| All Time | Past Year | Past 30 Days | |
|---|---|---|---|
| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 163 | 42 | 2 |
| PDF Downloads | 12 | 3 | 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.
A study of the influence of mountain-generated cumulonimbus systems on the rainfall of the northern Great Plains, using daily rainfalls and satellite images, has shown the seasonal variations and areal extent of the rain swaths. Rainfall from these systems is greatest during June and July. The greatest rainfalls occur ∼400 km northeast from the eastern boundaries of the mountains; the rain then decreases to beyond 1000 km.
A study of the influence of mountain-generated cumulonimbus systems on the rainfall of the northern Great Plains, using daily rainfalls and satellite images, has shown the seasonal variations and areal extent of the rain swaths. Rainfall from these systems is greatest during June and July. The greatest rainfalls occur ∼400 km northeast from the eastern boundaries of the mountains; the rain then decreases to beyond 1000 km.
| All Time | Past Year | Past 30 Days | |
|---|---|---|---|
| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 163 | 42 | 2 |
| PDF Downloads | 12 | 3 | 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