|Move your cursor over the station you want to download. Right-Click the mouse and a pop-up menu will appear. Select the Save Link As... menu option. A File Dialog Box will open up.|
|Change the directory to the one that contains your forecast profiles. Then click the Save button.|
18.104.22.168 Downloading profiles using Internet Explorer.
|Move your cursor over the station you want to download. Right-Click the mouse and a pop-up menu will appear. Select the Save Target As... menu option. A File Dialog Box will open up.|
|Change the directory to the one that contains your forecast profiles.
Note Internet Explorer will try to save the file as a Text Document.
This would be compatable with Bufkit except that is you clicked the Save
button now the file would be saved with a .txt extension appended to the
In this case, if you clicked the Save button now, the file would be saved as metakit.gsp.txt
|To overcome this limitation, just place quotes (i.e. the " character) around the file name. Now when you select the Save button, the profile will be saved under its correct name. In this case metakit.gsp|
22.214.171.124 Downloading profiles using BufGet. Downloading individual profiles can be tedious of you routinely retrieve a site. The problem is worse if you want to routinely retrieve several sites. The BufGet software package addresses these problems. You identify up to four lists of profiles that you may want to download. A list may contain profiles from several different NWS offices and combine HTTP and FTP transfers. The program with detailed instructions are available at http://www.erh.noaa.gov/er/buf/bufkit/bufget.html
4.0 Profile Mode. BUFKIT has two major display modes. The PROFILE display presents an analysis of a single hour of profile data. The OVERVIEW display presents a time line of parameters from the entire model run. BUFKIT starts in the Profile display mode.
4.1 Profile Selection
4.1.1 Selecting Model: On startup BUFKIT will search for etakit.xxx profiles in the eta profile directory specified in the BUFKIT.CFG file. By clicking on the Meso button BUFKIT will search for metakit.xxx profiles in the meso eta directory specified in the BUFKIT.CFG file. The NGM selection will scan for ngmkit.xxx files in your specified directory.
4.1. 2 Selecting Site: On selecting a model BUFKIT will display the station ID names of the etakit, metakit, or ngmkit files found in the respective data directory. BUFKIT will automatically select with the first profile found. To examine the data for another site, click on the site name with the mouse.
4.2 Time Selection: When a city is loaded it is set for forecast hour zero. To scan through the latter hours you can:
- Manual Control: On the HOUR vertical scroll bar, drag the control button or press the up/down arrow buttons. BUFKIT will display the hour of the mode run above the HOUR vertical scroll bar. You can click of the HOUR display to return to forecast hour 0.
- Automatic Looping: Click on the LOOP button. BUFKIT will enter a time lapse mode. You can change the looping speeds using controls displayed when selection the CONTROL panel display. The top scroll bar determines frame speed while the bottom slide bar determines the end of loop delay.
4.3 Thermodynamic Diagram Display. Bufkit will display the profile for a selected hour in the thermodynamic diagram display. You may adjust the scales as follows:
|Zoom in||Move the mouse over the Thermodynamic Diagram Display and Left-Click the mouse|
|Zoom Out||Move the mouse over the Thermodynamic Diagram Display and Right-Click the mouse|
|Adjust the Right Edge of the Display||Click on either the "<" (cooler) or the ">" (warmer) button at the bottom-right of the Thermodynamic Diagram Display|
|Adjust the left Edge of the Display||Click on either the "<" (cooler) or the ">" (warmer) button at the bottom-left of the Thermodynamic Diagram Display|
4.3.1 Active Readout Profile and Hodograph displays. When this option is selected under the Controls panel, moving the mouse over the profile will cause Bufkit to display height, temperature, dew point, and wind values for the nearest forecast layer on that display. If you have the Hodograph display open, the shear vector between the active level and the previous one is highlighted in purple. You can toggle between readout in feet, kilometers, or mb by clicking the button after Active Read Out option.
4.4 Profile Overlays: There are six categories of Profile Overlays: Controls, Alerts, Convection, Lake Effect, CONvective Research Animation Display, and Loop. Select a profile overlay category clicking on the appropriate overlay categoty box.
126.96.36.199 Vector Winds. Displays sigma level winds as a vector. The length of the vector is proportional to wind speed. The option button next to the Vector Wind Option will toggle the color of thge wind vectors based upon wind speed.
188.8.131.52 Digital Winds. Displays sigma level winds as "direction / speed" (knots).
184.108.40.206 Omega. Display the vertical velocity in microbars per second. Note the upward vertical velocity is negative. Depending how your configuration file is set, the values may have been filtered. When omega is selected a button appears next to this selection. Press the button to toggle between filtered and unfiltered views of omega.
220.127.116.11 10M Wind. Displays the 10 meter wind spped and direction on the profile.
18.104.22.168 Relative Humidity. When selected the program plots relative humidity on the left side of the sounding as follows:
|Red||>=70% to <90%|
22.214.171.124 Inversions. When checked will display inversions as gray shading with a label at the base of the inversion in millibars. If the Lake Effect Panel is displayed while inversions are selected, the Lake Effect Panel will also present lake effect snow radar coverage information. BUFKIT defines and inversion using one of two criteria:
126.96.36.199 Skew-T. When selected the temperate axis is similar to a Skew-T diagram. When not selected, the plot is similar to a pseudo-adiabatic chart.
188.8.131.52 Lines. When selected, the vertical axis tick marks (in feet, pressure or kilometers) are extended as lines across the profile display.
184.108.40.206 Clouds. The hourly model forecasts include the percent of cloud cover in the low, middle and high cloud decks. BUFKIT plots these cloud fractions to wherever relative humidity exceed 70% in the low levels (SFC-6000 ft), and 50% at middle (6000-20000 ft) and high (above 20000 ft) levels. The only exception is that a cloud deck is never plotted below the LCL. The intensity of the Gray scale is set by the sky cover fraction. So:
|Fractional Coverage||RGB Values||Color|
|0.00||00 00 00||Black|
|0.50||7F 7F 7F||Gray|
|1.00||FF FF FF||White|
220.127.116.11 Vertical Axis Units. Determine if BUFKIT plots the vertical axis using feet above ground level, kilometers above ground level, or pressure.
18.104.22.168 Icing Algorithm.
Example of Icing Profile between 21,000' and 35,000' (Blue curve [-8*DPD] greater than temperature curve)
|22.214.171.124 Momentium Transfer. This technique, developed at WFO Tauton and WFO Burlington, indicates the potential for upperlevel winds to mix down to the surface. The display is computed as follows: Starting at the surface, go up the temperature profile until the temperature decrease is no longer close to the dry adiabatic lapse rate. Bufkit highlights this portion of the temperature profile in light red and displays the wind speed and direction at that top level. Bufkit then computes the vector mean wind within that layer.||
4.4.2 Alerts Section. You can set the ALERT and ALARM levels of the thermodynamic indexes. To set Alert Levels:
4.4.3 Convection Section. This section displays theromodynamic calculations are based upon a lifting a parcel. The parcel is defined as having a mean-layer-averaged temperature and mositure from the lowest 500 meters of the atmosphere.
126.96.36.199 LFC/Equilibrium Level/LCL/CCL. When selected, BUFKIT will label and point an arrow to the vertical level in the sounding where is is occurring. If a parameter is not defined for a particular sounding, BUFKIT will not plot a label.
188.8.131.52 CAPE/CIN. When selected the CAPE will be plotted in yellow and CIN will be plotted in blue. CAPE and CIN will not be plotted of there is no LFC.
184.108.40.206 Convective Temperature. BUFKIT will plot the convective temperature in Celcius on the horizontal temperature scale near the surface.
220.127.116.11 Wet Bulb Zero. When selected, BUFKIT will plot the Wet Bulb Zero temperature in light blue on the vertical profile.
4.4.4 Lake Effect. This panel allows you to calculate several indices associated with lake effect snow.
18.104.22.168 Lake Index. This index is calculated by raisning the selected Lake temperature to 850 mb dry adiabatically and then subtracts the forecast sounding temperature at 850 mb from that "lifted parcel" temperature. Think of this like the Lifted Index except you lift the lake temperature and you only raise the parcel to 850 mb. Like the LI, when the index is negative, the parcel is warmer than the environment and you achieve lake-induced instability. The index display as on the profile in blue and white.
22.214.171.124 Moist Lake Index. Mixes the selected lake temperature with the lowest 2 layers of the model. It then raises modified parcel 150 mb above the surface moist adiabatically. BUFKIT then subtracts the forecast sounding temperature at 150 mb above the surface from that "modified lifted parcel" temperate. The index display as on the profile in green and white. Again, when this index is negative, the parcel is warmer than the environment and you achieve lake-induced instability. Which one to use? Moist Lake Index appears to forecast the start of Lake Effect Snow better than the Lake Index when there is high amounts of residual low-level moisture.
126.96.36.199 The Collier Index. This is a matrix that compares the Lake Temperature with the forecast temperature at 850 mb and 700 mb. Below the matrix BUFKIT will display a qualitative description of the extent of lake-induced instability: Conditional, Moderate, or Extreme.
188.8.131.52 Lake Induced Thermodynamic Parameters. BUFKIT displays Lake Induced CAPE (LIC), Lake Induced Equilibrium Level (LIE), and Normalized Lake Induced CAPE (NLIC). The parcel is lifted most adiabatically until the parcel temperature intercepts the environmental sounding. The starting parcel temperature is based on the lowest two model layers mixing with the operator selected lake temperature. The Lake Induced parameters are displayed on the Lake Effect panel while the Lake Induced CAPE is traced in white on the profile display.
In the "Ocean Effect" example above, the sounding is produced a LIC
of 382 J/kg, a LIE of only 4200 AGL, and a Normalized LIC of 0.3
m/s^2 (or 30 cm/s^2). This example contained an "Ocean Effect"
band that dropped 17 inches of snow in South Weymouth, MA.
4.4.5 CONRAD Section. This Convective Research Animation Display section
allows the user to apply the COMET module "A Convective Storm Matrix" to
the forecast sounding and hodograph.
|184.108.40.206 Storm Environment ID. For a given forecast hour, BUFKIT will analyze the hodograph and sounding profile and match it with one of 64 thunderstorm environments defined by this Module. If the required criteria of CAPE and hodograph shape are met, BUFKIT will display the appropriate storm environment ID in the black box. If you left click on this environment ID box, BUFKIT will display its rationale box plotting the shear and helicity for each 2.5 km layer up to 7.5 km AGL.||
|220.127.116.11 Storm Animations.. If an environment ID is present you can
play an animation of modeled thunderstorm model resulting from that environment.
To play the animation:
- the COMET module "A Convective Storm Matrix" CD-ROM is loaded in the CD-ROM drive or the module has been installed an accessible hard drive.
- The BUFKIT.CFG file has been configured to point to the drive where the COMET module is located. Just a drive letter and not a directory is required.
To play the radar animation, click on the 0.4 km and 4.0 km elevation display buttons. To display a visual depiction of the display, click on the CLOUD display button. Once the animation is started you can press to PAUSE/PLAY toggle button to stop and start the animation loop. The animation can be moved to the right or left side of the BUFKIT display by pressing the --> or <--- buttons. To end the animation display and restore the normal BUFKIT display, click on the CLEAR button.
4.4.6 Loop Paramenters. You can set the looping speed using these slider bars. This panel also provides the cability to print the profile display. However this capability only works with printers set to 300 dot-per-inch or less.
4.5 Profile Analysis Section. The region to the left of the profile displays five types of information associated with that hour's profile.
4.5.1 Data. BUFKIT will print the pressure, temperature, dew point, relative humidity, and wind velocity for each of the lowest 20 model layers.
- CAPE/CINS. The GEMPAK calculates these two values using the layer average of the lowest 100 mb of the sounding. This is similar to the method to calculate "B+"/"B-" values by SHARP when using the "Mean" parcel lifting technique. It can produce significantly different results when SHARP uses its default technique -- "PMAX" (Maximum instability in the lowest layers of the atmosphere).
- Helicity. This is calculated by the model post processor as follows: The layer-mean wind in the cloud bearing layer is estimated with the 850-300mb layer average wind. For wind speeds less than 15 m/s, the storm motion vector or estimated as 75% of the magnitude and 30 degrees to the right of this mean-layer wind. For wind speeds greater than 15 m/s the storm motion vector is estimated as 80% or the magnitude and 20 degrees to the right of the mean-layer wind. The storm relative helicity is then integrated for the 0 to 3 km AGL layer of the model atmosphere using the wind data from each layer. Note that this technique differs from the one used by SHARP to estimate storm relative Helicity.
- EHI. BUFKIT calculates the Energy Helicity Index by multiplying the CAPE by Helicity and then dividing by 160,000.
- BRN. The GEMPAK calculates the Bulk Richardson Number by dividing
CAPE by one-half the square of the difference between the mean wind over
the lowest 6 km of the model and the mean surface wind taken over the lowest
500 m of the model.
|- Normalized CAPE. Added to the Indices display is Normalized CAPE in units of meters per second squared. NCAPE is computed as CAPE / (EQL - LFC). It is based on the work published by David Blanchard at in Weather & Forecasting (Sep '98). In Blanchard's abstract he states: "NCAPE may provide a more useful indicator of buoyancy in environments in which the depth of free convection is shallow and total CAPE is small."||
- EQ LVL. GEMPAK calculated Equilibrium level in AGL feet. (All heights are displayed as AGL except the WSR-88D Hail Algorithm values on the overview screen.)
- WBZero. BUFKIT calculates Wet Bulb Zero in feet AGL.
- The following indices are calculated by GEMPAK.
- Pcpble Water. Precipitable water in inches.
- LCL, CCL, LFC, and Equilibrium Level are displayed in pressure and feet AGL.
4.5.3 Hodograph. This display allows the BUFKIT user to visually inspect and modify the model's hodograph. BUFKIT computes this helicity value using the same technique as implemented in SHARP. The layer-mean wind in the cloud bearing layer is estimated with the 0 - 6 km layer average wind. The storm motion is then estimated by deflecting this mean wind to the right by a user defined angle and a user defined percentage. BUFKIT allows the user to define two methods. The height over which the helicity is integrated is also user definable.
4.5.4 Storm Type. BUFKIT plots a large colored dot on this SHEAR vs CAPE diagram. The color of the dot is determined by CINS. Up to 5 previous SHEAR-CAPE-CINS values are also plotted in diminishing dot sizes. The shear calculations default using to 0 to 4 km, however, if enabled in the BUFKIT configuration file, the user can change over which layers the shear values are calculated.
4.5.5 Map. BUFKIT displays a map of an area defined by the configuration file. If the wind is coming from a direction defined in the BUFKIT.DAT, the map area will also display lake effect snow threat areas. Determining the steering winds of a lake effect snow band is one of the current meteorological challenges forecasters face today. Thus BUFKIT provided two methods to compute lake effect band steering winds.
18.104.22.168 Sigma Level Wind. When selected, the map display shows wind information for a given sigma level. It is the wind from this level that determine the position of any plotted lake effect snow regions. The program defaults to using a signal level closest to the pressure you specified in the BUFKIT.CFG configuration. You have the option of selecting other Sigma winds by clicking on the SIGMA LEVEL scroll bar that appears below to the map display box. A white horizontal line appears on the right hand side of the sounding profile at the specified sigma level. Shear is computed over a 100 mb layer centered on the selected sigma level. It is this calculated shear value that determines the color of the snow threat.
|Boundary Color||Shear Environment||Implication|
|Green||Low||single LES band|
|Yellow||Moderate||transition between single & multiple bands|
|Red||High||multiple LES bands|
|Red||Warm Air Advection at these levels|
|Blue||Cold Air Advection|
|Boundary Color||Shear Environment||Implication|
|Green||RMS Low||single LES band|
|Yellow||RMS Moderate||transition between single & multiple bands|
|Red||RMS High||multiple LES bands|
4.5.6 Precipitation Type Analysis. There are three different and independent precipitation Bufkit displays.
22.214.171.124 Model Output. The eta, NGM and RUC profiles contain
precipitation type. This output is displayed on the profile itself.
|126.96.36.199 Energy Area. BUFKIT now fully implements the AES
Canada precipitation type analysis developed by Pierre Bourgouin.
See "A Method to Determine Precipitation Type", Weather and Forecasting,
October 2000). Bufkit will present one of three displays depending
upon how many times the temperature profile crosses the zero degree isotherm.
You may access the alternative precipitation type technique by clicking on the Thickness button.
188.8.131.52 Partial Thickness. This technique, developed by Kermit Keeter and the forecasters at WFO Raleigh, forecast precipitation type based upon the 1000mb - 850 mb thickness (vertical axis) and the 850mb - 700 thickness (horizontal axis). By default, the last 6-hours of data is plotted, but this can be extended by clicking on the numbered-button at the bottom of this display. Click here for details on using this technique.
You may access the alternative precipitation type technique by clicking on the Energy button.
Example of the WFO Raleigh Precipitation Type Display
5.0 Overview Mode. Clicking on the overview button changes the display from a single hour to a time plot of all 49 sounding hours for the eta/ngm or 33 hours for the meso eta. The following display options are available in this overview mode.
5.1.1 Relative Humidity. When selected, the relative humidity for the entire model run is plotted. The color code is as follows:
|Red||>=70% to 90%|
5.1.3 Contour Internal. Sets the Interval for any selected contour products.
5.1.4 Reset Button. Clears all the selected products from display.
5.1.5 Height Section Buttons. Changes the vertical display to feet, kilometers, or pressure. The long button underneath the height selection buttons elevates the location where the vertical products are displayed. This is useful in viewing low level winds on the VAD product.
5.1.6 Vertical and Horizontal Axis. An overview parameter is plotted for a value (using the Vertical axis) over time (Horizontal axis). The last parameter plotted will usually activate a horizontal axis with a checked box is presented at the bottom of the screen below the vertical axis. When you have multiple vertical axis displayed, you can select any horizontal grid by clicking on one of these axis display boxes. To zoom in on a vertical axis, left click on the axis. To zoom out, right click on the appropriate vertical axis.
5.2 Contour Products. Bufkit can display 12 different time vs height contours.
Example of the Surface Delta Theta-E Contour for a Tornadic Event
Example of Air Force Weather's Icing Algorithm Time-Height Display
5.3 Temperature Products.
5.3.1 Inversions. Inversion heights are plotted as gray cross-hatched.
5.3.2 Lake Index. The computed Lake Index is plotted over all forecast hours. The line is plotted as red when the index implies lake-induced instability, yellow for a neutral low-level environment, and green to represents stable lake conditions.
5.3.3 Moist Lake Index. When Moist Lake Index 1, 2, or 3 is selected, BUFKIT will plot that index for all forecast hours. Like the Lake Index, the line is color coded to represent stability conditions. Red implies lake-induced instability, yellow implies a neutral low-level environment, and green implies stable lake conditions.
5.3.4. Two-meter temperature products. These two meter products are available on the eta and meso eta profiles. (The NGM plots up parameters from the lowest layer of the model instead).
5.4.1 Sigma Level Wind. When selected, a plot of the wind direction is presented for the controlling sigma level plus the wind direction 50 mb (approximately) above and 50 mb below the controlling sigma level. You can change the controlling sigma level by clicking on sigma level selection scroll bar.
5.4.2 Layer Mean Wind. When selected, a plot of the mean wind between two sigma levels. You can change either the base or top sigma level by clicking on sigma level selection scroll bar where the level number and pressure will be displayed. The color of the wind plot corresponds to the RMS of the wind in the specified layer as follows:
|Wind Color||Shear Environment||Implication|
|Green||RMS Low||single LES band|
|Yellow||RMS Moderate||transition between single & multiple bands|
|Red||RMS High||multiple LES bands|
|5.4.3 VWP. Wind vectors are presented for all forecast periods. The length of the vector is proportional to the wind speed. When enabled, you can display every third sigma wind (the default), every second sigma wind (2) or every wind (1). You can also display the 10 meter wind by clicking in the 10 meter selection button. When the color option is selected, the winds direction will be plotted in a color associated with its wind speed. Another effective display is the VWP with the wind speed contour overlayed.||
5.5.1 CAPE. The line is color coded by CINE.
|Red||Low||No significant cap|
5.5.2 Helicity. The Sharp Helicity value is plotted. Changes made on the hodograph panel on the profile display impact these values.
5.5.3 Total Totals.
5.5.4 Warm Cloud Depth. Not Implemented in this release.
5.5.5 Convective Instability. Shades levels where theta-e is decreasing with height
5.5.6 Storm Relative Inflow. Displays the difference between the mean surface to 2 km wind and the computed storm motion as presented on the hodograph display (see section 4.4.3)
5.5.7 WSR-88D Hail Data. Plots the 0 degree and -20 degree heights for that location as a function of time. A circle is plotted whenever the height changes by the threshold defined in the BUFKIT.CFG configuration file (i.e. 1000 ft). The number next to the circle in thousands of feet MSL. Note: this is the only MSL height depicted by Bufkit as the UCP algorithm entry screen requires MSL values.
In their 14 April 98 memo to the field, the OSF provided guidance on implementing changes to the WSR-88D Hail algorithm Probability of Severe Hail (POSH) offset. "Adjusting POSH Offset should be done whenever your site experiences a summertime environment characterized [by] a high melting level and a low vertical shear to alleviate an overforecasting bias. Wyatt and Witt (1997) defined a high melting level as > 4 km (or 13 kft) MSL and characterized low vertical shear as having winds at 500 mb < 30 kts. When these conditions occur, the POSH Offset should be lowered to 30%. When the summertime environment is no longer in effect, it is important that the POSH offset be reset to the default value of 50%." When selected, Bufkit plots a color coded bar at the top of the overview screen depicting whether the UCP parameter for POSH offset should be set to 50% or 30%.
5.6.1 Davis Stability Index. Computes the difference between the 2 meter temperature and 850 mb temperature. The line is color coded as follows:
5.6.4 Transport Wind. The mean wind speed and direction from the surface to the height of the maxing layer (see section 5.6.3)
5.6.5 Ventilation Factor. The Mixing Layer Height (in meters) multiplied by the Transport Wind Speed ( in meters per second).
5.7.1 Surface Pressure and 3 Hour Change. These are in millibars and used for isallobaric wind forecasting.
5.7.2 Evaporation and Runoff. Plotted in mm/hr. These values can be integrated over time using the right mouse button.
5.7.3 LLIW. For each level and hour, displays 10 log(Lifted Index * W)
5.7.4 Windex. The thick line is the conditional convective gust potential in knots. The thin line is Windex plus 50% of the forecast storm motion as computed using the technique described in section 4.4.3.
5.7.5 Clouds. A graphical display of the model's cloud cover output. BUFKIT plots the model's output of Low (SFC-6500), Mid (6500-20000) and High (above 20000) Fractional Cloud Coverage level that exceeds 70% RH for Low or 50% RH for Mid and High levels. Also, no clouds are plotted below the LCL. The box that is plotted is:
|Sky Fraction||Box Plotted||Implied|
|.00 - .09||none||Clear|
|.10 - .24||Single Cross Hatched||Few|
|.25 - .49||Double Cross Hatched||Scattered|
|.50 - .74||Gray||Broken|
|.75 - 1.00||White||Overcast|
5.8.1 Precipitation Integration. The right mouse button allows you to integrate precipitation over time. Move the mouse pointer into the data area at the starting time. Then click and hold down the right mouse button and drag the mouse left or right to another time. BUFKIT will plot a box near the cursor that show the sum of the precipitation from the starting time to the time where the mouse cursor is located.
5.8.2 Hourly Profile Display. Many of the Profile displays described in section 4 are also available on the overview screen. Move the mouse over the data area. Then click and hold down the left mouse button and one of the profile displays are overlayed on the overview screen. If you hold down the left mouse button and drag the mouse to the left or right (changing the valid time), the profile display will animate.
5.8.3 Now. When selected, BUFKIT will plot a vertical white bar on the time plot to indicate the current time.
5.8.4 Time. When selected BUFKIT will display a vertical grid associated with the time axis.
5.9.1 Defining a Metafunction Key. To define a metafunction key, first set up the Overview screen in the configuration you may commonly use. For example, you can display the lake index, VWP winds (in color), omega with a countor inverval of 2 microbars persecond, and then zoom the vertical axis into to see only up to 9000 ft as a metafunction. Then press one of the four save keys labeled "A" through "D". BUFKIT will then save a definition of that screen (made up of 96 different Overview parameters) to a file called BUFKIT.SV#, where the number # can be 0,1,2, or 3. BUFKIT will attempt to save these metafunction files on your local hard drive in the directory C:\WINDOWS\TEMP. If that directory doesn't exist then BUFKIT will save the metafunction files in same directory as the BUFKIT executable. The advantage of the first method is to support sites that have BUFKIT running off a single LAN directory. By saving the Metafunction definitions on a local drive and not the LAN drive, your Metafunctions will not be over written by someone else running BUFKIT on the LAN at the same time.
5.9.2 Using the Metafunctions. Once you have defined a Metafunction, you can invoke that definition anytime the overview screen is active by clicking on one of the four Metafunction recall buttons. A Metafunction can be applied against any site and any model run. If you have multiple instances of BUFKIT running at once, that Metafunction is available to each instance. All 96 parameters are recalled exactly as saved with the follow exception: the sigma winds and mean wind levels (see section 5.4) are defined by pressure values, not sigma levels. When a Metafunction is invoked, BUFKIT will find the sigma level closest in pressure to the Metafunction definition.
6.1 BUFKIT.MAP. This file contains the points to plot on the background map. The easiest way to create this file is using the MAPMAKER software. MAPMAKER is available from the NWSFO Buffalo anonymous FTP server. Once MAPMAKER creates BUFKIT.MAP, copy this BUFKIT.MAP file to the BUFKIT directory.
6.2 BUFKIT.CTY Plots locations on the background map with optional labels. Each line contains the latitude and longitude in decimal degrees, followed by an optional label. Entries are separated by commas.
Note in this example, the second location plots only the dot on the map without any label. Also note that, even in this case, the second comma is still required.
6.3 BUFKIT.DAT Defines the lake effect snow threat boxes. BUFKIT will support up to 10 series of threat boxes. Each series is make up of a wind direction followed by the four points that define the threat box for that wind direction. The points defined in latitude - longitude decimal degrees. The end of the series is defined with a -999.
|230||Beginning of Lake Erie Series|
|45.10, 83.00||This Box is for 230 degree winds|
|270||This Box is for winds at 270 degrees|
|-999||End of the Lake Erie series|
|240||This the start of the Lake Ontario series|
|42.53, 80.17||240 degree wind box|
|245||The 245 degree box|
|42.53, 80.17||Note that these wind box needs to be|
|43.73, 78.18||defined very carefully as a 245 Wind|
|43.40, 78.08||hits SYR while 240 misses SYR!|
|255||Start of 250 degree threat box|
|-999||End of second LES threat box|
=====> enter the latitude and longitude of each radar site
7.0 SHARP Soundings. (This feature is optional and requires that you have installed the BUFSHARP programs into the SHARP directory.) BUFKIT allows full integration of the eta and meso eta sounding data with SHARP. To convert a model sounding into SHARP format:
- Display the profile for the desired hour using the Hour vertical scroll bar.
- Ensure the lake temperature is appropriately set using the Lake Temperature vertical scroll bar.
- Click on the WSFO Buffalo logo in the upper-right corner of the BUFKIT display.
BUFKIT will convert the displayed profile to a file compatible with SHARP and then automatically load SHARP. After examining the data and exiting SHARP you will be returned to BUFKIT.
||LES Threat Maps
All-Around LES Guru
||Moist Lake Index|
||MODSND eta, meso eta, and NGM Scripts|
||Parcel Mixed Lake Index|
||Adaptable Lower Boundary Layered Winds|
||Omega Display Scheme
Bufkit "What If You Add" Guy
|Peggy Bruehl (COMET)||RUC II Profiles|
John Eise (MKE)
|Fire Weather Equations|
||Convective Animations from the Training
Module "A Convective Storm Matrix"