QA FOR SATELLITE SEA SURFACE TEMPERATURES USING THE ISAR SHIP-BORNE RADIOMETRIC SYSTEM

Satellite measurements of global sea surface temperature (SST) distribution are increasingly recognised to have great importance for understanding changes in the world's climate, as well as for operational forecasting of the oceans and atmosphere If satellite-derived SSTs are to provide the basis of an essential climate variable (ECV) it is necessary to establish methods for independently verifying their quality Previously the validation of satellite SST products has been performed by comparison with sea temperatures measured by contact thermometers on the hulls of moored or drifting buoys or of ships Such sensors operate below the sea surface, within the top few metres of the water column, recording what is now referred to [1] as SSTdepth Infrared radiometers on satellites measure the temperature of the surface skin of the ocean, referred to as SST,5, However, significant uncertainties are introduced when validation is based on comparisons between SSTdepth and SSTskin because the sea temperature is not uniform across the skin and the upper few metres, especially but not only because of diurnal variability Such uncertainties can be eliminated by using in situ SSTskin measurements as the basis for a satellite SST validation approach which genuinely compares like with like This paper describes the principles and results of such a system which has now been in place for five years It has been used to validate SST measurements from the Advanced Along Track Scanning Radiometer (AATSR) on Envisat Within the collaborative approach developed by the Group for High Resolution SST (GHRSST, [1]) for merging of complementary data from different satellites, the primary role of AATSR data is to provide a reference for bias adjustment of other data Precise validation of AATSR measurements is therefore essential for maintaining the quality of other GHRSST products