Characteristics of Supercooled Liquid Water in Clouds at Mountaintop Sites in the Colorado RockiesSource: Journal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 009::page 1271Author:Hindman, Edward E.
DOI: 10.1175/1520-0450(1986)025<1271:COSLWI>2.0.CO;2Publisher: American Meteorological Society
Abstract: Observations and measurements were made of supercooled liquid water in clouds which enveloped high elevation sites in the Colorado Rocky Mountains for the winters of 1980/81 through 1983/84. The observations showed that liquid water was more frequent at the southern and northern Rocky sites than at the central sites. Eighty percent of the liquid water periods persisted 3 to 20 h at the northern Rocky site. This site was enveloped by supercooled liquid cloud 24% of the time during the months of December 1981 and January 1982. Average liquid water contents at the sites ranged between 0.14 to 0.23 g m?3; the maximum individual value was 0.60 g m?3. The measurements indicated that substantial amounts of liquid water were flowing over the Colorado Rockies at mountaintop heights.
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| contributor author | Hindman, Edward E. | |
| date accessioned | 2017-06-09T14:01:21Z | |
| date available | 2017-06-09T14:01:21Z | |
| date copyright | 1986/09/01 | |
| date issued | 1986 | |
| identifier issn | 0733-3021 | |
| identifier other | ams-11048.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4146233 | |
| description abstract | Observations and measurements were made of supercooled liquid water in clouds which enveloped high elevation sites in the Colorado Rocky Mountains for the winters of 1980/81 through 1983/84. The observations showed that liquid water was more frequent at the southern and northern Rocky sites than at the central sites. Eighty percent of the liquid water periods persisted 3 to 20 h at the northern Rocky site. This site was enveloped by supercooled liquid cloud 24% of the time during the months of December 1981 and January 1982. Average liquid water contents at the sites ranged between 0.14 to 0.23 g m?3; the maximum individual value was 0.60 g m?3. The measurements indicated that substantial amounts of liquid water were flowing over the Colorado Rockies at mountaintop heights. | |
| publisher | American Meteorological Society | |
| title | Characteristics of Supercooled Liquid Water in Clouds at Mountaintop Sites in the Colorado Rockies | |
| type | Journal Paper | |
| journal volume | 25 | |
| journal issue | 9 | |
| journal title | Journal of Climate and Applied Meteorology | |
| identifier doi | 10.1175/1520-0450(1986)025<1271:COSLWI>2.0.CO;2 | |
| journal fristpage | 1271 | |
| journal lastpage | 1279 | |
| tree | Journal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 009 | |
| contenttype | Fulltext |