The Active Role of the Ocean in the Temporal Evolution of Climate Sensitivity
Abstract
Transient climate sensitivity has been shown to be influenced by the changing pattern of SST and Ocean Heat Uptake (OHU), which in turn have been attributed to ocean circulation changes. A set of novel experiments are performed to isolate the active role of the ocean by comparing a fully-coupled CO2-quadrupling CESM simulation against a partially-coupled one, where the effect of the ocean circulation change and its impact on surface fluxes are disabled. The active OHU is the main factor responsible for the reduced transient climate sensitivity and weaker surface warming response in the fully-coupled simulation. The passive OHU excites qualitatively similar feedbacks to CO2 forcing in a slab ocean model configuration due to the similar SST spatial pattern response in both experiments. Additionally, the non-unitary forcing efficacy of the active OHU (1.7) explains the very different net feedback parameters in the fully-and partially-coupled responses.
- Authors:
-
- Pacific Northwest National Lab. (PNNL), Richland, WA (United States)
- Univ. of China and National Lab. for Marine Science and Technology, Qinqdao (China)
- Publication Date:
- Research Org.:
- Pacific Northwest National Laboratory (PNNL), Richland, WA (United States)
- Sponsoring Org.:
- USDOE
- OSTI Identifier:
- 1420443
- Alternate Identifier(s):
- OSTI ID: 1421323; OSTI ID: 1464415
- Report Number(s):
- PNNL-SA-129309
Journal ID: ISSN 0094-8276; TRN: US1801497
- Grant/Contract Number:
- AC05-76RL01830; AC02-05CH11231
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Geophysical Research Letters
- Additional Journal Information:
- Journal Volume: 45; Journal Issue: 1; Journal ID: ISSN 0094-8276
- Publisher:
- American Geophysical Union
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 54 ENVIRONMENTAL SCIENCES; Climate sensitivity; Ocean heat uptake; Ocean circulation change; Radiative Feedbacks; Air-sea interactions; climate; ocean heat uptake; OHU; ocean; SST
Citation Formats
Garuba, Oluwayemi A., Lu, Jian, Liu, Fukai, and Singh, Hansi A. The Active Role of the Ocean in the Temporal Evolution of Climate Sensitivity. United States: N. p., 2017.
Web. doi:10.1002/2017GL075633.
Garuba, Oluwayemi A., Lu, Jian, Liu, Fukai, & Singh, Hansi A. The Active Role of the Ocean in the Temporal Evolution of Climate Sensitivity. United States. https://doi.org/10.1002/2017GL075633
Garuba, Oluwayemi A., Lu, Jian, Liu, Fukai, and Singh, Hansi A. Thu .
"The Active Role of the Ocean in the Temporal Evolution of Climate Sensitivity". United States. https://doi.org/10.1002/2017GL075633. https://www.osti.gov/servlets/purl/1420443.
@article{osti_1420443,
title = {The Active Role of the Ocean in the Temporal Evolution of Climate Sensitivity},
author = {Garuba, Oluwayemi A. and Lu, Jian and Liu, Fukai and Singh, Hansi A.},
abstractNote = {Transient climate sensitivity has been shown to be influenced by the changing pattern of SST and Ocean Heat Uptake (OHU), which in turn have been attributed to ocean circulation changes. A set of novel experiments are performed to isolate the active role of the ocean by comparing a fully-coupled CO2-quadrupling CESM simulation against a partially-coupled one, where the effect of the ocean circulation change and its impact on surface fluxes are disabled. The active OHU is the main factor responsible for the reduced transient climate sensitivity and weaker surface warming response in the fully-coupled simulation. The passive OHU excites qualitatively similar feedbacks to CO2 forcing in a slab ocean model configuration due to the similar SST spatial pattern response in both experiments. Additionally, the non-unitary forcing efficacy of the active OHU (1.7) explains the very different net feedback parameters in the fully-and partially-coupled responses.},
doi = {10.1002/2017GL075633},
journal = {Geophysical Research Letters},
number = 1,
volume = 45,
place = {United States},
year = {Thu Nov 30 00:00:00 EST 2017},
month = {Thu Nov 30 00:00:00 EST 2017}
}
Web of Science
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