Year: 2025
Type: article
Abstract: Sea surface salinity (SSS), an essential climate variable that is sensitive to changes in the global water cycle, varies seasonally in many places due to annual variations in rainfall and evaporation, as well as vertical mixing and advection. The seasonal variability of global mean SSS, with maximum/minimum SSS in March/September has been increasing in amplitude since the start of the satellite observation era in 2010. This variability, with a range of 0.04, is equivalent to approximately 3.0 cm of water leaving from and returning to the surface of the ocean over the course of the year, with its 0.015 increase in range since 2011, roughly equating to an additional 1.0 cm of water cycling out and returning to the ocean. This trend is consistent with predictions of an accelerating global water cycle on a warming planet.
Source: Geophysical Research Letters
DOI: 10.1029/2024gl111608
Authors: F. M. Bingham, E. Bayler
Language: English
Subfield: Global and Planetary Change
Field: Environmental Science
Domain: Physical Sciences
Open Access status: gold
Estimated APC paid: $3,190
OpenAlex ID: W4409627192
