Stith, J. L., Avallone, L., Bansemer, A., Basarab, B., Dorsi, S. W., Fuchs, B., Lawson, R. P., Rogers, D. C., Rutledge, S., Toohey, D. W. (2013) Ice particles in the upper anvil regions of mid-latitude continental thunderstorms: the case for frozen-drop aggregates. Atmospheric Chemistry and Physics Discussions, 13 (10). 27019-27052 doi:10.5194/acpd-13-27019-2013
Reference Type | Journal (article/letter/editorial) | ||
---|---|---|---|
Title | Ice particles in the upper anvil regions of mid-latitude continental thunderstorms: the case for frozen-drop aggregates | ||
Journal | Atmospheric Chemistry and Physics Discussions | ||
Authors | Stith, J. L. | Author | |
Avallone, L. | Author | ||
Bansemer, A. | Author | ||
Basarab, B. | Author | ||
Dorsi, S. W. | Author | ||
Fuchs, B. | Author | ||
Lawson, R. P. | Author | ||
Rogers, D. C. | Author | ||
Rutledge, S. | Author | ||
Toohey, D. W. | Author | ||
Year | 2013 (October 17) | Volume | 13 |
Issue | 10 | ||
Publisher | Copernicus GmbH | ||
DOI | doi:10.5194/acpd-13-27019-2013Search in ResearchGate | ||
Generate Citation Formats | |||
Mindat Ref. ID | 8984744 | Long-form Identifier | mindat:1:5:8984744:6 |
GUID | 0 | ||
Full Reference | Stith, J. L., Avallone, L., Bansemer, A., Basarab, B., Dorsi, S. W., Fuchs, B., Lawson, R. P., Rogers, D. C., Rutledge, S., Toohey, D. W. (2013) Ice particles in the upper anvil regions of mid-latitude continental thunderstorms: the case for frozen-drop aggregates. Atmospheric Chemistry and Physics Discussions, 13 (10). 27019-27052 doi:10.5194/acpd-13-27019-2013 | ||
Plain Text | Stith, J. L., Avallone, L., Bansemer, A., Basarab, B., Dorsi, S. W., Fuchs, B., Lawson, R. P., Rogers, D. C., Rutledge, S., Toohey, D. W. (2013) Ice particles in the upper anvil regions of mid-latitude continental thunderstorms: the case for frozen-drop aggregates. Atmospheric Chemistry and Physics Discussions, 13 (10). 27019-27052 doi:10.5194/acpd-13-27019-2013 | ||
In | (2013, October) Atmospheric Chemistry and Physics Discussions Vol. 13 (10) Copernicus GmbH |
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