The cloud imaging and particle size experiment on the aeronomy of ice in the mesosphere mission: Cloud morphology for the northern 2007 season

被引:56
作者
Rusch, D. W. [1 ]
Thomas, G. E. [1 ]
McClintock, W. [1 ]
Merkel, A. W. [1 ]
Bailey, S. M. [2 ]
Russell, J. M., III [3 ]
Randall, C. E. [1 ]
Jeppesen, C. [1 ]
Callan, M. [1 ]
机构
[1] Univ Colorado, Atmospher & Space Phys Lab, Boulder, CO 80303 USA
[2] Virginia Polytech & State Univ, Bradley Dept Elect & Comp Engn, Blacksburg, VA 24061 USA
[3] Hampton Univ, Ctr Atmospher Sci, Hampton, VA 23668 USA
关键词
Polar mesospheric clouds; Mesosphere; Dynamics; Gravity waves; NOCTILUCENT CLOUDS; GRAVITY-WAVES;
D O I
10.1016/j.jastp.2008.11.005
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
The Aeronomy of Ice in the Mesosphere (AIM) mission was launched from Vandenberg Air Force Base in California at 4:26:03 EDT on April 25, 2007, becoming the first satellite mission dedicated to the study of noctilucent clouds (NLCs), also known as polar mesospheric clouds (PMC) when viewed from space. We present the first results from one of the three instruments on board the satellite, the Cloud Imaging and Particle Size (CIPS) instrument. CIPS has produced detailed morphology of the Northern 2007 PMC and Southern 2007/2008 seasons with 5 km horizontal spatial resolution. CIPS, with its very large angular field of view, images cloud structures at multiple scattering angles within a narrow spectral bandpass centered at 265 nm. Spatial coverage is 100% above about 70 degrees latitude, where camera views overlap from orbit to orbit, and terminates at about 82 degrees. Spatial coverage decreases to about 50% at the lowest latitudes where data are collected (35 degrees). Cloud structures have for the first time been mapped out over nearly the entire summertime polar region. These structures include 'ice rings', spatially small but bright clouds, and large regions ('ice-free regions') in the heart of the cloud season essentially devoid of ice particles. The ice rings bear a close resemblance to tropospheric convective outflow events, suggesting a point source of mesospheric convection. These rings (often circular arcs) are most likely Type IV NLC ('whirls' in the standard World Meteorological Organization (WMO) nomenclature). (C) 2008 Elsevier Ltd. All rights reserved.
引用
收藏
页码:356 / 364
页数:9
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