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Ocean Science An interactive open-access journal of the European Geosciences Union
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Volume 10, issue 5
Ocean Sci., 10, 745–758, 2014
https://doi.org/10.5194/os-10-745-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
Ocean Sci., 10, 745–758, 2014
https://doi.org/10.5194/os-10-745-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 02 Sep 2014

Research article | 02 Sep 2014

Characterisation and quantification of regional diurnal SST cycles from SEVIRI

I. Karagali1 and J. L. Høyer2 I. Karagali and J. L. Høyer
  • 1DTU Wind Energy, Technical University of Denmark, Risø Campus, Building 125, Roskilde, 4000, Denmark
  • 2Centre for Ocean and Ice (COI), Danish Meteorological Institute (DMI), Lyngbyvej 100, 2100, Denmark

Abstract. Hourly SST (sea surface temperature) fields from the geostationary Spinning Enhanced Visible and Infrared Imager (SEVIRI) offer a unique opportunity for the characterisation and quantification of the diurnal cycle of SST in the Atlantic Ocean, the Mediterranean Sea and the northern European shelf seas. Six years of SST fields from SEVIRI are validated against the Advanced Along-Track Scanning Radiometer (AATSR) Reprocessed for Climate (ARC) data set. The overall SEVIRI–AATSR bias is −0.07 K, and the standard deviation is 0.51 K, based on more than 53 × 106 match-ups. Identification of the diurnal signal requires an SST foundation temperature field representative of well-mixed conditions which typically occur at night-time or under moderate and strong winds. Such fields are generated from the SEVIRI archive and are validated against pre-dawn SEVIRI SSTs and night-time SSTs from drifting buoys. The different methodologies tested for the foundation temperature fields reveal variability introduced by averaging night-time SSTs over many days compared to single-day, pre-dawn values. Diurnal warming is most pronounced in the Mediterranean and Baltic seas while weaker diurnal signals are found in the tropics. Longer diurnal warming duration is identified in the high latitudes compared to the tropics. The maximum monthly mean diurnal signal can be up to 0.5 K in specific regions.

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