Near‐coastal circulation in the Northern Humboldt Current System from shipboard ADCP data. Issue 10 (15th October 2013)

• Record Type: Journal Article
• Authors: Chaigneau, Alexis; Dominguez, Noel; Eldin, Gérard; Vasquez, Luis; Flores, Roberto; Grados, Carmen; Echevin, Vincent
• Is Part Of: Journal of geophysical research. Volume 118:Issue 10(2013:Oct.)
• Page Start: 5251
• Page End: 5266
• Publication Date: 2013-10-15
• Subjects: Oceanography -- Periodicals; 551.4605
• DOI: 10.1002/jgrc.20328
• Languages: English
• ISSNs: 2169-9275

Abstract

<abstract abstract-type="main"> <title> <x xml:space="preserve">Abstract</x> </title> <p>[1] The near‐coastal circulation of the Northern Humboldt Current System is described analyzing ∼8700 velocity profiles acquired by a shipboard acoustic Doppler current profiler (SADCP) during 21 surveys realized between 2008 and 2012 along the Peruvian coast. This data set permits observation of (i) part of the Peru Coastal Current and the Peru Oceanic Current that flow equatorward in near‐surface layers close to the coast and farther than ∼150 km from the coast, respectively; (ii) the Peru‐Chile Undercurrent (PCUC) flowing poleward in subsurface layers along the outer continental shelf and inner slope; (iii) the near‐surfacing Equatorial Undercurrent renamed as Ecuador‐Peru Coastal Current that feeds the PCUC; and (iv) a deep equatorward current, referred to as the Chile‐Peru Deep Coastal Current, flowing below the PCUC. A focus in the PCUC core layer shows that this current exhibits typical velocities of 5–10 cm s<sup>−1</sup>. The PCUC deepens with an increasing thickness poleward, consistent with the alongshore conservation of potential vorticity. The PCUC mass transport increases from ∼1.8 Sv at 5°S to a maximum value of ∼5.2 Sv at 15°S, partly explained by the Sverdrup balance. The PCUC experiences relatively weak seasonal variability and the confluence of eddy‐like structures and coastal currents strongly complicates the circulation. The PCUC intensity is also affected by the southward propagation of coastally trapped waves, as revealed by a strong PCUC intensification in March 2010 coincident with the passage of a downwelling coastal wave associated with a weak El Niño event.</p> </abstract>