Atmospheric Chemistry and Physics Global Isoprene Emissions Estimated Using Megan, Ecmwf Analyses and a Detailed Canopy Environment Model

The global emissions of isoprene are calculated at 0.5 resolution for each year between 1995 and 2006, based on the MEGAN (Model of Emissions of Gases and Aerosols from Nature) version 2 model (Guenther et al., 2006) and a detailed multi-layer canopy environment model for the cal- culation of leaf temperature and visible radiation fluxes. The calculation is driven by meteorological fields - air temper- ature, cloud cover, downward solar irradiance, windspeed, volumetric soil moisture in 4 soil layers - provided by anal- yses of the European Centre for Medium-Range Weather Forecasts (ECMWF). The estimated annual global isoprene emission ranges between 374 Tg (in 1996) and 449 Tg (in 1998 and 2005), for an average of ca. 410 Tg/year over the whole period, i.e. about 30% less than the standard MEGAN estimate (Guenther et al., 2006). This difference is due, to a large extent, to the impact of the soil moisture stress factor, which is found here to decrease the global emissions by more than 20%. In qualitative agreement with past studies, high annual emissions are found to be generally associated with El Ni˜ no events. The emission inventory is evaluated against flux measurement campaigns at Harvard forest (Massachus- sets) and Tapaj ´ os in Amazonia, showing that the model can capture quite well the short-term variability of emissions, but that it fails to reproduce the observed seasonal variation at the tropical rainforest site, with largely overestimated wet season fluxes. The comparison of the HCHO vertical columns calcu- lated by a chemistry and transport model (CTM) with HCHO

[1]  J. Goudriaan,et al.  Modelling Potential Crop Growth Processes: Textbook with Exercises , 1994 .

[2]  E. Schulze,et al.  Leaf nitrogen, photosynthesis, conductance and transpiration : scaling from leaves to canopies , 1995 .

[3]  A. Guenther,et al.  Eddy covariance measurement of isoprene fluxes , 1998 .

[4]  Sasha Madronich,et al.  The Role of Solar Radiation in Atmospheric Chemistry , 1999 .

[5]  Jean‐François Müller,et al.  Geographical distribution and seasonal variation of surface emissions and deposition velocities of atmospheric trace gases , 1992 .

[6]  Trissevgeni Stavrakou,et al.  Inversion of CO and NO x emissions using the adjoint of the IMAGES model , 2004 .

[7]  J. Kesselmeier,et al.  Seasonal differences in isoprene and light‐dependent monoterpene emission by Amazonian tree species , 2004 .

[8]  C. Jones,et al.  Effect of Climate Change on Isoprene Emissions and Surface Ozone Levels , 2003 .

[9]  L. Gatti,et al.  Seasonal cycles of isoprene concentrations in the Amazonian rainforest , 2004 .

[10]  Thomas P. Kurosu,et al.  Mapping isoprene emissions over North America using formaldehyde column observations from space , 2003 .

[11]  A. Dalcher,et al.  A Simple Biosphere Model (SIB) for Use within General Circulation Models , 1986 .

[12]  P. Crutzen,et al.  Development and Intercomparison of Condensed Isoprene Oxidation Mechanisms for Global Atmospheric Modeling , 2000 .

[13]  D. Jacob,et al.  Formaldehyde Distribution over North America: Implications for Satellite Retrievals of Formaldehyde Columns and Isoprene Emission , 2006 .

[14]  Thomas P. Kurosu,et al.  Satellite observations of formaldehyde over North America from GOME , 2000 .

[15]  P. Sellers Canopy reflectance, photosynthesis and transpiration , 1985 .

[16]  J. Lelieveld,et al.  Isoprene and monoterpene fluxes from Central Amazonian rainforest inferred from tower-based and airborne measurements, and implications on the atmospheric chemistry and the local carbon budget , 2007 .

[17]  Dorian S. Abbot,et al.  Seasonal and interannual variability of North American isoprene emissions as determined by formaldehyde column measurements from space , 2003 .

[18]  P. Palmer,et al.  Estimates of global terrestrial isoprene emissions using MEGAN (Model of Emissions of Gases and Aerosols from Nature) , 2006 .

[19]  Xubin Zeng,et al.  Global Vegetation Root Distribution for Land Modeling , 2001 .

[20]  Xingguo Mo,et al.  Evaluation of Reanalysis Soil Moisture Simulations Using Updated Chinese Soil Moisture Observations , 2005 .

[21]  Y. Malhi,et al.  Effect of elevated CO2 concentration and vapour pressure deficit on isoprene emission from leaves of Populus deltoides during drought. , 2004, Functional plant biology : FPB.

[22]  Louisa Emmons,et al.  Contribution of isoprene to chemical budgets: A model tracer study with the NCAR CTM MOZART-4 , 2008 .

[23]  P. Harley,et al.  Isoprene and monoterpene fluxes measured above Amazonian rainforest and their dependence on light and temperature , 2002 .

[24]  S. Solberg,et al.  Atmospheric Chemistry and Physics , 2002 .

[25]  A. Huete,et al.  Amazon rainforests green‐up with sunlight in dry season , 2006 .

[26]  J. Goudriaan,et al.  Modelling Potential Crop Growth Processes , 1994, Current Issues in Production Ecology.

[27]  S. Wofsy,et al.  Seasonal course of isoprene emissions from a midlatitude deciduous forest , 1998 .

[28]  K. Chance,et al.  Constraining global isoprene emissions with Global Ozone Monitoring Experiment (GOME) formaldehyde column measurements , 2005 .

[29]  D. Wuebbles,et al.  Sensitivity of global biogenic isoprenoid emissions to climate variability and atmospheric CO2 , 2004 .

[30]  Christine Wiedinmyer,et al.  Quantifying the Seasonal and Interannual Variability of North American Isoprene Emissions using Satellite Observations of Formaldehyde Column , 2005 .

[31]  F. Meixner,et al.  Coupling isoprene and monoterpene emissions from Amazonian tree species with physiological and environmental parameters using a neural network approach , 2005 .

[32]  D. Blake,et al.  The tropical forest and fire emissions experiment: Emission, chemistry, and transport of biogenic volatile organic compounds in the lower atmosphere over Amazonia , 2007 .

[33]  W. Rossow,et al.  ISCCP Cloud Data Products , 1991 .

[34]  Barbara Barletta,et al.  Space‐based formaldehyde measurements as constraints on volatile organic compound emissions in east and south Asia and implications for ozone , 2007 .

[35]  J. Burrows,et al.  Global observations of formaldehyde , 2004 .

[36]  C. N. Hewitt,et al.  A global model of natural volatile organic compound emissions , 1995 .

[37]  D Hauglustaine,et al.  The global atmospheric environment for the next generation. , 2006, Environmental science & technology.

[38]  J. Dudhia,et al.  Coupling an Advanced Land Surface–Hydrology Model with the Penn State–NCAR MM5 Modeling System. Part I: Model Implementation and Sensitivity , 2001 .

[39]  Eric A. Rosenberg,et al.  A Long-Term Hydrologically Based Dataset of Land Surface Fluxes and States for the Conterminous United States: Update and Extensions* , 2002 .

[40]  J. Randerson,et al.  Carbon emissions from fires in tropical and subtropical ecosystems , 2003 .

[41]  D. Hauglustaine,et al.  Impact of climate variability and land use changes on global biogenic volatile organic compound emissions , 2005 .

[42]  M. Andreae,et al.  Emission of trace gases and aerosols from biomass burning , 2001 .