Estimating the effects of increased urbanization on surface meteorology and ozone concentrations in the New York City metropolitan region

被引:122
作者
Civerolo, Kevin [1 ]
Hogrefe, Christian
Lynn, Barry
Rosenthal, Joyce
Ku, Jia-Yeong
Solecki, William
Cox, Jennifer
Small, Christopher
Rosenzweig, Cynthia
Goldberg, Richard
Knowlton, Kim
Kinney, Patrick
机构
[1] New York State Dept Environm Conservat, Div Air Resources, Albany, NY USA
[2] SUNY Albany, Atmospher Sci Res Ctr, Albany, NY 12222 USA
[3] NASA, Goddard Inst Space Studies, New York, NY 10025 USA
[4] Columbia Univ, Earth Inst, Ctr Climate Syst Res, New York, NY USA
[5] Columbia Univ, Grad Sch Architecture Planning & Preservat, New York, NY USA
[6] CUNY Hunter Coll, Dept Geog, New York, NY 10021 USA
[7] Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY 10964 USA
[8] Columbia Univ, Mailman Sch Publ Hlth, New York, NY USA
基金
美国国家环境保护局;
关键词
models-3/CMAQ; MM5; air pollution meteorology; O-3; land use change;
D O I
10.1016/j.atmosenv.2006.10.076
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Land use and pollutant emission changes can have significant impacts on air quality, regional climate, and human health. Here we describe a modeling study aimed at quantifying the potential effects of extensive changes in urban land cover in the New York City (NYC), USA metropolitan region on surface meteorology and ozone (O-3) concentrations. The SLEUTH land-use change model was Used to extrapolate Urban land cover over this region from "present-day" (ca. 1990) conditions to a future year (ca. 2050), and these projections were subsequently integrated into meteorological and air quality simulations. The development of the fUture-year land-use scenario followed the narrative of the "AT' scenario described by the Intergovcrnmental Panel on Climate Change (IPCC), but was restricted to the greater NYC area. The modeling system consists of the Penn State/NCAR MM5 mesoscale meteorological model-, the Sparse Matrix Operator Kernal Emissions processing system; and the US EPA Community Multiscale Air Quality model, and simulations were performed for two 18-day episodes, one near-past and one future. Our results suggest that extensive urban growth in the NYC metropolitan area has the potential to increase afternoon near-surface temperatures by more than 0.6 degrees C and planetary boundary layer (PBL) heights by more than 150m, as well as decrease water vapor mixing ratio by more than 0.6 g kg(-1) across the NYC metropolitan area, with the areal extent of all of these changes generally coinciding with the area of increased urbanization. On the other hand, the impacts of these land use changes on ozone concentrations are more complex. Simulation results O-3 levels by about 1-5 ppb, and episode-maximum 8 h O-3 levels by more than 6 ppb across much of the NYC area. However, spatial patterns of ozone changes are heterogeneous and also indicate the presence of areas with decreasing ozone concentrations. When anthropogenic emissions were increased to be consistent with the extensive urbanization in the greater NYC area, the O-3 levels increased in outer counties of the metropolitan region but decreased in others, including coastal Connecticut and the Long Island Sound area. (c) 2006 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1803 / 1818
页数:16
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