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Effect of Small‐Scale Gravity Waves on Polar Mesospheric Clouds Observed From CIPS/AIM
Author(s) -
Gao Haiyang,
Li Licheng,
Bu Lingbing,
Zhang Qilin,
Tang Yuanhe,
Wang Zhen
Publication year - 2018
Publication title -
journal of geophysical research: space physics
Language(s) - English
Resource type - Journals
eISSN - 2169-9402
pISSN - 2169-9380
DOI - 10.1029/2017ja024855
Subject(s) - albedo (alchemy) , atmospheric sciences , aeronomy , cloud albedo , wavelength , environmental science , polar , mesosphere , effective radius , water vapor , gravity wave , radius , physics , meteorology , atmosphere (unit) , gravitational wave , astronomy , optics , stratosphere , cloud computing , cloud cover , art , computer security , galaxy , performance art , computer science , art history , operating system
Data from the Cloud Imaging and Particle Size experiment on the Aeronomy of Ice in the Mesosphere (AIM) satellite are employed to study the impact of small‐scale gravity wave (GW) on albedo, ice water content (IWC), and particle radius (PR) of polar mesospheric clouds. Overall, 23,987 eligible GW events, with a horizontal wavelength of 20–150 km are eventually extracted from Cloud Imaging and Particle Size level 2 orbit albedo maps during 2007–2011. The overall statistical results show that when small‐scale GWs travel horizontally in polar mesospheric clouds, they can amplify the albedo and IWC by a rate of 10.0–22.6%, while reducing the PR by as much as −7.01%. Owing to the strong temporal and spatial dependences, the albedo and IWC variations are larger on an average during the core of the season, while they decrease during the initial and final periods of the season. The obvious zonal asymmetries are also found. The albedo variations show a positive linear relation with the GW amplitudes in albedo, as opposed to a negative linear relation with GW horizontal wavelengths. In most of the GW events, the periodic variation in the trend of albedo exhibits an anticorrelation with that of PR. Combining previous research studies with our results, we deduce that the rapid change in particle concentration and the upward movement of water vapor by GWs may be very important aspects for explaining the influence mechanism.