Contributions of Atmospheric Forcing and Chaotic Ocean Variability to Regional Sea Level Trends Over 1993–2015. Issue 24 (21st December 2018)

• Record Type: Journal Article
• Authors: Llovel, William; Penduff, Thierry; Meyssignac, Benoit; Molines, Jean‐Marc; Terray, Laurent; Bessières, Laurent; Barnier, Bernard
• Is Part Of: Geophysical research letters. Volume 45:Issue 24(2018)
• Page Start: 13, 405
• Page End: 13, 413
• Publication Date: 2018-12-21
• Subjects: sea level trend -- satellite altimetry -- atmospheric forcing -- chaotic ocean variability; Geophysics -- Periodicals; Planets -- Periodicals; Lunar geology -- Periodicals; 550
• DOI: 10.1029/2018GL080838
• Languages: English
• ISSNs: 0094-8276

Abstract

Abstract: A global ¼° ocean/sea‐ice 50‐member ensemble simulation is analyzed to disentangle the imprints of the atmospheric forcing and the chaotic ocean variability on regional sea level trends over the satellite altimetry period. We find that the chaotic ocean variability may mask atmospherically forced regional sea level trends over 38% of the global ocean area from 1993 to 2015, and over 47% of this area from 2005 to 2015. These regions are located in the western boundary currents, in the Southern Ocean and in the subtropical gyres. While these results do not question the anthropogenic origin of global mean sea level rise, they give new insights into the intrinsically oceanic versus atmospheric forcing of regional sea level trends and provide new constraints on the measurement time required to attribute regional sea level trends to the atmospheric forcing or to climate change. Plain Language Summary: As a direct consequence of anthropogenic influences, global mean sea level rises in response to ocean warming and land ice melting. Since the early 1990s, satellite altimetry has revealed large regional contrasts in sea level trends, controlled by temperature and salinity changes, oceanic processes and atmospheric forcing. Using an ensemble of forced eddying ocean simulations, we show that regional sea level trends over the altimetric period are only partly determined by the atmospheric evolution (both natural and anthropogenic): nonlinear ocean processes produce additional sea level trends that are inherently random, which can compete in certain regions with the externally forced trends. These results do not question the existence of global and regional sea level trends, but suggest that sea level trends may not be unambiguously attributed to external causes in certain regions. Key Points: Atmospheric drivers force regional sea level trends over most of the global ocean area since 1993 Chaotic ocean variability may mask these atmospherically forced regional trends over a substantial fraction of the global ocean area In the latter regions, altimeter‐derived regional sea level trends may not be representative of anthropogenic or atmospheric causes