Spatial variation of future trends in Atlantic upwelling cells from two CMIP6 models

Eastern Boundary Upwelling Systems (EBUS) are characterized by wind-triggered upwelling of deep waters along the coast. They are hotspots of biological productivity and diversity and therefore have a high economic, ecological and social importance. In the past, different methods using surface data have been used to estimate upwelling. Recently, the IPCC has suggested directly assessing vertical velocities as a promising method. We use this method to study the two Atlantic EBUS from CMIP6 models from the HadGEM3-GC3.1 and the CNRM6-CM6 family, for both the historical period and a high-emission future scenario with spatial resolutions in the ocean component ranging from 1°to 1/12°. The two major upwelling regions are divided in subregions depending on their seasonality. The vertical transport index shows similar values to a wind-derived Ekman index. Directly evaluating upwelling from transport processes further provides information about the depth of the upwelling, which has previously been identified as an important factor for nutrient availability. We show that depending on the subregion of the upwelling system, different cell structures can be seen in terms of depth and distance to the coast of maximum velocities. When looking at possible future changes, high interannual variability limits the significance of the trends but could indicate a poleward shift of the upwelling regions. A detailed comparison of the spatial structures and the distinction in subregions is important to explain contradictory trends in previous works. • The Atlantic upwelling cells are diagnosed from the vertical velocity in the CNRM-CM6-1 and HadGEM3-GC3.1 coupled models. • Cell structures differ in terms of depth and distance to the coast depending on the subregion of each upwelling system. • Subregions also show different future trends, but few are significant. • The trends tend to support the hypothesis of a future poleward migration of upwelling systems.

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Journal
Deep Sea Research Part II Topical Studies in Oceanography
Published
2025-05-08
DOI
https://doi.org/10.1016/j.dsr2.2025.105483
Primary Topic
Oceanographic and Atmospheric Processes
Type
article
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article

Spatial variation of future trends in Atlantic upwelling cells from two CMIP6 models

Malcolm Roberts, Steven Herbette, Anne‐Marie Tréguier, Robin Waldman et al.
Deep Sea Research Part II Topical Studies in Oceanography
Oceanographic and Atmospheric Processes
article

Spatial variation of future trends in Atlantic upwelling cells from two CMIP6 models

Malcolm Roberts, Steven Herbette, Anne‐Marie Tréguier, Robin Waldman, Raquel Flügel
article en

Abstract

Eastern Boundary Upwelling Systems (EBUS) are characterized by wind-triggered upwelling of deep waters along the coast. They are hotspots of biological productivity and diversity and therefore have a high economic, ecological and social importance. In the past, different methods using surface data have been used to estimate upwelling. Recently, the IPCC has suggested directly assessing vertical velocities as a promising method. We use this method to study the two Atlantic EBUS from CMIP6 models from the HadGEM3-GC3.1 and the CNRM6-CM6 family, for both the historical period and a high-emission future scenario with spatial resolutions in the ocean component ranging from 1°to 1/12°. The two major upwelling regions are divided in subregions depending on their seasonality. The vertical transport index shows similar values to a wind-derived Ekman index. Directly evaluating upwelling from transport processes further provides information about the depth of the upwelling, which has previously been identified as an important factor for nutrient availability. We show that depending on the subregion of the upwelling system, different cell structures can be seen in terms of depth and distance to the coast of maximum velocities. When looking at possible future changes, high interannual variability limits the significance of the trends but could indicate a poleward shift of the upwelling regions. A detailed comparison of the spatial structures and the distinction in subregions is important to explain contradictory trends in previous works. • The Atlantic upwelling cells are diagnosed from the vertical velocity in the CNRM-CM6-1 and HadGEM3-GC3.1 coupled models. • Cell structures differ in terms of depth and distance to the coast depending on the subregion of each upwelling system. • Subregions also show different future trends, but few are significant. • The trends tend to support the hypothesis of a future poleward migration of upwelling systems.

Deep Sea Research Part II Topical Studies in OceanographyVol. 221
Met Office (GB), Université de Bretagne Occidentale (FR), Phillips Exeter Academy (US), Centre National de Recherches Météorologiques (FR), Centre Européen de Recherche et de Formation Avancée en Calcul Scientifique (FR), Laboratoire d’Études en Géophysique et Océanographie Spatiales (FR), Laboratory for Ocean Physics and Satellite Remote Sensing (FR), Institut Universitaire Européen de la Mer (FR)
Life below water
Openalex Percentile: Top 88%
Oceanographic and Atmospheric Processes
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