Tools
Tools
Karlowska, Eliza 
ORCID: https://orcid.org/0000-0003-2401-0871, Matthews, Adrian J. ORCID: https://orcid.org/0000-0003-0492-1168, Webber, Benjamin ORCID: https://orcid.org/0000-0002-8812-5929, Graham, Tim and Xavier, Prince
(2024)
The effect of diurnal warming of sea surface temperatures on the propagation speed of the Madden-Julian Oscillation.
Quarterly Journal of the Royal Meteorological Society, 150 (758).
pp. 334-354.
ISSN 0035-9009
Preview |
PDF (karlowskaetal2023_accepted)
- Accepted Version
Available under License Creative Commons Attribution. Download (3MB) | Preview |
Abstract
The diurnal warm layer in the upper ocean develops during low surface winds and high incoming solar radiation conditions, often increasing sea-surface temperatures (SSTs) by up to 1°C. The suppressed phase of the Madden–Julian Oscillation (MJO) favours the formation of such a layer. Here, we analyse the coupled ocean–atmosphere and atmosphere-only numerical weather prediction systems of the UK Met Office to reveal that important differences arise from the representation of the diurnal warm layer in the coupled model. Though both models are skilful in predicting the MJO to at least a 7-day lead time, the coupled model predicts approximately 12% faster MJO RMM phase speed propagation than the atmosphere-only model due to the ability to resolve diurnal warming in the upper ocean that rectifies onto MJO-associated SST anomalies. The diurnal warming of SST (dSST) in the coupled model leads to an increase in daily mean SST compared with the atmosphere-only model persisted foundation SST. The strength of the dSST in the coupled model is modulated by MJO conditions. During suppressed MJO conditions on lead day 1, the dSST is enhanced, leading to 0.2°C warmer daily mean MJO-associated SST anomalies and increased convection in the coupled model by lead day 7. During active MJO convection, the dSST is suppressed, leading to 0.1°C colder MJO-associated SST anomalies in the coupled model and reduced convection by lead day 7. This variability in dSST further amplifies the MJO propagation speed, underlining the importance of the two-way feedback between the MJO and the diurnal cycle of SST and the need to accurately represent this process in coupled models.
| Item Type: | Article |
|---|---|
| Additional Information: | Funding information: Natural Environment Research Council (NERC) and ARIES DTP [grant NE/S007334/1] and Terra Maris project [grant NE/R016704/1]. |
| Uncontrolled Keywords: | madden–julian oscillation,convection,diurnal warm layer,ocean–atmosphere coupling,atmospheric science ,/dk/atira/pure/subjectarea/asjc/1900/1902 |
| Faculty \ School: | Faculty of Science Faculty of Science > School of Environmental Sciences Faculty of Science > School of Natural Sciences (former - to 2024) University of East Anglia Research Groups/Centres > Theme - ClimateUEA |
| UEA Research Groups: | Faculty of Science > Research Groups > Centre for Ocean and Atmospheric Sciences Faculty of Science > Research Groups > Climatic Research Unit Faculty of Science > Research Groups > Fluids & Structures Faculty of Science > Research Groups > Numerical Simulation, Statistics & Data Science |
| Related URLs: | |
| Depositing User: | LivePure Connector |
| Date Deposited: | 17 Oct 2023 00:43 |
| Last Modified: | 10 Dec 2024 01:42 |
| URI: | https://ueaeprints.uea.ac.uk/id/eprint/93292 |
| DOI: | 10.1002/qj.4599 |
Downloads
Downloads per month over past year
Actions (login required)
 |
View Item |