| All Time | Past Year | Past 30 Days | |
|---|---|---|---|
| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 176 | 28 | 0 |
| PDF Downloads | 14 | 11 | 0 |
Displayed acceptance dates for articles published prior to 2023 are approximate to within a week. If needed, exact acceptance dates can be obtained by emailing amsjol@ametsoc.org.
The laser radar system at Kingston, Jamaica (189N, 17°W) has been used to study periodic variations in atmospheric density at altitudes between 68 and 100 km. A major feature of these variations is an oscillation with a vertical wavelength of 12–14 km, descending phase, and a probable period of 24 h. This has been identified as the θ3ω,1 atmospheric tidal oscillation and a comparison of its observed characteristics with theoretical predictions for this tidal mode shows good agreement.
The laser radar system at Kingston, Jamaica (189N, 17°W) has been used to study periodic variations in atmospheric density at altitudes between 68 and 100 km. A major feature of these variations is an oscillation with a vertical wavelength of 12–14 km, descending phase, and a probable period of 24 h. This has been identified as the θ3ω,1 atmospheric tidal oscillation and a comparison of its observed characteristics with theoretical predictions for this tidal mode shows good agreement.
| All Time | Past Year | Past 30 Days | |
|---|---|---|---|
| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 176 | 28 | 0 |
| PDF Downloads | 14 | 11 | 0 |
AMS Publications
Get Involved with AMS
Follow Us
Contact Us
Email: amsjol@ametsoc.org
Phone: 617-227-2425
Fax: 617-742-8718
Headquarters:
45 Beacon Street
Boston, MA 02108-3693
DC Office:
1200 New York Ave NW
Suite 500
Washington, DC 200005-3928