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State of Vermont
Agency of Natural Resources
Department of Environmental Conservation
Agency Memorandum
To: Brian Fitzgerald
Thru: Paul Wishinski
From: Dan Riley
Subject: Addressing some uncertainties in our
acceptance of the pre-application modeling
Protocol for Southern Vermont Gas ^ Combined Cycle
Power plants.
Date: March 22, 1999
In the telephone memorandum from you to the A2
file dated March 3, 1999, regarding Southern
Vermont Gas, uncertainty exists concerning the
need for preconstruction monitoring of
meteorological data. This memorandum addresses
that question and offers additional advice
concerning new modeling guidance from the IWAQM
Phase 2 Summary Report for modeling long-range
transport impacts.
Addressing the first question, as you know, for
the ambient air quality standards in class II
domain we have typically waived the requirement
for onsite meteorological data. However, this
question must be evaluated with respect to
possible complex terrain impacts, and subsequent
need of a model such as CTDMPLUS, which does
require on-site measurements. Additionally, there
may be a dual purpose for on-site met.
Measurements in examination of impacts on the
Class I areas, but only if a refined analysis is
necessary. If the refined analysis were
necessary, other meteorological data fields, such
as from a prognostic model such as RAMS could also
be valuable for running the Calpuff modeling
system as outlined in the IWAQM Phase 2 Summary
Report. In either case, the primary benefit of
additional meteorological data would be definition
of the windfield and stability classification in
the deep, isolated valley the sources are proposed
to be sited. If on-site meteorology were
collected with the intent of dual usage,
measurement must occur at multiple vertical levels
to establish stability and wind profiles.
Since there may be no need for on-site meteorology
for a refined Class I impact analysis if the
proposed source passes the Calpuff screening
analysis, the applicant should perform this as a
first step. Some concern has arisen regarding
sufficient conservatism of the analysis. However,
as long as the source to receptor wind direction
is not the prevailing wind direction, as possibly
demonstrated with a wind rose, the screen analysis
should be conservative with respect to the refined
analysis, except for deposition impacts. CALPUFF
does not adequately account for the aqueous phase
oxidation of sulfur-dioxide to sulfate, which can
become dominant in the presence of fog or clouds.
For deposition impacts on Lye Brook it may be
advisable to use the IWAQM phase I procedures,
starting with the screening analysis, since it is
considerably more conservative than the phase II
analysis.
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