Differences between mean monthly winds obtained from actual observations and geostrophic wind derived from mean monthly altitudes of constant-pressure surfaces are examined for January and July at four levels between 10,000 and 40,000 ft. Differences in speed for both east-west and north-south components are significantly and unexpectedly large. These results demonstrate the advantage of using observed winds rather than deduced values to provide climatic winds at altitudes betweet 10,000 and 40,000 ft. Modification of the existing system to include winds from actual observations wherever and whenever possible is recommended. (Author)."Aeronomy Laboratory Project 8624."ADA021897 (from http://www.dtic.mil).""22 January 1976."Includes bibliogr...
The equatorial-stratospheric wind that shows a Quasi Biennial Oscillation (22-32 months) has been re...
Resultant surface winds presented as monthly averages for each hour of the day for two years have be...
Earth’s atmosphere is commonly divided into different layers based on the change of temperature with...
The objective of this study is to compare observed mean meridional winds with those deduced from the...
International audienceThis study consists to retrieve wind data from trajectories of balloon flights...
Two sets of wind data were compared in this paper for two days with different circulation forms: com...
Over 1200 hours of simultaneous, interplanetary, solar wind data from the satellites Explorer 33 and...
The atmospheric properties above three sites (Dome A, Dome C and the South Pole) are investigated ...
International audienceThis study focuses on the ability of the ECMWF ERA-Interim reanalysis to repre...
An updated empirical climatic zonally averaged prevailing wind model for the upper mesosphere/lower...
This project involved the comparison of horizontal winds in the upper mesosphere at 80-105 km which ...
Yearly percentiles of geostrophic wind speeds serve as a widely used proxy for assessing past storm ...
Monthly & annual wind distributions as function of altitude for pacific missile rang
The equatorial-stratospheric wind that shows a Quasi Biennial Oscillation (22-32 months) has been re...
Resultant surface winds presented as monthly averages for each hour of the day for two years have be...
Earth’s atmosphere is commonly divided into different layers based on the change of temperature with...
The objective of this study is to compare observed mean meridional winds with those deduced from the...
International audienceThis study consists to retrieve wind data from trajectories of balloon flights...
Two sets of wind data were compared in this paper for two days with different circulation forms: com...
Over 1200 hours of simultaneous, interplanetary, solar wind data from the satellites Explorer 33 and...
The atmospheric properties above three sites (Dome A, Dome C and the South Pole) are investigated ...
International audienceThis study focuses on the ability of the ECMWF ERA-Interim reanalysis to repre...
An updated empirical climatic zonally averaged prevailing wind model for the upper mesosphere/lower...
This project involved the comparison of horizontal winds in the upper mesosphere at 80-105 km which ...
Yearly percentiles of geostrophic wind speeds serve as a widely used proxy for assessing past storm ...
Monthly & annual wind distributions as function of altitude for pacific missile rang
The equatorial-stratospheric wind that shows a Quasi Biennial Oscillation (22-32 months) has been re...
Resultant surface winds presented as monthly averages for each hour of the day for two years have be...
Earth’s atmosphere is commonly divided into different layers based on the change of temperature with...