| All Time | Past Year | Past 30 Days | |
|---|---|---|---|
| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 89 | 46 | 1 |
| PDF Downloads | 41 | 22 | 2 |
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 coherent atmospheric pressure waves traveling at sonic velocities from a squall line storm 20–75 km. distant, were observed in detail for a period of 100 min. The measurements indicate that the infrasonic wave was generated in or near the leading edge of the storm. Infrasonic waves were not observed from funnel clouds or from the heavy rain clouds accompanying the storm front.
The coherent atmospheric pressure waves traveling at sonic velocities from a squall line storm 20–75 km. distant, were observed in detail for a period of 100 min. The measurements indicate that the infrasonic wave was generated in or near the leading edge of the storm. Infrasonic waves were not observed from funnel clouds or from the heavy rain clouds accompanying the storm front.
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