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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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North Africa
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Atlas Mountains
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Moroccan Atlas Mountains
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Anti-Atlas (1)
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Primary terms
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Tertiary
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Invertebrata
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Mesozoic
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Kuroshio Extension
Sedimentary effects of interplay between the Kuroshio Extension and Pacific plate motion
Map of the North Pacific Ocean and bimonthly δ 18 O, Sr/Ca, and U/Ca record...
The 1500-year climate oscillation in the midlatitude North Pacific during the Holocene
Subtropical coral reveals abrupt early-twentieth-century freshening in the western North Pacific Ocean
(a) Locations of the Japan Sea in the global ocean and the typical sites re...
MEMORIAL TO HIROSHI UJIIÉ
SEDIMENT TRAP RESULTS FROM THE JAPAN TRENCH IN THE KUROSHIO DOMAIN: SEASONAL VARIATIONS IN THE PLANKTIC FORAMINIFERAL FLUX
Calcareous dinoflagellates from a northwestern Pacific sediment trap and their paleoceanographic implications
Linking ocean and continental records of paleoclimate: determining accord and discord in the records
New REE-Constrained Terrigenous Depositional Changes in the Central Okinawa Trough and their Responses to Climate since 92 Millennia
Glacio-eustatic control on deep-marine clastic forearc sedimentation, Pliocene-mid-Pleistocene (c. 1180–600 ka) Kazusa Group, SE Japan
Summer and winter distribution and malformation of coccolithophores in the East China Sea
Clay-mineral assemblages across the Nankai-Shikoku subduction system, offshore Japan: A synthesis of results from the NanTroSEIZE project
Effects of the coupling between slope morphology and bottom currents on flow erosion and sedimentation at the Dongsha Continental Margin, South China Sea
2022 Cushman Foundation Awards and Grant Recipients
Intermediate-water dynamics and ocean ventilation effects on the Indonesian Throughflow during the past 15,000 years: Ostracod evidence
Formation of authigenic carbonates contributed by sulfate- and metal-driven anaerobic oxidation of methane in the northern Okinawa Trough, East China Sea
Late Miocene–mid-Pliocene tectonically induced formation of the semi-closed Japan Sea, inferred from seawater Nd isotopes
Abstract The changes in the sea-ice conditions and sea surface temperatures in the Subarctic Pacific caused by the closure of the Central American Seaway and their influence on the East Asian monsoon are investigated by a series of closed (CE), open (OE) and re-closed (RCE) seaway experiments with a climate model. It is found that a permanent halocline forms in the Subarctic Pacific because of the termination of saline water transport through the seaway in CE and RCE. Efficient cooling by shallow convection in the stratified permanent halocline causes thicker and more extensive sea ice in winter, and leads to colder surface water in summer in the Subarctic Pacific. Colder air, over more extensive sea ice cover in winter and over the colder water in summer, produces higher surface air pressure with anticyclonic wind anomalies in both seasons. Southeasterly and southerly wind anomalies develop around the Japanese archipelago in the East Asian monsoon region and induce warm and humid surface air with increased precipitation over the East Asian continent. These results indicate that the East Asian monsoon is weakened in winter and strengthened in summer as a result of closing the Central American Seaway.