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March 10, 2026Meteorological Applications2 citationsOpen Access

Solar and Wind Energy Variability in Tropical South America: Seasonal Ocean‐Atmospheric Modulators

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NDNicolás Duque‐GardeazabalSBStefan BrönnimannAFAndrew R. Friedman

Key Points

  • To investigate how ocean-atmospheric modes like ENSO and AMM affect the availability of solar and wind energy in tropical South America.
  • Applied partial correlations and composite analyses on reanalysis and satellite data
  • Identified seasonal anomalies linked to ocean-atmospheric modes
  • Focus on energy hubs: north Caribbean, eastern Brazil, western Perú/Bolivia
  • ENSO significantly influences wind capacity factors (CF) and solar CF in the north Caribbean and eastern Brazil
  • AMM modulates cross-equatorial wind anomalies affecting solar and wind CF
  • Limited complementarity between solar and wind energy availability at interannual scales

Abstract

ABSTRACT Interannual climate variability strongly influences renewable energy availability, making it a critical factor for achieving UN Sustainable Development Goals (SDGs). However, our knowledge about the potential solar and wind energy production in tropical South America and its relation to ocean‐atmospheric modes of variability is limited; modes such as El Niño/Southern Oscillation (ENSO), the Atlantic Meridional Mode (AMM), among others. Therefore, we investigate the influence of these modes on solar and wind energy. We apply partial correlations and composite analyses to reanalysis and satellite data to identify the processes connecting large‐scale ocean‐atmospheric variability to seasonal anomalies in renewable power generation. Our study identifies three energy hubs as regions with high climatological mean energy availability: The north Caribbean (NC), eastern Brazil (EB) and western Perú/Bolivia (WPB). ENSO influences the sea level pressure (SLP) gradients, generating wind anomalies that directly affect the wind capacity factor (CF). ENSO also affects the solar CF through reduced atmospheric moisture transport and convergence, which results in fewer clouds leading to higher‐than‐average surface radiation or by atmospheric subsidence. ENSO impacts the NC and EB hubs, with weaker effects in the WPB hub. The AMM is associated with cross‐equatorial wind anomalies that modulate wind CF, as well as moisture convergence and cloud cover, thereby influencing solar CF. Wind CF in the NC and EB hubs is inversely modulated by the AMM, weakening winds and reducing radiation over the NC and strengthening winds and increasing radiation on the EB. The Atlantic equatorial El Niño mode (Atl3) exerts minor effects, with anomalies confined to the equatorial Atlantic. Overall, we find limited complementarity between solar and wind energy at interannual time‐scale. Our results provide insights for forecasting energy production and managing energy storage for periods of low renewable energy availability.

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Cite This Study

Duque‐Gardeazabal et al. (2026) studied this question.

synapsesocial.com/papers/69af953870916d39fea4c9a9https://doi.org/10.1002/met.70165
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Also Consider

Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context:

  1. 1Solar and Wind Energy Variability in Tropical South America: Seasonal Ocean-Atmospheric Modulators2026
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  5. 5Revisiting climate extremes in South America and their modulation by oceanic teleconnections2026