GROUND-BASED NEAR-INFRARED IMAGING OBSERVATIONS OF VENUS DURING THE GALILEO ENCOUNTER

被引:68
作者
CRISP, D
MCMULDROCH, S
STEPHENS, SK
SINTON, WM
RAGENT, B
HODAPP, KW
PROBST, RG
DOYLE, LR
ALLEN, DA
ELIAS, J
机构
[1] CALTECH,PALOMAR OBSERV,PASADENA,CA 91125
[2] CALTECH,DIV GEOL & PLANETARY SCI,PASADENA,CA 91125
[3] LAS CAMPANAS OBSERV,LA SERENE,CHILE
[4] UNIV HAWAII,INST ASTRON,HONOLULU,HI 96822
[5] SAN JOSE STATE UNIV FDN,SAN JOSE,CA 95192
[6] UNIV HAWAII,MAUNA KEA OBSERV,MAUNA KEA,HI
[7] KITT PEAK NATL OBSERV,TUCSON,AZ 85719
[8] NASA,AMES RES CTR,MOFFETT FIELD,CA 94035
[9] ANGLO AUSTRALIAN OBSERV,EPPING,NSW 2121,AUSTRALIA
[10] CERRO TOLOLO INTERAMER OBSERV,LA SERENA,CHILE
关键词
D O I
10.1126/science.253.5027.1538
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Near-infrared images of Venus, obtained from a global network of ground-based observatories during January and February 1990, document the morphology and motions of the night-side near-infrared markings before, during, and after the Galileo Venus encounter. A dark cloud extended halfway around the planet at low latitudes (< +/- 40-degrees) and persisted throughout the observing program. It had a rotation period of 5.5 +/- 0.15 days. The remainder of this latitude band was characterized by small-scale (400 to 1000 kilometers) dark and bright markings with rotation periods of 7.4 +/- 1 days. The different rotation periods for the large dark cloud and the smaller markings suggests that they are produced at different altitudes. Mid-latitudes (+/- 40-degrees to 60-degrees) were usually occupied by bright east-west bands. The highest observable latitudes (+/- 60-degrees to 70-degrees) were always dark and featureless, indicating greater cloud opacity. Maps of the water vapor distribution show no evidence for large horizontal gradients in the lower atmosphere of Venus.
引用
收藏
页码:1538 / 1541
页数:4
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