Titlebook: Oceanography from Space; J. F. R. Gower Book 1981 Plenum Press, New York 1981 Atlantic Ocean.Coast.Meteorology.Sea ice.marine.ocean.oceano

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Satellite Sea Surface Temperature Measurements an Introductioned satellite infrared observations from achieving agreement with ship and other in-situ results to better than 1° C average r.m.s. temperature error. Some errors are definitely due to atmospheric contamination of the satellite data, and the problems of correcting these for current satellites were di

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极肥胖

Corrections for Atmospheric Attenuation and Surface Reflectivity in Satellite-Borne SST Measurementsrime climate variable; SST patterns indirectly show special features of oceanic circulation, and SST values above a certain threshold depict possible hurricane generating areas. The most transparent wavelength region with simultaneously high enough radiance values has to be chosen for accurate SST s

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Interannual Variability of Arabian Sea Surface Temperature 1977. Satellite derived temperature fields are found to have lower rms variability and to be better adapted to large scale pattern identification while ship observations have greater mean accuracy, resolve finer scales near the coastal boundaries and show larger rms variability. Mean satellite retr

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On the Accuracy of Satellite-Observed Sea Surface Temperatureshe Pacific coast of Canada indicates that in each case a linear regression is sufficient to relate the two sets of data. The standard error of estimate for the temperatures observed by the above satellites were: ±0.5°C, ±0.6°C, ±0.3 – ±0.4°C, ±0.6°C and ±0.5°C, respectively. When reliable ground tru

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NASA’s Oceanic Remote Sensing Plans for the 1980’s this in mind, we are working to effect a closer coupling between the remote sensing and oceanographic communities, so that we will be prepared to optimally exploit the oceanic satellite missions planned for the latter part of this decade.