| タイトル | Validation of the Aura Microwave Limb Sounder Temperature and Geopotential Height Measurements |
| 本文（外部サイト） | http://hdl.handle.net/2060/20070035760 |
| 著者（英） | Froidevaux, L.; Snyder, W. V.; Jiang, J. H.; Lambert, A.; Daffer, W. H.; Li, J.-L. F.; Russell, J. M., III; Krueger, K.; Jarnot, R. F.; Cofield, R. E.; Manney, G. L.; Fetzer, E. J.; Ao, C. O.; Pawson, S.; Santee, M. L.; Knosp, B. W.; Fuller, R. A.; Bernath, P. F.; Drouin, B. J.; Jiang, Y. B.; Livesey, N. J.; Mlynczak, M. G.; Read, W. G.; Schwartz, M. J.; Boone, C. D. |
| 著者所属（英） | Jet Propulsion Lab., California Inst. of Tech.; NASA Goddard Space Flight Center |
| 発行日 | 2007-01-01 |
| 言語 | eng |
| 内容記述 | This paper describes the retrievals algorithm used to determine temperature and height from radiance measurements by the Microwave Limb Sounder on EOS Aura. MLS is a "limbscanning" instrument, meaning that it views the atmosphere along paths that do not intersect the surface - it actually looks forwards from the Aura satellite. This means that the temperature retrievals are for a "profile" of the atmosphere somewhat ahead of the satellite. Because of the need to view a finite sample of the atmosphere, the sample spans a box about 1.5km deep and several tens of kilometers in width; the optical characteristics of the atmosphere mean that the sample is representative of a tube about 200-300km long in the direction of view. The retrievals use temperature analyses from NASA's Goddard Earth Observing System, Version 5 (GEOS-5) data assimilation system as a priori states. The temperature retrievals are somewhat deperrde~zt on these a priori states, especially in the lower stratosphere. An important part of the validation of any new dataset involves comparison with other, independent datasets. A large part of this study is concerned with such comparisons, using a number of independent space-based measurements obtained using different techniques, and with meteorological analyses. The MLS temperature data are shown to have biases that vary with height, but also depend on the validation dataset. MLS data are apparently biased slightly cold relative to correlative data in the upper troposphere and slightly warm in the middle stratosphere. A warm MLS bias in the upper stratosphere may be due to a cold bias in GEOS-5 temperatures. |
| NASA分類 | Meteorology and Climatology |
| 権利 | Copyright, Distribution as joint owner in the copyright |
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