Paper
8 December 1999 Upper stratospheric temperature climatology derived from SAGE II observations: preliminary results
Pi-Huan Wang, Derek M. Cunnold, H. J. Wang, William P. Chu, Larry W. Thomason
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Abstract
This study shows that the temperature information in the upper stratosphere can be derived from the SAGE II 385-nm observations. The preliminary results indicate that the zonal mean temperature increases with altitude below 50 km and decreases above 50 km. At 50 km, a regional maximum of 263 K is located in the tropics, and a minimum of 261 K occurs in the subtropics in both hemispheres. The derived long-term temperature changes from 1985 to 1997 reveal a statistically significant negative trend of -2 to -2.5 K/decade in the tropical upper stratosphere and about -2 K/decade in the subtropics near the stratopause. At latitudes poleward of 50 degrees, the results show a statistically significant positive trend of about 1 K/decade in the upper stratosphere. The preliminary results also show large annual temperature oscillations in the extratropics with a maximum amplitude of approximately 8 K located at about 44 km near 50 degrees in both hemispheres during local summer. In addition, the semiannual oscillation is found to be a maximum in the tropics with a peak amplitude of approximately 3.3 K located at about 42 km during the equinox.
© (1999) COPYRIGHT Society of Photo-Optical Instrumentation Engineers (SPIE). Downloading of the abstract is permitted for personal use only.
Pi-Huan Wang, Derek M. Cunnold, H. J. Wang, William P. Chu, and Larry W. Thomason "Upper stratospheric temperature climatology derived from SAGE II observations: preliminary results", Proc. SPIE 3867, Satellite Remote Sensing of Clouds and the Atmosphere IV, (8 December 1999); https://doi.org/10.1117/12.373063
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KEYWORDS
Stratosphere

Temperature metrology

Knowledge management

Climatology

Error analysis

Mass attenuation coefficient

Optical testing

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