Errors induced by ozone field horizontal inhomogeneities into simulated nadir-viewing orbital backscatter UV measurements
Autor: | Martin Felder, Paul Poli, Joanna Joiner |
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Rok vydání: | 2007 |
Předmět: |
Atmospheric Science
Ecology Backscatter Solar zenith angle Paleontology Soil Science Forestry Aquatic Science Oceanography Atmospheric sciences Ozone depletion Atmosphere Geophysics Space and Planetary Science Geochemistry and Petrology Earth and Planetary Sciences (miscellaneous) Radiance Radiative transfer Nadir Environmental science Tropopause Earth-Surface Processes Water Science and Technology |
Zdroj: | Journal of Geophysical Research. 112 |
ISSN: | 0148-0227 |
DOI: | 10.1029/2005jd006769 |
Popis: | Received 15 October 2005; revised 2 August 2006; accepted 25 August 2006; published 4 January 2007. [1] Radiative transfer calculations for nadir-viewing satellites normally assume the atmosphere to be horizontally homogeneous. Yet it has been shown recently that horizontal gradients can lead to significant errors in satellite infrared and microwave soundings. We extend the methodology to nadir backscatter ultraviolet forward modeling and present a first estimate of the effect’s magnitude. The Solar Backscatter Ultraviolet/2 (SBUV/2) instrument, a nadir sounder, serves as our test bed. We find that the RMS error in calculated SBUV radiance induced by ozone inhomogeneities ranges between 0.05 and 0.3% (0.1–0.5%) for the 318 nm (306 and 313 nm) channel. The lower (higher) estimate corresponds to soundings with small (high) solar zenith angle. Occurrence of higher errors, particularly at wavelengths longer than 300 nm, coincides with some of the most interesting atmospheric phenomena like tropopause folds and the south polar ozone hole. This leads to a seasonal variation of the magnitude of the effect. Because of the mostly zonal variability of the ozone distribution, there is also the possibility that biases may be introduced, which is particularly critical if the data are to be assimilated or used to determine trends. The results presented are tested for robustness using different model atmospheres. |
Databáze: | OpenAIRE |
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