Generic Guidance and Optimum Model Settings for the CALPUFF ...

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2.4 Prognostic-Derived Surface (SURF.DAT) and Upper (UP.DAT) files In light of the other approaches mentioned above and especially the ease and flexibility of using 3-D gridded prognostic data that is readily available either from MM5, WRF, TAPM or other simulations, it is not recommended to use the prognostic models to generate single station surface and upper air meteorological files. In particular in Australasia, TAPM-derived surface and upper air station files are often used to drive CALMET. These ‘pseudo-profiles’ of surface and upper air data are used twice in CALMET (once to setup the initial guess phase and a second time in the Step 2 wind field) and carry the weight of real observations in CALMET. In most instances the TAPM or other prognostic data is best used as a 3-D input field in CALMET as the initial guess field rather than as pseudo-stations. The use of the full 3-D field allows all of the spatial variability in the prognostic model to be carried forward and used by CALMET and using the 3-D data as the initial guess field allows for smaller-scale terrain adjustments to be made by the CALMET diagnostic algorithms. Use of pseudo-stations involves the subjective choice of which “stations” to be selected from the prognostic gridded fields and only partially reproduces the spatially varying winds of the original prognostic fields. 2.5 Seven Critical CALMET Parameters When Using Observations When using CALMET with observational data, seven critical parameters must be carefully assessed and which are unique to every application. These values are; TERRAD, RMAX1, RMAX2, R1, R2, IEXTRP and BIAS. Table A-1 addresses each of these parameters individually. In developing the Step 1 wind field, CALMET adjusts the initial guess field to reflect the effects of the terrain, including slope flows and blocking effects. At this early stage the model accounts for the surface and upper air data in the initial guess phase and the user has the choice to use BIAS parameters to weight the effects of the wind field from an upper air station that may be located far away and not representative of the facility and site at all. Slope flows are a function of the local slope and altitude of the nearest crest. The crest is defined as the highest peak within a radius TERRAD (km) around each grid point. The value of TERRAD is determined based on an analysis of the characteristic length scale of the surrounding terrain. The Step 1 field produces a flow field consistent with the fine-scale CALMET terrain resolution. In Step 2, observations are incorporated into the Step 1 wind field to produce a final wind field. Each observation site influences the final wind field within a radius of influence (parameters RMAX1 (km) at the surface and RMAX2 (km) aloft). Observations and the Step 1 wind field are weighted by means of parameters R1 (km) at the surface and R2 (km) aloft. For example, at a distance R1 from an observation site, the Step 1 wind field and the surface observations are weighted equally. 12
Note that in no-observations (No-Obs) mode only one of the seven parameters is used (TERRAD), which simplifies the setup and operation of CALMET. Figure 2-1. Figure showing examples of how to choose RMAX1, R1, RMAX2 and R2 values. One value of RMAX1, RMAX2, R1 and R2 apply to all surface and upper air stations. RMAX1 and RMAX2 is typically the maximum radius of influence of the surface and upper air station, respectively. The approximate length (km) of RMAX1 and RMAX2 is shown in the figure as black solid lines. The blue circles represent approximate values (km) of R1 values representative of all surface stations. In complex terrain the R1 value is usually smaller than the RMAX value. The pink circle represents the R2 value of the upper air station for level 2 and aloft. 2.6 Other Important Parameters – Overwater Surface Fluxes and Mixing Heights The US Department of the Interior, Minerals Management Service (MMS) is responsible for the managing development of mineral resources including oil and gas on the Outer Continental Shelf (OCS) of the USA. In the early 1980s, the MMS sponsored the development of the Offshore and Coastal Dispersion (OCD) model (Hanna et al., 1985) to evaluate pollutants located over water. More recently MMS has sponsored a three-year study to enhance the capability of CALMET and CALPUFF for overwater transport and coastal interaction effects using the most current knowledge on meteorology and dispersion. An objective of the updated model is for use in both short-range and long-range applications. 13
Page 1 and 2: Generic Guidance and Optimum Model
Page 3 and 4: Contents SCOPE OF WORK AND BACKGROU
Page 5 and 6: LIST OF FIGURES Page Figure 2-1. Fi
Page 7 and 8: SCOPE OF WORK AND BACKGROUND A.1 In
Page 9 and 10: 1. INTRODUCTION The CALPUFF modelin
Page 11 and 12: 2.3 Methodologies for Running CALME
Page 13 and 14: hourly profiles of wind speed, wind
Page 15 and 16: Table 2-2. Model Option Switches fo
Page 17: 2.3.4 Single Station Meteorology It
Page 21 and 22: Table 2-3. Tabulated List of Variou
Page 23 and 24: 3 RECOMMENDED MODEL OPTION SETTINGS
Page 25 and 26: Ridge 1 distance (km) Ridge 2 Figur
Page 27 and 28: Boundary Layer (TIBL) over the land
Page 29 and 30: � algorithms were designed to tre
Page 31 and 32: Figure 3-3. Shows a cross-section o
Page 33 and 34: 3.5.2 Evaluation Studies Figure 3-6
Page 35 and 36: AERMOD BLP 60 70 80 90 95 98 99 Cum
Page 37 and 38: In CALPUFF, by default, a calm peri
Page 39 and 40: UTM Y Coordinate (km) - WGS84 6474.
Page 41 and 42: It is important to note that no eva
Page 43 and 44: 6474.5 6474 6473.5 6473 6472.5 6472
Page 45 and 46: sigma v (CALPUFF calculated) Figure
Page 47 and 48: 4. DISCUSSION ON THE APPROPRIATE PR
Page 49 and 50: 4.3.1 Graphical Evaluation Graphica
Page 51 and 52: (uncorrelated). A line of best fit,
Page 53 and 54: 4.3.3 Other Meteorological Evaluati
Page 55 and 56: Schulman, L.L. and J.S. Scire, 1980
Page 57 and 58: Table A-1. An Explanation of the 7
Page 59 and 60: Table A-1 An Explanation of the 7 C
Page 61 and 62: Table A-2 Explanation and Recommend
Page 67 and 68: Table A-4. Explanation and Recommen
Page 69:
Table A-4 Explanation and Recommend
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