Authigenic phillipsite formation rates in the central Indian Ocean and the Equatorial Pacific Ocean

1973 ◽  
Vol 20 (6) ◽  
pp. 555-559 ◽  
Author(s):  
Kenneth Czyscinski
2011 ◽  
Vol 24 (14) ◽  
pp. 3593-3608 ◽  
Author(s):  
Dongliang Yuan ◽  
Jing Wang ◽  
Tengfei Xu ◽  
Peng Xu ◽  
Zhou Hui ◽  
...  

Abstract Controlled numerical experiments using ocean-only and ocean–atmosphere coupled general circulation models show that interannual sea level depression in the eastern Indian Ocean during the Indian Ocean dipole (IOD) events forces enhanced Indonesian Throughflow (ITF) to transport warm water from the upper-equatorial Pacific Ocean to the Indian Ocean. The enhanced transport produces elevation of the thermocline and cold subsurface temperature anomalies in the western equatorial Pacific Ocean, which propagate to the eastern equatorial Pacific to induce significant coupled evolution of the tropical Pacific oceanic and atmospheric circulation. Analyses suggest that the IOD-forced ITF transport anomalies are about the same amplitudes as those induced by the Pacific ENSO. Results of the coupled model experiments suggest that the anomalies induced by the IOD persist in the equatorial Pacific until the year following the IOD event, suggesting the importance of the oceanic channel in modulating the interannual climate variations of the tropical Pacific Ocean at the time lag beyond one year.


Nature ◽  
1994 ◽  
Vol 371 (6493) ◽  
pp. 123-129 ◽  
Author(s):  
J. H. Martin ◽  
K. H. Coale ◽  
K. S. Johnson ◽  
S. E. Fitzwater ◽  
R. M. Gordon ◽  
...  

2018 ◽  
Vol 52 (7-8) ◽  
pp. 4351-4369 ◽  
Author(s):  
Xia Zhao ◽  
Dongliang Yuan ◽  
Guang Yang ◽  
Jing Wang ◽  
Hailong Liu ◽  
...  

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