Skip to Main Content U.S. Department of Energy
Science Directorate
Page 27 of 720

Atmospheric Sciences & Global Change
Research Highlights

May 2018

Sea Change: The Ocean's Powerful Effect on Earth Systems

A new modeling approach shows that the ocean circulation determines the varying rate of global temperature response to carbon dioxide.

ocean at dusk
Researchers isolated the role of ocean dynamics in shaping the pace of atmospheric warming.

The Science

What would happen if you gathered all the carbon dioxide released over centuries in a time capsule and released it at once into the climate system? Researchers at the U.S. Department of Energy's Pacific Northwest National Laboratory led a study that probed the pace of atmospheric warming.

Using a new modeling approach, they identified ocean dynamical feedback as the main reason for the time dependence of climate sensitivity. In their model, they disabled the effects of changing ocean circulation. In this way, they could isolate the role of ocean dynamics in shaping the pattern of heat absorption and the pace of warming.

The Impact

The partially coupled Earth system model is one-of-a-kind because the active role of the ocean dynamics can be separated from the total climate variations. Through this novel experimental design, scientists identified slow adjustments in ocean motion as the key for setting the transient behavior of climate sensitivity and organizing the related feedbacks.

Summary

The rate of global temperature response to increased atmospheric carbon dioxide is not constant. This fluctuation is due to interactions between the ocean and atmospheric changes caused by increased carbon dioxide. These interactions are difficult to separate in fully coupled Earth system model simulations.

Researchers developed a novel partial coupling approach to isolate the ocean's role in the global climate response to increased carbon dioxide by preventing the response of ocean circulation from coupling with the atmosphere. This approach revealed that the change in the ocean circulation is responsible for the slow evolution in the global ocean absorption of heat. This ocean feedback also produces a net global surface cooling resulting from the changing ocean circulation driving more heat into the deep ocean.

Acknowledgments

Sponsors: The U.S. Department of Energy (DOE) Office of Science, Biological and Environmental Research supported this research as part of the Regional and Global Climate Modeling program. H.A.S. is grateful for funding support from the Linus Pauling Distinguished Postdoctoral Fellowship at Pacific Northwest National Laboratory. F.L. is supported by the China Scholarship Council.

User Facility: The National Energy Research Scientific Computing Center (NERSC), a DOE Office of Science user facility, provided supercomputing resources.

Research Area: Climate and Earth Systems Science

Research Team: Oluwayemi A. Garuba, Jian Lu, and Hansi Singh, PNNL; and Fukai Liu, Ocean University of China and National Laboratory for Marine Science and Technology

Reference: O.A. Garuba, J. Lu, F. Liu, H.A. Singh, "The Active Role of the Ocean in the Temporal Evolution of Climate Sensitivity." Geophysical Research Letters 45, 306-315 (2018). [DOI: 10.1002/2017GL075633]


Page 27 of 720

Science at PNNL

Core Research Areas

User Facilities

Centers & Institutes

Additional Information

Research Highlights Home

Share

Print this page (?)

YouTube Facebook Flickr TwitThis LinkedIn

Contacts