Mechanisms of ocean heat uptake along and across isopycnals
Clement, Louis ORCID: https://orcid.org/0000-0002-6935-9455; McDonagh, E. L.; Gregory, J. M.; Wu, Q.; Marzocchi, A. ORCID: https://orcid.org/0000-0002-3430-3574; Zika, J. D.; Nurser, A. J. G.. 2022 Mechanisms of ocean heat uptake along and across isopycnals. Journal of Climate. 1-43. 10.1175/JCLI-D-21-0793.1
Before downloading, please read NORA policies.Preview |
Text
LClement_2ndSubmission.pdf - Accepted Version Download (10MB) | Preview |
Preview |
Text
[15200442 - Journal of Climate] Mechanisms of Ocean Heat Uptake along and across Isopycnals (1).pdf - Published Version Available under License Creative Commons Attribution 4.0. Download (5MB) | Preview |
Abstract/Summary
Warming of the climate system accumulates mostly in the ocean and discrepancies in how this is modelled contribute to uncertainties in predicting sea level rise. In this study, regional temperature changes in an atmosphere–ocean general circulation model (HadCM3) are partitioned between excess (due to perturbed surface heat fluxes) and redistributed (arising from changing circulation and perturbations to mixing) components. In simulations with historical forcing, we firstly compare this excess–redistribution partitioning with the spice and heave decomposition, in which temperature anomalies enter the ocean interior either along isopycnals (spice) or across isopycnals (heave, without affecting the temperature-salinity curve). Secondly, heat and salinity budgets projected into thermohaline space naturally reveal the mechanisms behind temperature change by spice and heave linked with water mass generation or destruction. Excess warming enters the ocean as warming by heave in subtropical gyres whereas it mainly projects onto warming by spice in the Southern Ocean and the tropical Atlantic. In subtropical gyres, Ekman pumping generates excess warming as confirmed by Eulerian heat budgets. In contrast, isopycnal mixing partly drives warming and salinification by spice, as confirmed by budgets in thermohaline space, underlying the key role of salinity changes for the ocean warming signature. Our study suggests a method to detect excess warming using spice and heave calculated from observed repeat profiles of temperature and salinity.
Item Type: | Publication - Article |
---|---|
Digital Object Identifier (DOI): | 10.1175/JCLI-D-21-0793.1 |
ISSN: | 0894-8755 |
Date made live: | 22 Apr 2022 11:51 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/532528 |
Actions (login required)
View Item |
Document Downloads
Downloads for past 30 days
Downloads per month over past year