64
datasets. When no water vapor data is available the inaccuracy in the retrieved temperature is in fact
more crucial for land data (up to 6 K) and mean climatic SW coefficients should not be used for accurate
temperature retrievals. Consequently the determination of the water vapor content is necessary.
Therefore, the possibility to determine W from space, using the Split-Window variance method for
instance, has now to be investigated.
For SST measurements the Double-Viewing method seems to be a valuable first approach giving
good results when no other data than Nadir and Forward satellite temperatures are available. According
to the simulation, the Double-Viewing method (which does not necessitate any ancillary information in
its accurate and simplified version) is supposed to give SST with a bias lower than 0.5 K when the water
vapor amount is lower than 3 g/cm^. Both applications with ATSR data show actually a mean error lower
than this simulated value (either when compared with ground truth data or with Lowtran7 retrieved
temperature). Further studies have to be done for LST retrieval because it proves difficult to derive a
straightforward LST double-viewing method.
Acknowledgements
We would like to thanks Noelle Scott for providing us with the TIGR dataset and the 4A
program, and for fruitful discussions. We are grateful to Xingfa Gu who provided us with the CRAU92
data, to I. J. Barton who provided us with the Coral Sea data and also to RAL for the other ATSR data.
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