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Aitala EM Amato S Anjos JC Appel JA Ashery D Banerjee S Bediaga I Blaylock G Bracker SB Burchat PR Burnstein RA Carter T Carvalho HS Copty NK Costa I Cremaldi LM Darling C Denisenko K Fernandez A Gagnon P Gerzon S Gobel C Gounder K Halling AM Herrera G Hurvits G James C Kasper PA Kwan S Langs DC Leslie J Lundberg B MayTal-Beck S Meadows B de Mello Neto JR Milburn RH de Miranda JM Napier A Nguyen A d'Oliveira AB O'Shaughnessy K Peng KC Perera LP Purohit MV Quinn B Radeztsky S Rafatian A 《Physical review letters》1996,77(12):2384-2387
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F. G. Fernald B. G. Schuster E. F. Danielsen D. G. Deaven 《Optical and Quantum Electronics》1975,7(3):141-145
Airborne lidar currently offers the best means of observing the synoptic scale variability in the distribution of aerosols within the lower stratosphere. In this paper, some basic considerations regarding the processing and interpretation of this type of data are discussed. Results from the April 1973 flight between Madrid and Washington, D.C. are presented.The National Centre for Atmospheric Research is sponsored by the National Science Foundation. 相似文献
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