IMPROVED TECHNIQUES FOR THE DERIVATION OF SEA-SURFACE TEMPERATURES FROM ATSR DATA

Authors
Citation
Ij. Barton, IMPROVED TECHNIQUES FOR THE DERIVATION OF SEA-SURFACE TEMPERATURES FROM ATSR DATA, J GEO RES-O, 103(C4), 1998, pp. 8139-8152
Citations number
17
Categorie Soggetti
Oceanografhy,"Geosciences, Interdisciplinary","Astronomy & Astrophysics","Geochemitry & Geophysics","Metereology & Atmospheric Sciences
Journal title
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
ISSN journal
21699275 → ACNP
Volume
103
Issue
C4
Year of publication
1998
Pages
8139 - 8152
Database
ISI
SICI code
2169-9275(1998)103:C4<8139:ITFTDO>2.0.ZU;2-C
Abstract
A new technique is developed for the analysis of satellite data to pro vide accurate measurements of seasurface temperature (SST). Satellite data sets are partitioned into subsets depending on the value of a sel ected parameter (for example, latitude, total water vapor, and water v apor content of an atmospheric layer) to provide a suite of algorithm coefficients that reduces the errors associated with the derivation of SST. For data sets obtained with the along-track scanning radiometer (ATSR) the data themselves can be used to modify the coefficients used in the SST algorithm, but for other instruments it may be necessary t o use additional data sets to select a correct set of algorithm coeffi cients. A simulated set of ATSR data is used to develop algorithm coef ficients for different atmospheric conditions, and the improvement in SST derivation is demonstrated. For ATSR, when all the data for three infrared channels in both the nadir and forward views are available, t he improvement is marginal, but for situations when there are limited data the improvement is considerable. The analysis suggests that in th e future the best SST analyses will be obtained by developing an inter active system, where the satellite data are ingested into a numerical weather forecast model so that algorithms can be selected and applied with a forecast or analysis of the atmospheric state. The new techniqu es are tested by application to a large global data set of ATSR bright ness temperatures. This analysis highlights the future need for large SST validation data sets that include coincident satellite and surface -based measurements.