Global terrestrial isoprene emission models: sensitivity to variability in climate and vegetation

被引:126
作者
Arneth, A. [1 ,2 ]
Schurgers, G. [1 ]
Lathiere, J. [3 ]
Duhl, T. [4 ]
Beerling, D. J. [5 ]
Hewitt, C. N. [6 ]
Martin, M. [1 ]
Guenther, A. [4 ]
机构
[1] Lund Univ, Lund, Sweden
[2] Inst Meteorol & Climate Res Atmospher Environm Re, Karlsruhe Inst Technol, Garmisch Partenkirchen, Germany
[3] CEA CNRS UVSQ, Lab Sci Climat & Environm LSCE IPSL, UMR8212, Gif Sur Yvette, France
[4] NCAR, Boulder, CO USA
[5] Univ Sheffield, Dept Anim & Plant Sci, Sheffield S10 2TN, S Yorkshire, England
[6] Univ Lancaster, Lancaster Environm Ctr, Lancaster LA1 4YQ, England
基金
瑞典研究理事会; 英国自然环境研究理事会;
关键词
VOLATILE ORGANIC-COMPOUNDS; ATMOSPHERIC CO2; NONMETHANE HYDROCARBONS; COMPOUND EMISSIONS; CARBON-DIOXIDE; ELEVATED CO2; LEAF-AREA; FOREST; IMPACT; RESOLUTION;
D O I
10.5194/acp-11-8037-2011
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Due to its effects on the atmospheric lifetime of methane, the burdens of tropospheric ozone and growth of secondary organic aerosol, isoprene is central among the biogenic compounds that need to be taken into account for assessment of anthropogenic air pollution-climate change interactions. Lack of process-understanding regarding leaf isoprene production as well as of suitable observations to constrain and evaluate regional or global simulation results add large uncertainties to past, present and future emissions estimates. Focusing on contemporary climate conditions, we compare three global isoprene models that differ in their representation of vegetation and isoprene emission algorithm. We specifically aim to investigate the between-and within model variation that is introduced by varying some of the models' main features, and to determine which spatial and/or temporal features are robust between models and different experimental set-ups. In their individual standard configurations, the models broadly agree with respect to the chief isoprene sources and emission seasonality, with maximum monthly emission rates around 20-25 Tg C, when averaged by 30-degree latitudinal bands. They also indicate relatively small (approximately 5 to 10% around the mean) interannual variability of total global emissions. The models are sensitive to changes in one or more of their main model components and drivers (e. g., underlying vegetation fields, climate input) which can yield increases or decreases in total annual emissions of cumulatively by more than 30 %. Varying drivers also strongly alters the seasonal emission pattern. The variable response needs to be interpreted in view of the vegetation emission capacities, as well as diverging absolute and regional distribution of light, radiation and temperature, but the direction of the simulated emission changes was not as uniform as anticipated. Our results highlight the need for modellers to evaluate their implementations of isoprene emission models carefully when performing simulations that use nonstandard emission model configurations.
引用
收藏
页码:8037 / 8052
页数:16
相关论文
共 78 条
[1]  
[Anonymous], 1990, PRINCIPLES ENV PHYS
[2]   Why are estimates of global terrestrial isoprene emissions so similar (and why is this not so for monoterpenes)? [J].
Arneth, A. ;
Monson, R. K. ;
Schurgers, G. ;
Niinemets, Ue. ;
Palmer, P. I. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2008, 8 (16) :4605-4620
[3]   Effects of species composition, land surface cover, CO2 concentration and climate on isoprene emissions from European forests [J].
Arneth, A. ;
Schurgers, G. ;
Hickler, T. ;
Miller, P. A. .
PLANT BIOLOGY, 2008, 10 (01) :150-162
[4]   Process-based estimates of terrestrial ecosystem isoprene emissions:: incorporating the effects of a direct CO2-isoprene interaction [J].
Arneth, A. ;
Niinemets, U. ;
Pressley, S. ;
Back, J. ;
Hari, P. ;
Karl, T. ;
Noe, S. ;
Prentice, I. C. ;
Serca, D. ;
Hickler, T. ;
Wolf, A. ;
Smith, B. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2007, 7 :31-53
[5]   From biota to chemistry and climate: towards a comprehensive description of trace gas exchange between the biosphere and atmosphere [J].
Arneth, A. ;
Sitch, S. ;
Bondeau, A. ;
Butterbach-Bahl, K. ;
Foster, P. ;
Gedney, N. ;
de Noblet-Ducoudre, N. ;
Prentice, I. C. ;
Sanderson, M. ;
Thonicke, K. ;
Wania, R. ;
Zaehle, S. .
BIOGEOSCIENCES, 2010, 7 (01) :121-149
[6]   CO2 inhibition of global terrestrial isoprene emissions:: Potential implications for atmospheric chemistry [J].
Arneth, Almut ;
Miller, Paul A. ;
Scholze, Marko ;
Hickler, Thomas ;
Schurgers, Guy ;
Smith, Benjamin ;
Prentice, I. Colin .
GEOPHYSICAL RESEARCH LETTERS, 2007, 34 (18)
[7]   Sensitivity of isoprene emissions estimated using MEGAN to the time resolution of input climate data [J].
Ashworth, K. ;
Wild, O. ;
Hewitt, C. N. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2010, 10 (03) :1193-1201
[8]   Atmospheric chemistry of VOCs and NOx [J].
Atkinson, R .
ATMOSPHERIC ENVIRONMENT, 2000, 34 (12-14) :2063-2101
[9]  
Barkley MP, 2008, J GEOPHYS RES-ATMOS, V113, DOI 10.1029/2008JD01576
[10]   Regulated large-scale annual shutdown of Amazonian isoprene emissions? [J].
Barkley, Michael P. ;
Palmer, Paul I. ;
De Smedt, Isabelle ;
Karl, Thomas ;
Guenther, Alex ;
Van Roozendael, Michel .
GEOPHYSICAL RESEARCH LETTERS, 2009, 36