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Updated: Oct 29, 2025

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
Published on: June 13, 2020
Interaction between decadal-to-multidecadal oceanic variability and sudden stratospheric warmings
Blanca Ayarzagüena1, Elisa Manzini2, Natalia Calvo1
1Departamento de Física de la Tierra y Astrofísica, Universidad Complutense de Madrid, Madrid, Spain.
Pacific decadal variability (PDV) increases sudden stratospheric warming (SSW) events by interacting with tropospheric waves. Atlantic multidecadal variability (AMV) influences the atmospheric response to SSWs, aiding prediction.
Area of Science:
- Atmospheric Science
- Climate Dynamics
- Stratospheric Physics
Background:
- Major sudden stratospheric warmings (SSWs) are key drivers of wintertime stratospheric variability.
- SSWs cause polar temperature increases and stratospheric easterlies, impacting surface circulation.
- SSW occurrence varies multidecadally, potentially linked to sea surface temperatures.
Purpose of the Study:
- Investigate the influence of Pacific decadal variability (PDV) and Atlantic multidecadal variability (AMV) on SSWs.
- Examine how PDV and AMV modulate SSW frequency, precursors, and impacts.
- Utilize a large ensemble of historical experiments for comprehensive analysis.
Main Methods:
- Analysis of a large ensemble of historical climate simulations.
- Examination of the relationship between PDV, AMV, and SSW characteristics.
- Investigation of interference between oceanic variability and tropospheric stationary waves.
Main Results:
- PDV significantly impacts SSW occurrence, increasing frequency during its positive phase.
- PDV's influence is mediated by constructive interference with tropospheric stationary waves.
- AMV primarily modulates the tropospheric response to SSWs.
Conclusions:
- PDV is a significant factor in controlling SSW frequency.
- AMV affects the predictability of the tropospheric impacts of SSWs.
- Findings aid in understanding and predicting stratospheric variability and its teleconnections.
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