model experiments to investigate the Asian monsoon in the Late Miocene

Regional climate model experiments to investigate the Asian monsoon in the Late Miocene

South Asian summer monsoon enhanced by the uplift of Iranian Plateau in Middle Miocene

South Asian summer monsoon enhanced by the uplift of Iranian Plateau in Middle Miocene

Late Miocene Tarim desert wetting linked with eccentricity minimum and East Asian monsoon weakening

Dominance of climate warming effects on recent drying trends over wet monsoon regions

South Asian summer monsoon enhanced by the uplift of the Iranian Plateau in Middle Miocene

Strong winter monsoon wind causes surface cooling over India and China in the Late Miocene

Secular and orbital-scale variability of equatorial Indian Ocean summer monsoon winds during the late Miocene

Secular and orbital-scale variability of equatorial Indian Ocean summer monsoon winds during the late Miocene

Re-organization of Pacific overturning circulation across the Miocene Climate Optimum

Late Miocene climate cooling and intensification of southeast Asian winter monsoon

Regional climate model experiments to investigate the Asian monsoon in the Late Miocene

Regional climate model experiments to investigate the Asian monsoon in the Late Miocene

South Asian summer monsoon enhanced by the uplift of Iranian Plateau in Middle Miocene

South Asian summer monsoon enhanced by the uplift of Iranian Plateau in Middle Miocene

Late Miocene Tarim desert wetting linked with eccentricity minimum and East Asian monsoon weakening

Dominance of climate warming effects on recent drying trends over wet monsoon regions

South Asian summer monsoon enhanced by the uplift of the Iranian Plateau in Middle Miocene

Strong winter monsoon wind causes surface cooling over India and China in the Late Miocene

Secular and orbital-scale variability of equatorial Indian Ocean summer monsoon winds during the late Miocene

Secular and orbital-scale variability of equatorial Indian Ocean summer monsoon winds during the late Miocene

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