| All Time | Past Year | Past 30 Days | |
|---|---|---|---|
| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 184 | 26 | 1 |
| PDF Downloads | 20 | 13 | 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 c-axis orientation distributions of ice formed by the accretion of supercooled droplets have been determined for a wide range of air and deposit temperatures. There are peaks in the distributions which may be related to the air temperature. Consequently, quantitative information on the growth environment of a hailstone can be obtained from its crystallographic structure.
The c-axis orientation distributions of ice formed by the accretion of supercooled droplets have been determined for a wide range of air and deposit temperatures. There are peaks in the distributions which may be related to the air temperature. Consequently, quantitative information on the growth environment of a hailstone can be obtained from its crystallographic structure.
| All Time | Past Year | Past 30 Days | |
|---|---|---|---|
| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 184 | 26 | 1 |
| PDF Downloads | 20 | 13 | 2 |
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