Comparison of polar mesospheric cloud measurements from the Cloud Imaging and Particle Size experiment and the solar backscatter ultraviolet instrument in 2007

被引:35
作者
Benze, Susanne [1 ,2 ]
Randall, Cora E. [1 ,2 ]
DeLand, Matthew T. [3 ]
Thomas, Gary E. [4 ]
Rusch, David W. [4 ]
Bailey, Scott M. [5 ]
Russell, James M., III [6 ]
McClintock, William [4 ]
Merkel, Aimee W. [4 ]
Jeppesen, Chris [4 ]
机构
[1] Univ Colorado, Atmospher & Space Phys Lab, Boulder, CO 80309 USA
[2] Univ Colorado, Dept Atmospher & Ocean Sci, Boulder, CO 80309 USA
[3] SSAI, Greenbelt, MD USA
[4] Univ Colorado, Atmospher & Space Phys Lab, Boulder, CO 80303 USA
[5] Virginia Polytech & State Univ, Bradley Dept Elect & Comp Engn, Blacksburg, VA 24061 USA
[6] Hampton Univ, Ctr Atmospher Sci, Hampton, VA 23668 USA
基金
美国国家航空航天局;
关键词
Polar Mesospheric Cloud; PMC; SBUV; AIM; Validation; Noctilucent cloud; SBUV;
D O I
10.1016/j.jastp.2008.07.014
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We compare measurements from the Aeronomy of Ice in the Mesosphere (AIM) Cloud Imaging and Particle Size (CIPS) experiment to the NOAA-17 solar backscatter ultraviolet (SBUV/2) instrument during the 2007 Northern Hemisphere polar mesospheric cloud (PMC) season. Daily average Rayleigh scattering albedos determined from identical footprints from the CIPS nadir camera and SBUV/2 agree to better than similar to 5% throughout the season. Average PMC brightness values derived from the two instruments agree to within +/- 10%. PMC occurrence frequencies are on average similar to 5% to nearly a factor of two higher in CIPS, depending on latitude. Agreement is best at high latitudes where clouds are brighter and more frequent. The comparisons indicate that AIM CIPS data are valid for scientific analyses. They also show that CIPS measurements can be linked to the long time series of SBUV/2 data to investigate long-term variability in PMCs. (C) 2008 Elsevier Ltd. All rights reserved.
引用
收藏
页码:365 / 372
页数:8
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