Quantifying Global Ocean Inhomogeneity and Exploring Its Evolution in Climate Change
The ocean is intrinsically inhomogeneous in temperature and salinity. This inhomogeneity fundamentally influences physical and biogeochemical processes of oceans, causing mixing of water masses, and shaping three-dimensional geostrophic circulations. The ocean inhomogeneity ultimately determines marine biodistribution, ecosystem structure and functioning, and marine biodiversity.
Recently, the research team led by Prof. WANG Fan from the Institute of Oceanology of the Chinese Academy of Sciences (IOCAS) and Prof. Young-Oh Kwon from Woods Hole Oceanographic Institution quantified the global ocean inhomogeneity and explored how it has evolved in a changing climate.
The study was published in Geophysical Research Letters on Jun 23 and reported as a research spotlight in American Geophysical Union (AGU) Earth & Space Science News (Eos).
The long-term changes in global ocean inhomogeneity by computing three-dimensional volume-weighted spatial standard deviation (SSD) of temperature and salinity (SSDT and SSDS) using multiple datasets and climate model simulations show a consensus on the increased global ocean inhomogeneity over the past half-century.
The global SSDT and SSDS in 0-2000 m increased by 1.4 ± 0.1%, and 1.5 ± 0.1% during 1960-2010 from 1960 to 1980 average, respectively. A newly defined thermohaline inhomogeneity (THI) index, a holistic measure of both temperature and salinity changes, has increased by 2.4 ± 0.1%. Climate model simulations suggest that the observed ocean inhomogeneity increase is dominated by anthropogenic forcing and projected to accelerate by 200%-300% during 2015-2100.
Furthermore, the regional contributions to global ocean inhomogeneity change suggest that global inhomogeneity increase largely results from the amplification of the corresponding climatological contrast patterns. "The rapid upper-ocean warming over mid-to-low latitude dominates the global SSDT increase, while the amplification of the salinity pattern, primarily in the subtropical Atlantic, causes increasing SSDS," said REN Qiuping, first author of the study.
"Our quantifications of ocean inhomogeneity provide a novel perspective for understanding the ongoing climate change in oceans. The increase in ocean inhomogeneity implies that ocean hydrological structures are modulated to a new and more diverse equilibrium, which poses important enlightenment for the future climate prediction, marine ecological environment and biodiversity," said Prof. WANG.
This work was supported by the Strategic Priority Research Program of the Chinese Academy of Sciences, the National Key R&D Program of China, the Shandong Provincial Natural Science Foundation, and the U.S. National Science Foundation Physical Oceanography Program.
Changes of global ocean SSDT, SSDS, and THI
Ren, Q., Kwon, Y., Yang, J., Huang, R. X., & Li, Y. (2022). Increasing Inhomogeneity of the Global Oceans. Geophysical Research Letters. 1-11.
(Text by REN Qiuping)
Media Contact:
ZHANG Yiyi
Institute of Oceanology
E-mail: zhangyiyi@qdio.ac.cn
(Editor: ZHANG Yiyi)
