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DOI10.1029/2018GL078501
First Observed Temporal Development of a Noctilucent Cloud Ice Void
Megner, Linda1; Stegman, Jacek1; Pautet, Pierre-Dominique2; Taylor, Michael J.2
2018-09-28
发表期刊GEOPHYSICAL RESEARCH LETTERS
ISSN0094-8276
EISSN1944-8007
出版年2018
卷号45期号:18页码:10003-10010
文章类型Article
语种英语
国家Sweden; USA
英文摘要

Noctilucent clouds are thin ice clouds that appear around the summer polar mesopause. Recently, the Cloud Imaging and Particle Size instrument on the AIM satellite discovered nearly circular ice free regions within the clouds-denoted as "ice voids." The origin of these ice voids is not known. Their existence has so far only been reported by Cloud Imaging and Particle Size, which only can give very limited information of the time scales involved. On 4 July 2010, such an ice void was registered by our ground-based camera taking images with 30-s time interval. We thus here present the first full temporal development of an ice void. Surprisingly, the void did not drift with the prevailing wind as cloud features around it, but instead remained notably stationary for its entire existence of approximately 1 hr. This indicates that that the origin is of stationary character, rather than a rapid change of the local atmosphere.


Plain Language Summary Noctilucent clouds are ice clouds that appear high in the atmosphere, about 80 km above the summer pole. By observing them we have learned a lot about the remote and inaccessible region where they form. Recently, a satellite borne instrument discovered nearly circular ice-free regions within the clouds, denoted as "ice voids." The origin of these voids is a mystery-we do not know what causes the clouds to disappear in large circular areas. So far these voids have only been observed from satellites, which only can take pictures of the clouds when they pass above once every 1.5 hr-longer than most ice voids exist. This means that until now we completely lack observations of the development and disappearance of the voids. Here we therefore present the first full temporal development of a void, as observed by our ground-based camera taking images every 30 s. Surprisingly, the void did not drift with the wind as cloud features around it, but it remained notably stationary for approximately 1 hr. These observations give important clues to help us solve the mystery of the origin of these voids-they suggest a steady local heating of the atmosphere as the cause.


领域气候变化
收录类别SCI-E
WOS记录号WOS:000447761300073
WOS关键词POLAR MESOSPHERIC CLOUDS ; PERIOD GRAVITY-WAVES
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
引用统计
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/26630
专题气候变化
作者单位1.Stockholm Univ, Dept Meteorol, Stockholm, Sweden;
2.Utah State Univ, Ctr Atmospher & Space Sci, Logan, UT 84322 USA
推荐引用方式
GB/T 7714
Megner, Linda,Stegman, Jacek,Pautet, Pierre-Dominique,et al. First Observed Temporal Development of a Noctilucent Cloud Ice Void[J]. GEOPHYSICAL RESEARCH LETTERS,2018,45(18):10003-10010.
APA Megner, Linda,Stegman, Jacek,Pautet, Pierre-Dominique,&Taylor, Michael J..(2018).First Observed Temporal Development of a Noctilucent Cloud Ice Void.GEOPHYSICAL RESEARCH LETTERS,45(18),10003-10010.
MLA Megner, Linda,et al."First Observed Temporal Development of a Noctilucent Cloud Ice Void".GEOPHYSICAL RESEARCH LETTERS 45.18(2018):10003-10010.
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