Abstract

Abstract. Plant functional type (PFT) distributions affect the results of biogenic emission modeling as well as O3 and particulate matter (PM) simulations using chemistry-transport models (CTMs). This paper analyzes the variations of both surface biogenic volatile organic compound (BVOC) emissions and O3 concentrations due to changes in the PFT distributions in the Seoul Metropolitan Areas, Korea. The Fifth-Generation NCAR/Pennsylvania State Meso-scale Model (MM5)/the Model of Emissions of Gases and Aerosols from Nature (MEGAN)/the Sparse Matrix Operator Kernel Emissions (SMOKE)/the Community Multiscale Air Quality (CMAQ) model simulations were implemented over the Seoul Metropolitan Areas in Korea to predict surface O3 concentrations for the period of 1 May to 31 June 2008. Starting from a performance check of CTM predictions, we consecutively assessed the effects of PFT area deviations on the MEGAN BVOC and CTM O3 predictions, and we further considered the basis of geospatial and statistical analyses. The three PFT data sets considered were (1) the Korean PFT, developed with Korea-specific vegetation database; (2) the CDP PFT, adopted from the community data portal (CDP) of US National Center for Atmospheric Research in the United States (NCAR); (3) MODIS PFT, reclassified from the NASA Terra and Aqua combined land cover products. Although the CMAQ performance check reveals that all of the three different PFT data sets are applicable choices for regulatory modeling practice, noticeable primary data (i.e., PFT and Leaf Area Index (LAI)) was observed to be missing in many geographic locations. Based on the assessed effect of such missing data on CMAQ O3 predictions, we found that this missing data can cause spatially increased bias in CMAQ O3. Thus, it must be resolved in the near future to obtain more accurate biogenic emission and chemistry transport modeling results. Comparisons of MEGAN biogenic emission results with the three different PFT data showed that broadleaf trees (BTs) are the most significant contributor, followed by needleleaf trees (NTs), shrub (SB), and herbaceous plants (HBs) to the total BVOCs. In addition, isoprene from BTs and terpene from NTs were recognized as significant primary and secondary BVOC species in terms of BVOC emissions distributions and O3-forming potentials in the study domain. A geographically weighted regression analysis with locally compensated ridge (LCR-GWR) with the different PFT data (δO3 vs. δPFTs) suggests that addition of BT, SB, and NT areas can contribute to O3 increase, whereas addition of an HB area contributes to O3 decrease in the domain. Assessment results of the simulated spatial and temporal changes of O3 distributions with the different PFT scenarios reveal that hourly and local impacts from the different PFT distributions on occasional inter-deviations of O3 are quite noticeable, reaching up to 13 ppb. The simulated maximum 1 h O3 inter-deviations between different PFT scenarios have an asymmetric diurnal distribution pattern (low in the early morning, rising during the day, peaking at 05:00 p.m., and decreasing during the night) in the study domain. Exponentially diverging hourly BVOC emissions and O3 concentrations with increasing ambient temperature suggest that the use of different PFT distribution data requires much caution when modeling (or forecasting) O3 air quality in complicated urban atmospheric conditions in terms of whether uncertainties in O3 prediction results are expected to be mild or severe.

Highlights

  • Biogenic volatile organic compounds (BVOCs) emitted from vegetated areas play an important role in the chemistry of the lower troposphere and atmospheric boundary layer via a series of oxidation reactions with OH and NO3 radicals and O3 (Finlayson-Pitts and Fitts, 2000; Atkinson and Arey, 2003)

  • From the subsequent investigation of the δBVOC emission distributions, we found that the patterns from biogenic emission distributions closely resembled those from the plant functional type (PFT) distributions in the study domain, except for the missing biogenic emission zones detected over the Seoul and Incheon Metropolitan Areas and some of their neighborhood areas (Fig. 5)

  • PFT area loss might be inevitable at this point in time, it must be resolved in the near future to obtain more accurate biogenic emission and chemistry transport modeling results

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Summary

Introduction

Biogenic volatile organic compounds (BVOCs) emitted from vegetated areas play an important role in the chemistry of the lower troposphere and atmospheric boundary layer via a series of oxidation reactions with OH and NO3 radicals and O3 (Finlayson-Pitts and Fitts, 2000; Atkinson and Arey, 2003). The BVOC emissions can reduce O3 concentrations in the areas with low levels of NOx because the reaction of O3 and BVOC reduces hydroxyl radicals and leads to decreased O3 formation (Finlayson-Pitts and Fitts, 2000; Hogrefe et al, 2011). The flux of biogenic emission is a strong function of vegetation area, biomass density, and other environmental factors (Guenther et al, 1995, 2006). In order to more efficiently prepare vegetation area information as an input to biogenic emission modeling, plant functional type (PFT) data have been used (Guenther et al, 2006; Pfister et al, 2008; Arneth et al, 2011). Careful consideration of PFT distributions is needed for the estimation of biogenic emissions and subsequent predictive work such as the O3 prediction with chemistry-transport model (CTM)

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