Large nitric acid particles at the top of an Arctic stratospheric cloud -: art. no. 4517

被引:35
作者
Deshler, T [1 ]
Larsen, N
Weissner, C
Schreiner, J
Mauersberger, K
Cairo, F
Adriani, A
Di Donfrancesco, G
Ovarlez, J
Ovarlez, H
Blum, U
Fricke, KH
Dörnbrack, A
机构
[1] Univ Wyoming, Dept Atmospher Sci, Laramie, WY 82071 USA
[2] Danish Meteorol Inst, DK-2100 Copenhagen, Denmark
[3] Max Planck Inst Kernphys, Bereich Atmospharenphys, D-69029 Heidelberg, Germany
[4] CNR, Inst Atmospher Sci & Climate, I-00133 Rome, Italy
[5] Ctr Ric Energia Casaccia, Enter Nuove Tecnol Energia Ambiente, I-00196 Rome, Italy
[6] Ecole Polytech, IPSL, CNRS, Meteorol Dynam Lab, F-91128 Palaiseau, France
[7] Univ Bonn, Inst Phys, D-53115 Bonn, Germany
[8] Deutsch Zentrum Luft & Raumfahrt, Inst Phys Atmosphare, D-82230 Oberpfaffenhofen, Wessling, Germany
关键词
polar stratospheric clouds; in situ stratospheric cloud measurements; Arctic stratospheric clouds; polar stratospheric cloud composition; balloon-borne aerosol measurements; large polar stratospheric cloud particles;
D O I
10.1029/2003JD003479
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
[1] In early December 2001, balloon-borne in situ measurements of particle composition, size, number, phase, and backscatter were completed in an Arctic stratospheric cloud composed of three distinct layers between 22 and 26 km. Below 24.5 km, liquid solution droplets of water, nitric acid, and sulfuric acid and a thin ice layer were observed. Above this layer the particles were primarily solid nitric acid trihydrate. Just above 26 km, at cloud top, where temperatures were near or above the equilibrium temperature for nitric acid trihydrate, there was a thin layer of solid particles narrowly distributed around a radius of 2.0 mum at concentrations of < 0.001 cm(-3). Lidar backscatter and particle phase measurements approximately 200 km upwind of the in situ measurements indicate a similar vertical structure for the cloud. These in situ measurements represent, to our knowledge, the most comprehensive in situ observations of all phases of polar stratospheric cloud particles, while the large particles at cloud top have not been previously observed and may have implications for producing particles large enough to remove reactive nitrogen from the polar stratosphere.
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页数:9
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