Simulating the role of surface forcing on observed multidecadal upper-ocean salinity changes
Abstract
The ocean’s surface salinity field has changed over the observed record, driven by an intensification of the water cycle in response to global warming. However, the origin and causes of the coincident subsurface salinity changes are not fully understood. The relationship between imposed surface salinity and temperature changes and their corresponding subsurface changes is investigated using idealized ocean model experiments. The ocean’s surface has warmed by about 0.5°C (50 yr)–1 while the surface salinity pattern has amplified by about 8% per 50 years. The idealized experiments are constructed for a 50-yr period, allowing a qualitative comparison to the observed salinity and temperature changes previously reported. The comparison suggests that changes in both modeled surface salinity and temperature are required to replicate the three-dimensional pattern of observed salinity change. The results also show that the effects of surface changes in temperature and salinity act linearly on the changes in subsurface salinity. In addition, surface salinity pattern amplification appears to be the leading driver of subsurface salinity change on depth surfaces; however, surface warming is also required to replicate the observed patterns of change on density surfaces. This is the result of isopycnal migration modified by the ocean surface warming, which producesmore »
- Authors:
-
- CSIRO, Oceans and Atmosphere, Hobart (Australia). Centre for Australian Weather and Climate Research; Univ. of Tasmania, Hobart (Australia). Institute for Marine and Antarctic Studies
- CSIRO, Oceans and Atmosphere, Hobart (Australia). Centre for Australian Weather and Climate Research
- CSIRO, Oceans and Atmosphere, Hobart (Australia). Centre for Australian Weather and Climate Research; Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States). Program for Climate Model Diagnosis and Intercomparison
- CSIRO, Oceans and Atmosphere, Hobart (Australia). Centre for Australian Weather and Climate Research; Univ. of Tasmania, Hobart (Australia). Institute for Marine and Antarctic Studies; Antarctic Climate and Ecosystems Cooperative Research Centre, Hobart (Australia)
- CSIRO Oceans and Atmosphere Flagship, Victoria (Australia). Centre for Australian Weather and Climate Research
- Publication Date:
- Research Org.:
- Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States)
- Sponsoring Org.:
- USDOE
- OSTI Identifier:
- 1305857
- Report Number(s):
- LLNL-JRNL-677101
Journal ID: ISSN 0894-8755
- Grant/Contract Number:
- AC52-07NA27344
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Journal of Climate
- Additional Journal Information:
- Journal Volume: 29; Journal Issue: 15; Journal ID: ISSN 0894-8755
- Publisher:
- American Meteorological Society
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 54 ENVIRONMENTAL SCIENCES; oceanography; salinity; global change; ocean modeling; climate change; water cycle; physical meteorology and climatology; surface fluxes; models and modeling; variability; multidecadal variability; ocean variability
Citation Formats
Lago, Veronique, Wijffels, Susan E., Durack, Paul J., Church, John A., Bindoff, Nathaniel L., and Marsland, Simon J. Simulating the role of surface forcing on observed multidecadal upper-ocean salinity changes. United States: N. p., 2016.
Web. doi:10.1175/JCLI-D-15-0519.1.
Lago, Veronique, Wijffels, Susan E., Durack, Paul J., Church, John A., Bindoff, Nathaniel L., & Marsland, Simon J. Simulating the role of surface forcing on observed multidecadal upper-ocean salinity changes. United States. https://doi.org/10.1175/JCLI-D-15-0519.1
Lago, Veronique, Wijffels, Susan E., Durack, Paul J., Church, John A., Bindoff, Nathaniel L., and Marsland, Simon J. Mon .
"Simulating the role of surface forcing on observed multidecadal upper-ocean salinity changes". United States. https://doi.org/10.1175/JCLI-D-15-0519.1. https://www.osti.gov/servlets/purl/1305857.
@article{osti_1305857,
title = {Simulating the role of surface forcing on observed multidecadal upper-ocean salinity changes},
author = {Lago, Veronique and Wijffels, Susan E. and Durack, Paul J. and Church, John A. and Bindoff, Nathaniel L. and Marsland, Simon J.},
abstractNote = {The ocean’s surface salinity field has changed over the observed record, driven by an intensification of the water cycle in response to global warming. However, the origin and causes of the coincident subsurface salinity changes are not fully understood. The relationship between imposed surface salinity and temperature changes and their corresponding subsurface changes is investigated using idealized ocean model experiments. The ocean’s surface has warmed by about 0.5°C (50 yr)–1 while the surface salinity pattern has amplified by about 8% per 50 years. The idealized experiments are constructed for a 50-yr period, allowing a qualitative comparison to the observed salinity and temperature changes previously reported. The comparison suggests that changes in both modeled surface salinity and temperature are required to replicate the three-dimensional pattern of observed salinity change. The results also show that the effects of surface changes in temperature and salinity act linearly on the changes in subsurface salinity. In addition, surface salinity pattern amplification appears to be the leading driver of subsurface salinity change on depth surfaces; however, surface warming is also required to replicate the observed patterns of change on density surfaces. This is the result of isopycnal migration modified by the ocean surface warming, which produces significant salinity changes on density surfaces.},
doi = {10.1175/JCLI-D-15-0519.1},
journal = {Journal of Climate},
number = 15,
volume = 29,
place = {United States},
year = {Mon Jul 18 00:00:00 EDT 2016},
month = {Mon Jul 18 00:00:00 EDT 2016}
}
Web of Science
Figures / Tables:
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