Operational measurement of sea surface temperatures at CMS Lannion from NOAA-7 AVHRR data
- 1 August 1986
- journal article
- research article
- Published by Taylor & Francis in International Journal of Remote Sensing
- Vol. 7 (8), 953-984
- https://doi.org/10.1080/01431168608948903
Abstract
Data from the NOAA-7 Advanced Very-High-Resolution Radiometer (AVHRR) have been used on a routine basis for sea surface temperature (SST) retrieval at the Centre de Meteorologie Spatiale (CMS) in Lannion (France) since September 1983. Operational SST retrieval is still practised at CMS, using NOAA-9 data. Two methods are used. The first, which is automatic, produces numerical fields (resolution: 15 × 15 nautical miles); the second is manual and produces graphic documents (resolution about 10 km). The corresponding products are published in a monthly bulletin, SATMER. The accuracy of satellite SSTs has been tested by various methods, the results of which are discussed. Some case studies of SST time variability in the Mediterranean are presented. One of the main conclusions is the need for mesoscale (10 km) numerical SST fields produced as often as possible (daily) by interactive methods.Keywords
This publication has 6 references indexed in Scilit:
- Satellite multichannel infrared measurements of sea surface temperature of the N.E. Atlantic Ocean using AVHRR/2Quarterly Journal of the Royal Meteorological Society, 1984
- Theory and validation of the multiple window sea surface temperature techniqueJournal of Geophysical Research: Oceans, 1984
- Improved Ocean Surface Temperatures From Space—Comparisons With Drifting BuoysBulletin of the American Meteorological Society, 1984
- A Two-Dimensional Histogram Procedure to Analyze Cloud Cover from NOAA Satellite High-Resolution ImageryJournal of Climate and Applied Meteorology, 1983
- Surface Temperature Fronts in the Mediterranean Sea from Infrared Satellite ImageryElsevier Oceanography Series, 1982
- Atmospheric correction of infrared measurements of sea surface temperature using channels at 3.7, 11 and 12 ?mBoundary-Layer Meteorology, 1980