Wind Streaks on Venus: Clues to Atmospheric Circulation
Author(s) -
R. Greeley,
G. Schubert,
D. Limonadi,
K. Bender,
William I. Newman,
Peggy E. Thomas,
C. M. Weitz,
Stephen D. Wall
Publication year - 1994
Publication title -
science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 12.556
H-Index - 1186
eISSN - 1095-9203
pISSN - 0036-8075
DOI - 10.1126/science.263.5145.358
Subject(s) - geology , hadley cell , venus , streak , atmospheric circulation , global wind patterns , atmosphere (unit) , equator , aeolian processes , atmosphere of venus , impact crater , atmospheric sciences , climatology , meteorology , geophysics , astrobiology , general circulation model , geodesy , geography , oceanography , climate change , paleontology , physics , latitude
Magellan images reveal surface features on Venus attributed to wind processes. Sand dunes, wind-sculpted hills, and more than 5830 wind streaks have been identified. The streaks serve as local "wind vanes," representing wind direction at the time of streak formation and allowing the first global mapping of near-surface wind patterns on Venus. Wind streaks are oriented both toward the equator and toward the west. When streaks associated with local transient events, such as impact cratering, are deleted, the westward component is mostly lost but the equatorward component remains. This pattern is consistent with a Hadley circulation of the lower atmosphere.
Accelerating Research
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom
Address
John Eccles HouseRobert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom