Table of Contents - The Atmospheric Studies Group at TRC
Table of Contents - The Atmospheric Studies Group at TRC Table of Contents - The Atmospheric Studies Group at TRC
Section 9: CALPUFF Table 9-31 (Concluded) VOLEMARB.DAT - Time-Varying Data Record Contents (Next "NSRC" records) No. Variable Type a Description 1 CID C*16 Source identifier (must match values in time-invariant records) 2 XKM real X-coordinate (km) for source 3 YKM real Y-coordinate (km) for source 4 HTAGL real Effective height above ground (m) 5 ELMSL real Elevation of ground (m MSL) at source 6 SIGYI real Initial y (m) 7 SIGZI real Initial z (m) Next NSE QEMIT real array Emission rates (g/s) for each species in the order specified in Header Record 2 a C*16 = Character*16 9-196
Section 9: CALPUFF 9.7 Boundary Concentration Module File (BCON.DAT) The impact of significant regional pollution transport on concentrations and deposition fluxes computed within the modeling domain can be included in a CALPUFF analysis either by adding a spatially uniform (and either constant in time or varying by hour) field at the post-processing step with CALPOST, or by selecting the boundary concentration (BCON) module within CALPUFF. The latter choice is preferable if there are known spatial gradients in regional concentrations outside the modeling domain, or if chemical transformation and removal processes associated with the regional pollution must be explicitly modeled. Regional air-mass characteristics are defined and assigned to segments along each boundary of the computational domain when the boundary concentration module is used. A segment is equivalent to the length of one side of a grid cell. The number of air-mass types can be equal to the number of cells along the perimeter of the domain if sufficient information exists on this scale, or the number can be far fewer in typical applications where an entire side of the domain is characterized by a single air-mass. Air-mass characteristics include the concentration of each species advected into the domain and the thickness of the layer that contains these species. These concentrations are used to initialize puffs that are well-mixed in the vertical and the horizontal. The vertical depth of a puff is the thickness of the layer assigned to the air-mass, and the radius of the puff is related to the length of the segment and the component of the transport wind that is perpendicular to the segment (the mass flux into the domain and the initial concentration are conserved). The concentration of each species for each air-mass type may be scaled by factors that vary in one of the following ways: by hour of the day (24 factors); by month (12 factors); by hour and season (96 factors); by wind speed and stability class (36 factors); or by temperature (12 factors). These are the same factors provided for sources specified in the CALPUFF control file. If more detailed variation is needed for one or more air-mass types, air-mass characteristics for these can be provided hourly. When this method is used, the layer thickness may change as well as the concentrations. Otherwise, the layer thickness is constant for each air-mass type. The configuration of the boundary properties is provided to CALPUFF in a "BCON.DAT" file. Two formats are available for this file. The first is a formatted file prepared specifically for use with the BCON option (MBCON = 1). It is constructed using the CALPUFF control file conventions. A sample file is shown in Table 9-32, and a description of the input parameters is provided in Table 9-33. The second (MBCON = 2) is a standard CALPUFF unformatted “CONC.DAT” output concentration file. Receptors in this file must lie along the boundary of the modeling region, providing near-surface concentrations for the air mass transported across the boundary into the modeling domain. This format may be chosen if CALPUFF results from a larger domain are available. Input Group 1 in the BCON.DAT file identifies the grid information for the computational domain, the units for the concentrations that are provided, the number of air-mass types, and the type of temporal variation used in describing air-mass properties. Four air-mass types are used in this example. Three of these use the temporal variation factors provided in Input Group 3 and one uses an explicit sequence of 9-197
- Page 581 and 582: Section 9: CALPUFF Table 9-8 (conti
- Page 583 and 584: Section 9: CALPUFF table. A descrip
- Page 585 and 586: Section 9: CALPUFF Table 9-10: PLMM
- Page 587 and 588: Section 9: CALPUFF 9.2.4 SURFACE.DA
- Page 589 and 590: Section 9: CALPUFF Table 9-12: Samp
- Page 591 and 592: Section 9: CALPUFF Table 9-13 (cont
- Page 593 and 594: Section 9: CALPUFF Table 9-14: SURF
- Page 595 and 596: Section 9: CALPUFF Table 9-14 (conc
- Page 597 and 598: Section 9: CALPUFF Table 9-15 (cont
- Page 599 and 600: Section 9: CALPUFF 9.3 Point Source
- Page 601 and 602: Section 9: CALPUFF Table 9-17: PTEM
- Page 603 and 604: Section 9: CALPUFF Table 9-17 (Cont
- Page 605 and 606: Section 9: CALPUFF Table 9-18: PTEM
- Page 607 and 608: Section 9: CALPUFF Table 9-19: PTEM
- Page 609 and 610: Section 9: CALPUFF 9.4 Buoyant Area
- Page 611 and 612: Section 9: CALPUFF Table 9-21: BAEM
- Page 613 and 614: Section 9: CALPUFF . . . . . . . .
- Page 615 and 616: Section 9: CALPUFF Table 9-23 (Conc
- Page 617 and 618: Section 9: CALPUFF Table 9-24: Samp
- Page 619 and 620: Section 9: CALPUFF NCOMM+8 or 9 IEJ
- Page 621 and 622: Section 9: CALPUFF Table 9-26: LNEM
- Page 623 and 624: Section 9: CALPUFF a C*16 = Charact
- Page 625 and 626: Section 9: CALPUFF Table 9-28: Samp
- Page 627 and 628: Section 9: CALPUFF NCOMM+8 or 9 IEJ
- Page 629 and 630: Section 9: CALPUFF * "NSE" elements
- Page 631: Section 9: CALPUFF 9-195
- Page 635 and 636: Section 9: CALPUFF Table 9-32: Boun
- Page 637 and 638: Section 9: CALPUFF Table 9-32 (Cont
- Page 639 and 640: Section 9: CALPUFF Table 9-32 (Cont
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- Page 643 and 644: Section 9: CALPUFF Table 9-32 (Conc
- Page 645 and 646: Section 9: CALPUFF Table 9-33 (Cont
- Page 647 and 648: Section 9: CALPUFF Table 9-33 (Conc
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- Page 655 and 656: Section 9: CALPUFF The model checks
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- Page 659 and 660: Section 9: CALPUFF Table 9-40: Samp
- Page 661 and 662: Section 9: CALPUFF Table 9-41 (Cont
- Page 663 and 664: Section 9: CALPUFF Table 9-43: HILL
- Page 665 and 666: Section 9: CALPUFF Table 9-44: Samp
- Page 667 and 668: Section 9: CALPUFF where the follow
- Page 669 and 670: Section 9: CALPUFF 9.14 Mass Flux B
- Page 671 and 672: Section 9: CALPUFF Table 9-49: FLUX
- Page 673 and 674: Section 9: CALPUFF 9.15 CALPUFF Out
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- Page 677 and 678: Section 9: CALPUFF Table 9-52 (Cont
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Section 9: CALPUFF<br />
9.7 Boundary Concentr<strong>at</strong>ion Module File (BCON.DAT)<br />
<strong>The</strong> impact <strong>of</strong> significant regional pollution transport on concentr<strong>at</strong>ions and deposition fluxes computed<br />
within the modeling domain can be included in a CALPUFF analysis either by adding a sp<strong>at</strong>ially uniform<br />
(and either constant in time or varying by hour) field <strong>at</strong> the post-processing step with CALPOST, or by<br />
selecting the boundary concentr<strong>at</strong>ion (BCON) module within CALPUFF. <strong>The</strong> l<strong>at</strong>ter choice is preferable<br />
if there are known sp<strong>at</strong>ial gradients in regional concentr<strong>at</strong>ions outside the modeling domain, or if<br />
chemical transform<strong>at</strong>ion and removal processes associ<strong>at</strong>ed with the regional pollution must be explicitly<br />
modeled.<br />
Regional air-mass characteristics are defined and assigned to segments along each boundary <strong>of</strong> the<br />
comput<strong>at</strong>ional domain when the boundary concentr<strong>at</strong>ion module is used. A segment is equivalent to the<br />
length <strong>of</strong> one side <strong>of</strong> a grid cell. <strong>The</strong> number <strong>of</strong> air-mass types can be equal to the number <strong>of</strong> cells along<br />
the perimeter <strong>of</strong> the domain if sufficient inform<strong>at</strong>ion exists on this scale, or the number can be far fewer in<br />
typical applic<strong>at</strong>ions where an entire side <strong>of</strong> the domain is characterized by a single air-mass. Air-mass<br />
characteristics include the concentr<strong>at</strong>ion <strong>of</strong> each species advected into the domain and the thickness <strong>of</strong> the<br />
layer th<strong>at</strong> contains these species. <strong>The</strong>se concentr<strong>at</strong>ions are used to initialize puffs th<strong>at</strong> are well-mixed in<br />
the vertical and the horizontal. <strong>The</strong> vertical depth <strong>of</strong> a puff is the thickness <strong>of</strong> the layer assigned to the<br />
air-mass, and the radius <strong>of</strong> the puff is rel<strong>at</strong>ed to the length <strong>of</strong> the segment and the component <strong>of</strong> the<br />
transport wind th<strong>at</strong> is perpendicular to the segment (the mass flux into the domain and the initial<br />
concentr<strong>at</strong>ion are conserved). <strong>The</strong> concentr<strong>at</strong>ion <strong>of</strong> each species for each air-mass type may be scaled by<br />
factors th<strong>at</strong> vary in one <strong>of</strong> the following ways: by hour <strong>of</strong> the day (24 factors); by month (12 factors); by<br />
hour and season (96 factors); by wind speed and stability class (36 factors); or by temper<strong>at</strong>ure (12<br />
factors). <strong>The</strong>se are the same factors provided for sources specified in the CALPUFF control file. If more<br />
detailed vari<strong>at</strong>ion is needed for one or more air-mass types, air-mass characteristics for these can be<br />
provided hourly. When this method is used, the layer thickness may change as well as the concentr<strong>at</strong>ions.<br />
Otherwise, the layer thickness is constant for each air-mass type.<br />
<strong>The</strong> configur<strong>at</strong>ion <strong>of</strong> the boundary properties is provided to CALPUFF in a "BCON.DAT" file. Two<br />
form<strong>at</strong>s are available for this file. <strong>The</strong> first is a form<strong>at</strong>ted file prepared specifically for use with the<br />
BCON option (MBCON = 1). It is constructed using the CALPUFF control file conventions. A sample<br />
file is shown in <strong>Table</strong> 9-32, and a description <strong>of</strong> the input parameters is provided in <strong>Table</strong> 9-33. <strong>The</strong><br />
second (MBCON = 2) is a standard CALPUFF unform<strong>at</strong>ted “CONC.DAT” output concentr<strong>at</strong>ion file.<br />
Receptors in this file must lie along the boundary <strong>of</strong> the modeling region, providing near-surface<br />
concentr<strong>at</strong>ions for the air mass transported across the boundary into the modeling domain. This form<strong>at</strong><br />
may be chosen if CALPUFF results from a larger domain are available.<br />
Input <strong>Group</strong> 1 in the BCON.DAT file identifies the grid inform<strong>at</strong>ion for the comput<strong>at</strong>ional domain, the<br />
units for the concentr<strong>at</strong>ions th<strong>at</strong> are provided, the number <strong>of</strong> air-mass types, and the type <strong>of</strong> temporal<br />
vari<strong>at</strong>ion used in describing air-mass properties. Four air-mass types are used in this example. Three <strong>of</strong><br />
these use the temporal vari<strong>at</strong>ion factors provided in Input <strong>Group</strong> 3 and one uses an explicit sequence <strong>of</strong><br />
9-197