| All Time | Past Year | Past 30 Days | |
|---|---|---|---|
| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 370 | 180 | 50 |
| PDF Downloads | 154 | 49 | 6 |
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.
We are aware of a technical issue preventing figures and tables from showing in some newly published articles in the full-text HTML view.
While we are resolving the problem, please use the online PDF version of these articles to view figures and tables.
The vertical circulation and the changes of atmospheric structure during the formation of a shear line in the upper atmosphere are studied. The vertical distribution of divergence and convergence at the trough line is determined, assuming adiabatic processes. A scheme for the process of formation of an upper shear-line is proposed. A comparison of this process with that involved in the formation of upper cut-off cold lows is presented.
The vertical circulation and the changes of atmospheric structure during the formation of a shear line in the upper atmosphere are studied. The vertical distribution of divergence and convergence at the trough line is determined, assuming adiabatic processes. A scheme for the process of formation of an upper shear-line is proposed. A comparison of this process with that involved in the formation of upper cut-off cold lows is presented.
| All Time | Past Year | Past 30 Days | |
|---|---|---|---|
| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 370 | 180 | 50 |
| PDF Downloads | 154 | 49 | 6 |
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