Future changes in the influence of the Southern Annular Mode on South Pacific chlorophyll- a in the Cesm2 large ensemble
Bibliographic Data
| ID | 15549700 |
|---|---|
| Authors | Jae-Seung Yoon (0000-0002-7148-0369, Korea Polar Research Institute, corresponding author), Taewook Park (0000-0002-7787-0042, Korea Polar Research Institute), Keyhong Park (0009-0004-2735-2214, Korea Polar Research Institute), Jisoo Park (0000-0002-3865-083X, Korea Polar Research Institute), Tae‐Wook Kim (0000-0002-4236-0720, Korea University) |
| Year | 2025 |
| Volume | 21 |
| Issue | 2 |
| Pages | 024020-024020 |
| Publication date | 2025-12-11 |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | Environmental Research Letters (JOURNAL) |
| Journal identifiers | ISSN: 1748-9326 • E-ISSN: 1748-9326 |
| Publisher | IOP Publishing (PUBLISHER • GB) |
| DOI | 10.1088/1748-9326/ae2b85 |
| OpenAlex | W7114895592 |
| Language | EN |
| References cited | 2 |
The Southern Annular Mode (SAM) is the leading mode of atmospheric variability in the Southern Hemisphere, exerting a significant influence on ocean circulation and marine productivity. In the present climate, positive SAM phases enhance Ekman-driven northward nutrient transport, leading to delayed increases in chlorophyll- a (Chl- a ) concentrations in the mid-latitude South Pacific. However, the extent to which this relationship will persist under future climate change remains uncertain. Here, we investigate future changes in the SAM–Chl- a relationship using Community Earth System Model version 2 Large Ensemble simulations under the shared socioeconomic pathway3−7.0 scenario. A subset of ensemble members that successfully reproduce observed present-day SAM–Chl- a lag correlations was selected for analysis. In the historical period (1970–2014), Chl- a anomalies in the mid-latitude eastern South Pacific show a distinct peak approximately three months after positive SAM events, associated with enhanced northward nutrient transport. In contrast, future projections (2070–2100) reveal a weakened or absent lagged response, coinciding with reduced westerly wind anomalies and diminished Ekman transport. These results suggest that the SAM’s influence to regulate marine productivity in the mid-latitude South Pacific may decline under continued climate change. This has important implications for future biogeochemical dynamics and highlights the need for high-resolution modeling to better represent fine-scale ocean–atmosphere interactions
Biogeochemical cycle · Climate change · Climate model · Climate system · Ekman transport · Lag · Mode (computer interface · Precipitation · Sea surface temperature · Climate variability and models · Marine and coastal ecosystems · Oceanographic and Atmospheric Processes
| Highly cited | No |
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