Subseasonal Coastal Trapped Wave Propagations ... - AGU Publications

Mar 14, 2018 - NOAA/Atlantic Oceanographic and Meteorological Laboratory, Miami, Florida ... configurations of the southeastern Pacific and Atlantic Oceans.
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Journal of Geophysical Research: Oceans RESEARCH ARTICLE 10.1029/2017JC013539 This article is a companion to Illig et al. [2018], https://doi.org/10.1029/ 2017JC013540.

Subseasonal Coastal-Trapped Wave Propagations in the Southeastern Pacific and Atlantic Oceans: 1. A New Approach to Estimate Wave Amplitude Serena Illig1,2

, Emeline Cadier2, Marie-Lou Bache`lery2,3

2,4 , and Marion Kersale

1

Key Points:  We introduce and validate a simple methodology to estimate gravest CTW mode contributions to coastal variability from ocean model outputs  Inferred CTW characteristics (modal amplitude and propagating velocities) agree with the solution of a simple multimode linear CTW model  CTW dynamics controls a large part of the subseasonal variability along the coasts of southwestern American and African continents

Correspondence to: S. Illig, [email protected]

Citation: Illig, S., Cadier, E., Bache`lery, M.-L., & Kersal e, M. (2018). Subseasonal coastal-trapped wave propagations in the southeastern Pacific and Atlantic Oceans: 1. A new approach to estimate wave amplitude. Journal of Geophysical Research: Oceans, 123, 3915–3941. https://doi.org/10.1029/2017JC013539 Received 9 OCT 2017 Accepted 31 MAR 2018 Accepted article online 5 APR 2018 Published online 8 JUN 2018

Laboratoire d’Etudes en G eophysique et Oc eanographie Spatiale (LEGOS), CNRS/IRD/UPS/CNES, Toulouse, France, Department of Oceanography, MARE Institute, LMI ICEMASA, University of Cape Town, Cape Town, South Africa, 3 Nansen-Tutu Centre, Marine Research Institute, Department of Oceanography, University of Cape Town, Cape Town, South Africa, 4NOAA/Atlantic Oceanographic and Meteorological Laboratory, Cooperative Institute for Marine and Atmospheric Studies, University of Miami, Miami, FL, USA 2

Abstract The Humboldt and the Benguela upwelling systems are connected to the equatorial variability through the coastal waveguide, so that a large variance of the coastal sea level and current variability can be described as an infinite sum of orthonormal free Coastal-Trapped Wave (CTW) modes. The objective of this study is to infer the CTW mode contributions to the coastal variability in both systems at subseasonal timescales (