Surging of global surface temperature due to decadal legacy of ocean heat uptake
Sinha, Bablu; Sévellec, Florian; Robson, Jon; Nurser, George. 2020 Surging of global surface temperature due to decadal legacy of ocean heat uptake. Journal of Climate, 33 (18). 8025-8045. https://doi.org/10.1175/JCLI-D-19-0874.1
Before downloading, please read NORA policies.
|
Text
jclid190874.pdf - Accepted Version Available under License Creative Commons Attribution 4.0. Download (2MB) | Preview |
|
|
Text
jclid190874.pdf - Published Version Download (4MB) | Preview |
Abstract/Summary
Global surface warming since 1850 consisted of a series of slowdowns (hiatus) followed by surges. Knowledge of a mechanism to explain how this occurs would aid development and testing of interannual to decadal climate forecasts. In this paper a global climate model is forced to adopt an ocean state corresponding to a hiatus (with negative Interdecadal Pacific Oscillation, IPO, and other surface features typical of a hiatus) by artificially increasing the background diffusivity for a decade before restoring it to its normal value and allowing the model to evolve freely. This causes the model to develop a decadal surge which overshoots equilibrium (resulting in a positive IPO state) leaving behind a modified, warmer climate for decades. Water mass transformation diagnostics indicate that the heat budget of the tropical Pacific is a balance between large opposite signed terms: surface heating/cooling due to air-sea heat flux is balanced by vertical mixing and ocean heat transport divergence. During the artificial hiatus, excess heat becomes trapped just above the thermocline and there is a weak vertical thermal gradient (due to the high artificial background mixing). When the hiatus is terminated, by returning the background diffusivity to normal, the thermal gradient strengthens to pre-hiatus values so that the mixing (diffusivity x thermal gradient) remains roughly constant. However, since the base layer just above the thermocline remains anomalously warm this implies a warming of the entire water column above the trapped heat which results in a surge followed by a prolonged period of elevated surface temperatures.
Item Type: | Publication - Article |
---|---|
Digital Object Identifier (DOI): | https://doi.org/10.1175/JCLI-D-19-0874.1 |
ISSN: | 0894-8755 |
Date made live: | 11 Jun 2020 13:28 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/527944 |
Actions (login required)
View Item |
Document Downloads
Downloads for past 30 days
Downloads per month over past year