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Stratospheric Ozone Hole Chemistry: Processes and Reactions, Study notes of Meteorology

An in-depth analysis of the chemistry behind the formation of stratospheric ozone holes. It covers various topics such as heterogeneous reactions, denitrification, dehumidification, and the role of polar stratospheric clouds (pscs). The document also discusses the reaction probabilities on liquid/solid surfaces and the dominating ozone loss cycles for polar winter chemistry. Brasseur, orlando, and tyndall's book 'stratospheric ozone hole chemistry' is referenced throughout.

Typology: Study notes

Pre 2010

Uploaded on 02/13/2009

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Download Stratospheric Ozone Hole Chemistry: Processes and Reactions and more Study notes Meteorology in PDF only on Docsity! The “Ozone Hole” Total DU Plate 14; Evolution between 1979 and 1997 of the total ozone column abundance (March average) measured by the Total Ozone Mapping Spectrometer (TOMS) (Dobson Units). The figure highlights the substantial reduction in Arctic ozone during the 1990's (courtesy of P. Newman, NASA/Goddard Space Flight Center) Stratospheric ozone hole chemistry, | TT Preriorerepe gy mT TTT 7 T-4J S 1200 }- (a) 23 August | ~~ 3000 F (b) 16 September 7 a r 7 2 4 & a 4 2 ° <x re 7 S < g 600 g 2000 7 S 4 ° © 1 O O 1 0 1000 poten tis ty Ty 62 64 66 68 70 72 62 64 66 68 70 72 LATITUDE (°S) 2042:8,17:1/98:blm Figure 8.10. Measurements of highly enhanced CIO concentrations in the Antarctic Polar Vortex in 1987. The destruction of ozone during the period Aug. 23-Sept. 16 is evident, as is the anticorrelation of O3 and ClO concentrations (adapted with permission from Anderson, J. G., D. W. Toohey, and W. H. Brune (1991) Free radicals within the Antarctic vortex: The role of CFCs in Antarctic ozone loss, Science 251, 39, ©1991, American Association for the Advancement of Science). Stratospheric ozone hole chemistry, III • Heterogeneous (surface) reactions: – Surfaces: H2SO4 H2SO4-H2O-HNO3 mix PSCs – Incorporation of HNO3/H2O with time “Denitrification” Dehumidification ClONO2 liquid/solid particles HCl liquid/solid particles ClONO2 + HCl Cl2 + HNO3 ClONO2 + H2O HOCl + HNO3 HOCl + HCl Cl2 + H2O HOBr + HCl BrCl + H2O Polar Stratospheric Clouds (PSCs) SAT = Sulfuric acid tetrahydrate NAT = nitric acid trihydrate Finlayson-Pitts and Pitts, AP 2000 0.1 - <5 µm 1-10 cm-3 5 - 50 µm 10-3 - 10-2 cm-3 Finlayson-Pitts and Pitts, AP 2000 Reaction probabilities on liquid/solid surfaces • increase with decreasing T • faster on liquid (or ice) than solid SAT/NAT surfaces 35 30 25 20 15 Altitude (km) 10 FIGURE 12.17 Vertical O3 profile before (August 23) and after 12) development of the ozone Amundsen-Scott Station, South Pole, in 1993 (adapted from Hof- (October mann ef al., 1994a), Antarctic ozone hole extent, | * - Aug 23, 1993 Oct 12, 1993 POT 1 VW prretioirii tipi tiiig Po, (mPa) 5 10 15 20 hole at the 100 hPa Temperature Ozone layer temperature at Halley in 2005 - 2006 -30 -40 4 -50 -60 4 bi -70 4 -80 4 - Dally values ‘4-day mean Historic extreme gore ss Historic mean -100 I I I I i I Aug Sep Oct Nov Dec Jan Feb Mar Apr May Antarctic ozone hole extent, II EP/TOMS Version 8 Total Ozone for Sep 20, 2005 GSFC/613.3 py @ w a “s Oo WN oa 6 a Dobson Units O01 —- = = wp yan © a oa oqo s2z ose Oo bB B PB AB “NO MN G@ N a oao a aos Dark Gray < 100 and > 500 DU fotp mom oFoNG 2005 Southern Hemisphere Ozone Hole Area NOAA SBUV2 Current Year Compared Against Past 10 Years Million Sq Kin Updated through Dec 2, 2005 August September October November December oe 2005 — 2004 —— 2003 += 95-04 Mean — 95-04 Max —— 95-04 Min
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