Next Article in Journal / Special Issue
Correlation between Synthetic Aperture Radar Surface Winds and Deep Water Velocity in the Amundsen Sea, Antarctica
Previous Article in Journal
NASA Goddard’s LiDAR, Hyperspectral and Thermal (G-LiHT) Airborne Imager
Previous Article in Special Issue
Surface Imprints of Water-Column Turbulence: A Case Study of Tidal Flow over an Estuarine Sill
Remote Sens. 2013, 5(8), 4067-4087; doi:10.3390/rs5084067
Article

Unravelling Eastern Pacific and Central Pacific ENSO Contributions in South Pacific Chlorophyll-a Variability through Remote Sensing

1,2,†
,
2
 and
3,*
Received: 18 June 2013 / Revised: 22 July 2013 / Accepted: 5 August 2013 / Published: 13 August 2013
(This article belongs to the Special Issue Observing the Ocean’s Interior from Satellite Remote Sensing)
View Full-Text   |   Download PDF [1836 KB, uploaded 19 June 2014]   |   Browse Figures

Abstract

El Niño—Southern Oscillation (ENSO) is regarded as the main driver of phytoplankton inter-annual variability. Remotely sensed surface chlorophyll-a (Chl-a), has made it possible to examine phytoplankton variability at a resolution and scale that allows for the investigation of climate signals such as ENSO. We provide empirical evidence of an immediate and lagged influence of ENSO on SeaWiFS and MODIS-Aqua derived global Chl-a concentrations. We use 13 years of Chl-a remotely sensed observations along with sea surface temperature (SST) observations across the Tropical and South Pacific to isolate and examine the spatial development of Chl-a anomalies during ENSO: its canonical or eastern Pacific (EP) mode, and El Niño Modoki or central Pacific (CP) mode, using the extended empirical orthogonal function (EEOF) technique. We describe how an EP ENSO phase transition affects Chl-a, and identify an interannual CP mode of variability induced spatial pattern. We argue that when ENSO is analysed as a propagating signal by the EEOF, CP ENSO is found to be more influential on Chl-a interannual to decadal variability than the canonical EP ENSO. Our results cannot confirm the independence of the two ENSO modes but clearly demonstrate that both ENSO flavors manifest a distinct biological response.
Keywords: Chl-a; phytoplankton; ENSO; CP ENSO; EP ENSO; Modoki; El Niño; La Niña; primary productivity; SeaWiFS; MODIS Chl-a; phytoplankton; ENSO; CP ENSO; EP ENSO; Modoki; El Niño; La Niña; primary productivity; SeaWiFS; MODIS
This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

Share & Cite This Article

Further Mendeley | CiteULike
Export to BibTeX |
EndNote
MDPI and ACS Style

Couto, A.B.; Holbrook, N.J.; Maharaj, A.M. Unravelling Eastern Pacific and Central Pacific ENSO Contributions in South Pacific Chlorophyll-a Variability through Remote Sensing. Remote Sens. 2013, 5, 4067-4087.

View more citation formats

Related Articles

Article Metrics

For more information on the journal, click here

Comments

Cited By

[Return to top]
Remote Sens. EISSN 2072-4292 Published by MDPI AG, Basel, Switzerland RSS E-Mail Table of Contents Alert