Multidecadal Intensification of Atlantic Tropical Instability Waves

• Published in: Geophysical Research Letters
• Main Authors: Tuchen, Franz Philip, Perez, Renellys C., Foltz, Gregory R., Brandt, Peter, Lumpkin, Rick
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2022
• Subjects: North Atlantic
• Online Access: https://oceanrep.geomar.de/id/eprint/57487/; https://oceanrep.geomar.de/id/eprint/57487/1/Tuchen_Brandt_2022.pdf; https://doi.org/10.1029/2022GL101073

Tropical Instability Waves (TIWs) are the dominant source of intraseasonal variability in the central equatorial Atlantic and play an important role in the redistribution of heat in the upper ocean. Here we use multidecadal records of sea surface temperature, sea level anomaly, sea surface salinity, and near-surface currents constructed from in situ and satellite observations to reveal a long-term intensification of the intraseasonal variability of these variables due to an increase of TIW activity. Enhanced barotropic energy conversion from increased covariance of horizontal current fluctuations, rather than low-frequency changes of the mean zonal currents, drives the TIW intensification. As a consequence, boreal summer cooling of tropical North Atlantic surface waters through horizontal eddy temperature advection increased by 0.03°C month−1 decade−1 during 1993–2021, a change of 74% ± 53% relative to the long-term mean. The presented multidecadal TIW trends are strongly modulated by interannual variations like the 2021 Atlantic Niño. Key Points: - In situ and satellite observations show a long-term intensification of Tropical Instability Waves (TIWs) in the tropical North Atlantic - Enhanced TIW activity is mainly due to increased barotropic instability associated with increased covariance of velocity fluctuations - As a result, TIW-driven sea surface cooling north of the equator due to eddy temperature advection has increased by 74% from 1993 to 2021