A Climatological Study of the Mechanisms Controlling the Seasonal Meridional Migration of the Atlantic Warm Pool in an OGCM

Dahirou Wane,Malick Wade,Amadou Thierno Gaye,Alban Lazar

doi:10.3390/atmos12091224

Abstract

The tropical Atlantic Warm Pool is one of the main drivers of the marine intertropical convergence zone and the associated coastal Northeast Brazilian and West-African monsoons. Its meridional displacement is driven by the solar cycle, modulated by the atmosphere and ocean interactions, whose nature and respective proportions are still poorly understood. This paper presents a climatological study of the upper ocean and lower atmosphere contributions to the warm pool seasonal migration, using an Ocean General Circulation Model (OGCM). First, we provide quantitative, albeit simple, pieces of evidence on how the large amplitude of migration in the west, compared to the east, is mainly due to the strong east–west contrast of the background meridional SST gradient intensities, which is maintained by equatorial and eastern tropical upwellings. Our main results consist first in identifying a diagnostic equation for the migration speed of the two meridional boundary isotherms of the Warm Pool, expressed in terms of the various mixed-layer heat fluxes. We then evidence and quantify how, in general, the migration is forced by air–sea fluxes, and damped by ocean circulation. However, remarkable controls by the ocean are identified in some specific regions. In particular, in the northwestern part of the Warm Pool, characterized by a large temperature inversion area, the boreal spring northward movement speed depends on the restitution of the solar heating by the thermocline. Additionally, over the southern part of the Warm Pool, our study quantifies the key role of the equatorial upwelling, which, depending on the longitude, significantly accelerates or slows down the summer poleward migration.

Highlights

The Inter-Tropical Convergence Zone (ITCZ) is a band of deep atmospheric convection [1,2] which can be defined as a region of heavy precipitation on-time average [3], produced by the convergence of the Trade winds [4,5] and by intense solar heating [6].In tropical oceans, the warmest waters are generally found under regions with the most active convection [7,8]
To identify the isotherm associated with the Atlantic Warm Pool (AWP) meridional boundaries and with the ITCZ rain band, we quantified the relationship between Sea SurfaceTemperatures (SSTs) and rainfall
One of the characteristics of the tropical basin is the presence of the Atlantic Cold Tongue (ACT), whose signal in SST is maximum in the E30 sector

Summary

Introduction

The Inter-Tropical Convergence Zone (ITCZ) is a band of deep atmospheric convection [1,2] which can be defined as a region of heavy precipitation on-time average [3], produced by the convergence of the Trade winds [4,5] and by intense solar heating [6].In tropical oceans, the warmest waters are generally found under regions with the most active convection [7,8]. The Inter-Tropical Convergence Zone (ITCZ) is a band of deep atmospheric convection [1,2] which can be defined as a region of heavy precipitation on-time average [3], produced by the convergence of the Trade winds [4,5] and by intense solar heating [6]. Temperatures (SSTs), with deep atmospheric convection favored by warm SSTs [9,10,11,12]. This has been confirmed numerically by [13], who showed that ITCZ migration is blocked in boreal spring when the cold tongue is prevented from developing. A common definition of the Warm Pool (WP) relies on the simple concept of an SST threshold value associated with deep convection. Some authors choose ◦ C [12,14,15], others or 28.5 ◦ C [16,17,18,19], and we will retain the first value for the boundaries of the tropical Atlantic Warm Pool (AWP)

Methods

Results

Conclusion