维纳斯
纬向流(等离子体)
波长
极地的
地质学
纬向和经向
红外线的
物理
大气科学
遥感
天文
光学
天体生物学
量子力学
等离子体
托卡马克
作者
M. J. S. Belton,P. J. Gierasch,M. D. Smith,P. Helfenstein,P. J. Schinder,James B. Pollack,K. Rages,Andrew P. Ingersoll,K. P. Klaasen,Joseph Veverka,C. D. Anger,M. H. Carr,C. R. Chapman,Merton E. Davies,F. P. Fanale,R. Greeley,R. Greenberg,J. W. Head,David Morrison,G. Neukum,C. B. Pilcher
出处
期刊:Science
[American Association for the Advancement of Science (AAAS)]
日期:1991-09-27
卷期号:253 (5027): 1531-1536
被引量:92
标识
DOI:10.1126/science.253.5027.1531
摘要
Images of Venus taken at 418 (violet) and 986 [near-infrared (NIR)] nanometers show that the morphology and motions of large-scale features change with depth in the cloud deck. Poleward meridional velocities, seen in both spectral regions, are much reduced in the NIR. In the south polar region the markings in the two wavelength bands are strongly anticorrelated. The images follow the changing state of the upper cloud layer downwind of the subsolar point, and the zonal flow field shows a longitudinal periodicity that may be coupled to the formation of large-scale planetary waves. No optical lightning was detected.
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