scholarly journals The HEX experiment: Determination of the neutral wind field from 120 to 185 km altitude near a stable premidnight auroral arc by triangulating the drift of rocket-deployed chemical trails

2006 ◽  
Vol 111 (A9) ◽  
Author(s):  
E. M. Wescott ◽  
H. Stenbaek-Nielsen ◽  
M. Conde ◽  
Miguel Larsen ◽  
Dirk Lummerzheim
Keyword(s):  
Wind Field ◽  
Neutral Wind

Determination of the wind field over sea

1997 ◽  
Author(s):  
Christian Werner
Keyword(s):  
Wind Field

Determination of domain for diagnostic wind field estimation in Korea

2000 ◽  
Vol 34 (4) ◽  
pp. 595-601 ◽  
Author(s):  
Jin Young Kim ◽  
Young Sung Ghim ◽  
Yong Pyo Kim ◽  
Donald Dabdub
Keyword(s):  
Wind Field ◽  
Field Estimation

scholarly journals Spatial mapping of the thermospheric neutral wind field

1984 ◽  
Vol 32 (4) ◽  
pp. 493-501 ◽  
Author(s):  
C.A. Tepley ◽  
R.G. Burnside ◽  
J.W. Meriwether ◽  
P.B. Hays ◽  
L.L. Cogger
Keyword(s):  
Wind Field ◽  
Spatial Mapping ◽  
Neutral Wind

scholarly journals Sequential observations of the local neutral wind field structure associated with E region plasma layers

2005 ◽  
Vol 110 (A4) ◽  
Author(s):  
R. L. Bishop ◽  
G. D. Earle ◽  
M. F. Larsen ◽  
C. M. Swenson ◽  
C. G. Carlson ◽  
...  
Keyword(s):  
Wind Field ◽  
Field Structure ◽  
Neutral Wind ◽  
E Region ◽  
Region Plasma

scholarly journals Nebelkarten der Schweiz

1991 ◽  
Vol 46 (1) ◽  
pp. 21-31 ◽  
Author(s):  
F. Troxler ◽  
H. Wanner
Keyword(s):  
Satellite Data ◽  
Wind Field ◽  
Early Morning ◽  
Air Distribution ◽  
Weather Types ◽  
Cold Air ◽  
Noaa Satellite ◽  
Alpine Foreland

Abstract. The analysis of fog distribution over Switzerland consists of two different studies: The first deals with the spatial determination of fog frequencies and fog types for the early morning. It was realized by using the daily observations of 320 stations. This point by point information was spatially interpolated with the aid ofthe information (mean fog cover frequency) of 94 typical fog distributions detected from NOAA satellite data. The derived fog map of Switzerland includes four different fog zones: ground fog zone, fog-free intermediary and high fog (stratus) zone, fog-free slope zone, lower up-slope fog zone. The result of the second study consists of four maps showing the fog cover frequency of the important weather types with fog layers over the Swiss Alpine foreland. They were traced out by using the above mentioned satellite data. The four maps indicate clearly that the fog and cold air distribution during anticyclonic weather situations is strongly determined by the sub-synoptic pressure and wind field.

scholarly journals Measurements of the E region neutral wind field

1985 ◽  
Vol 33 (4) ◽  
pp. 373-379 ◽  
Author(s):  
L.L. Cogger ◽  
J.S. Murphree ◽  
C.A. Tepley ◽  
J.W. Meriwether
Keyword(s):  
Wind Field ◽  
Neutral Wind ◽  
E Region
Sign in / Sign up

Export Citation Format

Share Document