Aerosol microphysics modules in the framework of the ECHAM5 climate model - intercomparison under stratospheric conditions

被引:42
作者
Kokkola, H. [1 ,2 ]
Hommel, R. [1 ,4 ]
Kazil, J. [1 ]
Niemeier, U. [1 ]
Partanen, A. -I. [1 ,3 ,5 ]
Feichter, J. [1 ]
Timmreck, C. [1 ]
机构
[1] Max Planck Inst Meteorol, Hamburg, Germany
[2] Finnish Meteorol Inst, Kuopio, Finland
[3] Tampere Univ Technol, FIN-33101 Tampere, Finland
[4] Univ Cambridge, Dept Chem, Ctr Atmospher Sci, Cambridge CB2 1EW, England
[5] Univ Kuopio, Dept Phys, FIN-70211 Kuopio, Finland
基金
芬兰科学院;
关键词
AQUEOUS SULFURIC-ACID; EXPERIMENTAL THERMODYNAMICS; CLOUD; SIMULATION; NUCLEATION; POLLUTION; H2SO4; SCALE; WATER; H2O;
D O I
10.5194/gmd-2-97-2009
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
In this manuscript, we present an intercomparison of three different aerosol microphysics modules that are implemented in the climate model ECHAM5. The comparison was done between the modal aerosol microphysics module M7, which is currently the default aerosol microphysical core in ECHAM5, and two sectional aerosol microphysics modules SALSA, and SAM2. The detailed aerosol microphysical model MAIA was used as a reference to evaluate the results of the aerosol microphysics modules with respect to sulphate aerosol. The ability of the modules to describe the development of the aerosol size distribution was tested in a zero dimensional framework. We evaluated the strengths and weaknesses of different approaches under different types of stratospheric conditions. Also, we present an improved method for the time integration in M7 and study how the setup of the modal aerosol modules affects the evolution of the aerosol size distribution. Intercomparison simulations were carried out with varying SO2 concentrations from background conditions to extreme values arising from stratospheric injections by large volcanic eruptions. Under background conditions, all microphysics modules were in good agreement describing the shape of the aerosol size distribution, but the scatter between the model results increased with increasing SO2 concentrations. In particular in the volcanic case the setups of the aerosol modules have to be adapted in order to dependably capture the evolution of the aerosol size distribution, and to perform in global model simulations. In summary, this intercomparison serves as a review of the different aerosol microphysics modules which are currently available for the climate model ECHAM5.
引用
收藏
页码:97 / 112
页数:16
相关论文
共 68 条
[1]  
[Anonymous], 2020, Gothenburg Protocol to reduce transboundary air pollution, DOI DOI 10.5860/CHOICE.44-4512
[2]  
[Anonymous], 2003, ATMOSPHERIC GEN CIRC
[3]  
[Anonymous], 2007, Climate Change 2007: The Scientific Basis
[4]  
[Anonymous], 1994, THESIS U CALIFORNIA
[5]  
[Anonymous], 1998, HIST PERSPECTIVES CL
[6]  
[Anonymous], 2005, FUNDAMENTALS ATMOSPH, DOI DOI 10.1017/CBO9781139165389
[7]   RELATIONSHIPS BETWEEN OPTICAL EXTINCTION, BACKSCATTER AND AEROSOL SURFACE AND VOLUME IN THE STRATOSPHERE FOLLOWING THE ERUPTION OF MT-PINATUBO [J].
BROCK, CA ;
JONSSON, HH ;
WILSON, JC ;
DYE, JE ;
BAUMGARDNER, D ;
BORRMANN, S ;
PITTS, MC ;
OSBORN, MT ;
DECOURSEY, RJ ;
WOODS, DC .
GEOPHYSICAL RESEARCH LETTERS, 1993, 20 (22) :2555-2558
[8]   VODE - A VARIABLE-COEFFICIENT ODE SOLVER [J].
BROWN, PN ;
BYRNE, GD ;
HINDMARSH, AC .
SIAM JOURNAL ON SCIENTIFIC AND STATISTICAL COMPUTING, 1989, 10 (05) :1038-1051
[9]   Uncertainty analysis for estimates of the first indirect aerosol effect [J].
Chen, Y ;
Penner, JE .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2005, 5 :2935-2948
[10]  
CHLOND A, 1994, MON WEATHER REV, V122, P111, DOI 10.1175/1520-0493(1994)122<0111:LMVOBA>2.0.CO