Improved estimates of water cycle change from ocean salinity: the key role of ocean warming. (19th July 2018)

• Record Type: Journal Article
• Authors: Zika, Jan D; Skliris, Nikolaos; Blaker, Adam T; Marsh, Robert; Nurser, A J George; Josey, Simon A
• Is Part Of: Environmental research letters. Volume 13:Number 7(2018:Jul.)
• Publication Date: 2018-07-19
• Subjects: water cycle -- ocean warming -- ocean salinity -- climate change; Environmental sciences -- Periodicals; Human ecology -- Research -- Periodicals; Environmental health -- Periodicals; 333.7
• DOI: 10.1088/1748-9326/aace42
• Languages: English
• ISSNs: 1748-9326

Abstract

Abstract: Changes in the global water cycle critically impact environmental, agricultural, and energy systems relied upon by humanity (Jiménez Cisneros et al 21 Climate Change 2014: Impacts, Adaptation, and Vulnerability (Cambridge: Cambridge University Press)). Understanding recent water cycle change is essential in constraining future projections. Warming-induced water cycle change is expected to amplify the pattern of sea surface salinity (Durack et al 11 Science 336 455–8). A puzzle has, however, emerged. The surface salinity pattern has amplified by 5%–8% since the 1950s (Durack et al 11 Science 336 455–8, Skliris et al 37 Clim. Dyn. 43 709–36) while the water cycle is thought to have amplified at close to half that rate (Durack et al 11 Science 336 455–8, Skliris et al 38 Sci. Rep. 6 752). This discrepancy is also replicated in climate projections of the 21st century (Durack et al 11 Science 336 455–8). Using targeted numerical ocean model experiments we find that, while surface water fluxes due to water cycle change and ice mass loss amplify the surface salinity pattern, ocean warming exerts a substantial influence. Warming increases near-surface stratification, inhibiting the decay of existing salinity contrasts and further amplifying surface salinity patterns. Observed ocean warming can explain approximately half of observed surface salinity pattern changes from 1957–2016 with ice mass loss playing a minor role. Water cycle change of 3.6% ± 2.1% per degree Celsius of surface air temperature change is sufficient to explain the remaining observed salinity pattern change.