A study of photochemical and physical processes affecting carbonyl compounds in the Arctic atmospheric boundary layer

被引:78
作者
Grannas, AM [1 ]
Shepson, PB
Guimbaud, C
Sumner, AL
Albert, M
Simpson, W
Dominé, F
Boudries, H
Bottenheim, J
Beine, HJ
Honrath, R
Zhou, XL
机构
[1] Purdue Univ, Dept Chem, W Lafayette, IN 47907 USA
[2] Purdue Univ, Dept Earth & Atmospher Sci, W Lafayette, IN 47907 USA
[3] USA, Cold Reg Res & Engn Lab, Corps Engineers, Hanover, NH 03755 USA
[4] Univ Alaska Fairbanks, Dept Chem, Fairbanks, AK USA
[5] CNRS, Lab Glaciol & Geophys Environm, Grenoble, France
[6] Meteorol Serv Canada, Toronto, ON, Canada
[7] CNR, Ist Inquinamento Atmosfer, Rome, Italy
[8] Michigan Technol Univ, Houghton, MI 49931 USA
[9] SUNY Albany, Wadsworth Ctr, NYSDOH, Albany, NY 12222 USA
[10] SUNY Albany, Sch Publ Hlth, Albany, NY USA
关键词
snow chemistry; Polar Sunrise Experiment 2000; formaldehyde; acetaldehyde; acetone;
D O I
10.1016/S1352-2310(02)00134-6
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Experiments were conducted during the ALERT 2000 field campaign aimed at understanding the role of air-snow interactions in carbonyl compound chemistry and the associated ozone depletion in the atmospheric boundary layer. Under sunlit conditions, we find that formaldehyde, acetaldehyde and acetone exhibit a significant diel cycle with average ambient air concentrations of 166, 53 and 385 ppt, respectively. A box model of Arctic surface layer chemistry was used to understand the diel behavior of carbonyl compound concentrations at Alert, Nunavut, Canada, with a focus on the chemical and physical processes that affect carbonyl compounds. Results of the study showed that the measured carbonyl compound concentrations can only be simulated when a radiation-dependent snowpack source term (possibly photochemistry) and a temperature-dependent sink (physical uptake on snow grains) of carbonyl compounds were added to the model. We are able to simulate the concentration and amplitude of the observed diel cycle, but not the phase of the cycle. These results help confirm the importance of snowpack chemistry and physical processes with respect to carbonyl compound concentrations in the Arctic surface boundary layer, and reveal weakness in the details of our understanding. (C) 2002 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:2733 / 2742
页数:10
相关论文
共 36 条
[1]   Processes and properties of snow-air transfer in the high Arctic with application to interstitial ozone at Alert, Canada [J].
Albert, MR ;
Grannas, AM ;
Bottenheim, J ;
Shepson, PB ;
Perron, FE .
ATMOSPHERIC ENVIRONMENT, 2002, 36 (15-16) :2779-2787
[2]   OZONE DESTRUCTION AND PHOTOCHEMICAL-REACTIONS AT POLAR SUNRISE IN THE LOWER ARCTIC ATMOSPHERE [J].
BARRIE, LA ;
BOTTENHEIM, JW ;
SCHNELL, RC ;
CRUTZEN, PJ ;
RASMUSSEN, RA .
NATURE, 1988, 334 (6178) :138-141
[3]   Snow-pile and chamber experiments during the Polar Sunrise Experiment 'Alert 2000':: exploration of nitrogen chemistry [J].
Beine, HJ ;
Dominé, F ;
Simpson, W ;
Honrath, RE ;
Sparapani, R ;
Zhou, XL ;
King, M .
ATMOSPHERIC ENVIRONMENT, 2002, 36 (15-16) :2707-2719
[4]   MEASUREMENTS OF NOY SPECIES AND O-3 AT 82-DEGREES-N LATITUDE [J].
BOTTENHEIM, JW ;
GALLANT, AG ;
BRICE, KA .
GEOPHYSICAL RESEARCH LETTERS, 1986, 13 (02) :113-116
[5]   Cl and Br atom concentrations during a surface boundary layer ozone depletion event in the Canadian high Arctic [J].
Boudries, H ;
Bottenheim, JW .
GEOPHYSICAL RESEARCH LETTERS, 2000, 27 (04) :517-520
[6]   Distribution and trends of oxygenated hydrocarbons in the high Arctic derived from measurements in the atmospheric boundary layer and interstitial snow air during the ALERT2000 field campaign [J].
Boudries, H ;
Bottenheim, JW ;
Guimbaud, C ;
Grannas, AM ;
Shepson, PB ;
Houdier, S ;
Perrier, S ;
Dominé, F .
ATMOSPHERIC ENVIRONMENT, 2002, 36 (15-16) :2573-2583
[7]  
BURKHART J, 2002, UNPUB ATMOSPHERIC EN
[8]   The role of Br2 and BrCl in surface ozone destruction at polar sunrise [J].
Foster, KL ;
Plastridge, RA ;
Bottenheim, JW ;
Shepson, PB ;
Finlayson-Pitts, BJ ;
Spicer, CW .
SCIENCE, 2001, 291 (5503) :471-474
[9]  
FUENTES JD, 1996, J ATMOS CHEM, V29, P1
[10]  
FUHRER K, 1996, CHEM EXCHANGE ATMOSP, V43, P307