The bottom currents in the area of abyssal hills in the north-east tropical Pacific Ocean

1993 ◽  
Vol 4 (1) ◽  
pp. 53-61 ◽  
Author(s):  
T. A. Demidova ◽  
E. A. Kontar' ◽  
A. V. Sokov ◽  
A. M. Belyaev
Keyword(s):  
Pacific Ocean ◽  
Tropical Pacific ◽  
Tropical Pacific Ocean ◽  
Bottom Currents ◽  
North East ◽  
The North ◽  
Abyssal Hills

scholarly journals Sensitivity study of the tropical Pacific precipitation anomalies

2016 ◽  
Author(s):  
Shouwen Zhang ◽  
Hua Jiang ◽  
Hui Wang ◽  
Ling Du ◽  
Dakui Wang
Keyword(s):  
Pacific Ocean ◽  
Sea Ice ◽  
North Atlantic ◽  
Climate Model ◽  
Tropical Pacific ◽  
Tropical Pacific Ocean ◽  
The North ◽  
Precipitation Anomalies ◽  
The North Atlantic ◽  
The Tropical Pacific

Abstract. Climate model results have shown that precipitation in the tropical Pacific Ocean will change up to 15 % and 25 % in one century. In this paper, both reanalysis data and climate model are used to study the response of global ocean and atmosphere to precipitation anomalies in the tropical Pacific Ocean. It shows that positive precipitation anomalies could trigger an El Nino-like SSTA response, with warmer SST in the east tropical Pacific Ocean and slightly cooler SST in the west tropical Pacific Ocean. The zonal tropical ocean currents change significantly, of which the magnitudes and directions are mainly relying on the intensity of the precipitation anomalies. Through a wave train encompassing the whole Northern Hemisphere named as the Circumglobal Waveguide Pattern (CWP), the North Atlantic atmospheric circulation responds to the freshwater anomalies in a NAO-like pattern. The anomalous atmospheric circulation transport sea ice to the North Atlantic Ocean. The sea ice melts in summer and freshen the upper ocean, which makes the ocean more stable. It thus constrains vertical heat transport and makes the upper water cooler, forming a significant positive feedback mechanism.

scholarly journals Evidence of eddy-related deep ocean current variability in the North-East Tropical Pacific Ocean induced by remote gap winds

2020 ◽  
Author(s):  
Kaveh Purkiani ◽  
André Paul ◽  
Annemiek Vink ◽  
Maren Walter ◽  
Michael Schulz ◽  
...  
Keyword(s):  
Pacific Ocean ◽  
Deep Sea ◽  
Mesoscale Eddies ◽  
Deep Ocean ◽  
Ocean Current ◽  
Tropical Pacific Ocean ◽  
North East ◽  
The North ◽  
Gap Winds ◽  
Anticyclonic Eddies

Abstract. There has been a steady increase of interest in mining of deep-sea minerals in the Clarion-Clipperton Zone (CCZ) in the eastern Pacific Ocean during the last decade. This region is known to be one of the most eddy-rich regions in the world. Typically, mesoscale eddies are generated by intense wind bursts channelled through gaps in the Sierra Madre mountains in Central America. Here, we use a combination of satellite and in situ observations to evaluate the relationship between deep-sea current variability at the region of potential future mining and Eddy Kinetic Energy (EKE) in the vicinity of gap winds. A geometry-based eddy detection algorithm has been applied to altimetry sea surface height data for a period of 24 years from 1993 to 2016 in order to analyse the main characteristic parameters and the spatiotemporal variability of mesoscale eddies in the North-East Tropical Pacific Ocean (NETP). Significant differences between the characteristics of eddies with different polarity (cyclonic vs. anti-cyclonic) were found. For eddies with lifetimes longer than one day, cyclonic polarity is more numerous that anticyclonic rotation. However, anticyclonic eddies are larger in size, show stronger in vorticity, and survive longer in the ocean than cyclonic eddies (often 90 days or more). Besides the polarity of eddies, the location of eddy formation should be taken into consideration when investigating the impacted deep ocean region, as we found eddies originating from the Tehuantepec (TT) gap wind lasting longer in the ocean and travelling farther distances in a different direction compared to eddies produced by the Papagayo (PP) gap wind. Long-lived anticyclonic eddies generated by the TT gap wind are observed to travel distances up to 4500 km offshore, i.e. as far as west of 110 W. EKE anomalies observed in the surface of the central ocean at distances of ca. 2500 km from the coast correlate with the seasonal variability of EKE in the region of the TT gap winds with a time lag of 5–6 months. A significant seasonal variability of deep ocean current velocities at water depths of 4100 m was observed in multiple year time-series data likely reflecting the energy transfer of the surface EKE generated by the gap winds to the deep ocean. Furthermore, the influence of mesoscale eddies on deep ocean currents is examined by analyzing the deep ocean current measurements when an anticyclonic eddy crosses the study region. Our findings suggest that despite the significant modulation of dominant current directions driven by the bottom-reaching eddy, the current magnitude intensification was not strong enough to trigger local sediment resuspension in this region. A better insight of annual variability of ocean surface mesoscale activity in the CCZ and their effects on deep ocean current variability are of great help to mitigate the impact of the benthic ecosystem from future potential 1deep-sea mining activities. On an interannual scale, a significant relationship between cyclonic eddy characteristics and El-Niño Southern Oscillation (ENSO) was found, whereas no robust correlation was detected for anticyclonic eddies.

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