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Local versus Non-local Influences of PM2.5

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Title: Local versus Non-local Influences of PM2.5


1
Local versus Non-local Influences of PM2.5
  • Background and Rationale
  • Influence of wind speed on local concentrations
  • Mid-Atlantic Rural Sites PM2.5 Vs Surface Wind
    Speed
  • Mid-Atlantic Urban Sites PM2.5 Vs Surface Wind
    Speed
  • Seasonal Urban-Rural Difference
  • Conclusions
  • Resource Links

Contact Bret Schichtel, Bret_at_mecf.wuslt.edu
2
Background and Rationale
  • At any given location the PM concentration is the
    result of the PM mass originating from non-local
    sources transported in and PM mass originating
    from local sources. What is local??
  • The local/non-local contributions depend on
    emissions, transport and aerosol formation and
    removal processes, so there is no typical
    non-local concentration.
  • Quantifying the local contributions identifies
    the part of the PM problem that can be controlled
    locally.

3
Influence of wind speed on local concentrations
  • The concentration C is equal to the sum of the
    background (Co) and local contribution (QL/UH)
  • Assuming a fixed source region length (L),
    emission rate (Q) and mixing height (H) as the
    wind speed (U) increases the concentration from
    the local sources decreases asymptotically
    approaching the background concentration.

4
PM2.5 Vs Surface Wind Speed at Urban and Rural
Sites
The PM2.5 at the urban sites during the cold
season (Nov - March) decline sharply (60) with
increasing wind speeds compared to the rural
sites (30). This implies the urban PM2.5 is
dominated by local sources.
5
Washington, DC Seasonal PM2.5 Urban Excess
  • The excess PM2.5 at Washington DC ranges from gt10
    mg/m3 (70) in the winter to 1-2 mg/m3 (10) in
    the summer.

6
Phoenix, AZ Seasonal PM2.5 Urban Excess
  • The Phoenix excess PM2.5 ranges from 11 - 16
    mg/m3 (80) in the winter to 3 mg/m3 (30) in
    the summer.

7
Conclusions
  • Mid-Atlantic and Southwest urban centers are
    dominated by local sources during the winter.
  • At the Mid-Atlantic urban sites, the summer
    local sources contribute about 10 of the PM mass
    compared to up to 70 in the winter.
  • At the urban Southwest, the local sources
    contribute about 30 of the summertime PM mass
    compared to about 80 in the winter.

8
Resource Links
  • Workbook Table of Contents
  • Comment and Feedback Page
  • Applications / Reports
  • Data sets used in the Applications
  • Methods and tools used in the Applications
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