Model analysis of trace gas measurements and pollution impact during INDOEX

被引:31
作者
de Laat, ATJ
de Gouw, JA
Lelieveld, J
Hansel, A
机构
[1] Univ Utrecht, Inst Marine & Atmospher Res, NL-3508 TC Utrecht, Netherlands
[2] Univ Innsbruck, Inst Ionenphys, A-6020 Innsbruck, Austria
关键词
D O I
10.1029/2000JD900821
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
An analysis of acetone (CH3COCH3) and acetonitrile (CH3CN) measurements, performed during the Indian Ocean Experiment (INDOEX), using a chemistry general circulation model is presented. A comparison with measurements indicates that the model simulates realistic CO and acetone distributions, except toward the Indian west coast near the surface. The latter may be related to a sea breeze circulation at the Indian west coast, which is not resolved by the model. A comparison of the measured and modeled correlation between CO and acetone indicates the presence of a background marine acetone source. A model sensitivity study suggests a global marine emission strength of 15-20 Tg acetone yr(-1), which is a significant contribution to the estimated global acetone source of 56 (37-80) Tg acetone yr(-1). The comparison of measured and modeled CO-acetonitrile correlation from surface measurements indicates that a model sink of acetonitrile in the marine boundary layer is missing. A model sensitivity study suggests that this could be dry deposition (deposition velocity estimate: 0.01-0.05 cm s(-1)) on the ocean surface. A comparison of measured and modeled tropospheric acetonitrile indicates that the model overestimates the free tropospheric acetonitrile mixing ratios up to a factor of 3, which points to a missing free tropospheric sink of acetonitrile in the model. A possible explanation may be stratospheric loss and subsequent stratosphere-troposphere exchange, which was not included in the model.
引用
收藏
页码:28469 / 28480
页数:12
相关论文
共 54 条
[31]   Biofuel consumption, deforestation, and farm level tree growing in rural India [J].
Mahapatra, AK ;
Mitchell, CP .
BIOMASS & BIOENERGY, 1999, 17 (04) :291-303
[32]  
OECKNER E, 1996, 218 M PLANCK I MET
[33]  
OLIVIER J, 1996, 771060 RIVM NAT I PU
[34]  
RANIER C, 1996, BIOMASS BURNING GLOB, P140
[35]   COMPUTATIONAL ASPECTS OF MOISTURE TRANSPORT IN GLOBAL-MODELS OF THE ATMOSPHERE [J].
RASCH, PJ ;
WILLIAMSON, DL .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 1990, 116 (495) :1071-1090
[36]  
ROELOFFS GJ, 1998, 283 M PLANC I MET
[37]   Model study of the influence of cross-tropopause O-3 transports on tropospheric O-3 levels [J].
Roelofs, GJ ;
Lelieveld, J .
TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY, 1997, 49 (01) :38-55
[38]   DISTRIBUTION AND BUDGET OF O-3 IN THE TROPOSPHERE CALCULATED WITH A CHEMISTRY GENERAL-CIRCULATION MODEL [J].
ROELOFS, GJ ;
LELIEVELD, J .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1995, 100 (D10) :20983-20998
[39]   Tropospheric ozone simulation with a chemistry-general circulation model: Influence of higher hydrocarbon chemistry [J].
Roelofs, GJ ;
Lelieveld, J .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2000, 105 (D18) :22697-22712
[40]   A three-dimensional chemistry general circulation model simulation of anthropogenically derived ozone in the troposphere and its radiative climate forcing [J].
Roelofs, GJ ;
Lelieveld, J ;
vanDorland, R .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1997, 102 (D19) :23389-23401