Articles | Volume 17, issue 13
https://doi.org/10.5194/gmd-17-5145-2024
https://doi.org/10.5194/gmd-17-5145-2024
Development and technical paper
 | 
05 Jul 2024
Development and technical paper |  | 05 Jul 2024

Skin sea surface temperature schemes in coupled ocean–atmosphere modelling: the impact of chlorophyll-interactive e-folding depth

Vincenzo de Toma, Daniele Ciani, Yassmin Hesham Essa, Chunxue Yang, Vincenzo Artale, Andrea Pisano, Davide Cavaliere, Rosalia Santoleri, and Andrea Storto

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Cited articles

Artale, V., Iudicone, D., Santoleri, R., Rupolo, V., Marullo, S., and d'Ortenzio, F.: Role of surface fluxes in ocean general circulation models using satellite Sea Surface Temperature: Validation of and sensitivity to the forcing frequency of the Mediterranean thermohaline circulation, J. Geophys. Res.-Oceans, 107, 29–1, 2002. 
Bernie, D., Guilyardi, E., Madec, G., Slingo, J., and Woolnough, S.: Impact of resolving the diurnal cycle in an ocean–atmosphere GCM. Part 1: A diurnally forced OGCM, Clim. Dynam., 29, 575–590, 2007. 
Bernie, D., Guilyardi, E., Madec, G., Slingo, J. M., Woolnough, S. J., and Cole, J.: Impact of resolving the diurnal cycle in an ocean–atmosphere GCM. Part 2: A diurnally coupled C-GCM, Clim. Dynam., 31, 909–925, 2008. 
Chen, S. S. and Houze Jr., R. A.: Diurnal variation and life-cycle of deep convective systems over the tropical pacific warm pool, Q. J. Roy. Meteor. Soc., 123, 357–388, 1997. 
Copernicus Marine Environment Monitoring Service (CMEMS): OCEANCOLOUR_MED_CHL_L4_NRT_OBSERVATIONS_009_041, Euro Data Cube Public Collections [data set], https://collections.eurodatacube.com/oceancolour-med-chl-l4-nrt-observations-009-041/ (last access: 15 January 2024), 2021. 
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This study explores methods to reconstruct diurnal variations in skin sea surface temperature in a model of the Mediterranean Sea. Our new approach, considering chlorophyll concentration, enhances spatial and temporal variations in the warm layer. Comparative analysis shows context-dependent improvements. The proposed "chlorophyll-interactive" method brings the surface net total heat flux closer to zero annually, despite a net heat loss from the ocean to the atmosphere.
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