Unidata Summer Workshop - 2003IDV Lab F(updated to version 1.1) |
| Several, self-paced IDV labs are available. Each assumes different user backgrounds, addresses different problems, and highlights different IDV features. Please try the ones that seem most interesting. | |
Lab F Part a
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The IDV (Integrated Data Viewer) is Unidata's Java program that can run on any platform. Furthermore, there are several ways to start the application. Under Windows, Start the IDV by:
If using Sun Microsystem's Java Web Start program,
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The IDV uses multiple windows. Position them comfortably on your desktop.
The Unidata IDV contains a user's guide, which explains many IDV topics. Feel free to use it at any time.
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Displaying model data is a two step process. First, you select data; then, you create a display. I. Select model data.
Notice that the IDV retrieves data from remote servers. Thus, the IDV provides access to many data sources, and one is not limited by what is available locally. In the, Data Source Selector, window, note that data is available from several different NCEP models. In fact, data from the GFS model are available on several different grids; each covers a different geographic region. The CONUS grid covers the United States and surrounding areas, so it is the grid to use today. Each model is run several times each day, according to a set schedule. Each model run is identified by the day and starting hour, GMT (Greenwich Mean Time). It is initialized with observations available up to that time and makes forecasts by solving the laws of Physics. To see a list of available runs for a model, open the appropriate folder, by clicking on the key to the left of the folder icon.
The first model run, Latest, will link to the most recent run of the model. You will often want to look at the most recent model forecast, so, lets use it.
The, Data Source Selector, window will close; and you must return to the, Data Selector, window. In the, Data Selector, window the selected data source should be listed in the, Data Sources, pane. In the, Fields, pane you shuld see two folders: 2D grid and 3D grid, which contain two-dimensional and three-dimensional grids.
The next step is to select a quantity, by clicking on your choice.
The next step is to select forecast times, in the, Times, pane.
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II. Choose a display. One unique feature of the IDV is the availability of different display types. Choose one by clicking the display name, then click the, Create Display, button.
The display should appear soon in the, Unidata IDV, window, using a map appropriate to that data source. Only one forecast time is displayed at a time, however you can use the loop control buttons in the upper right hand corner of the, Unidata IDV, window to control an animation. Near the bottom of the, Unidata IDV, window is a legend bar for each display. To remove a display, if you made a mistake and want to start over, right click the middle of the legend bar, and choose, View --> Remove Display. To customize a display, right click the middle of the legend bar, and choose, Control Window. | |
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Next, you are going to overlay a similar forecast from the Eta model.
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To carefully compare forecasts, it is necesary to customize the map. The state boundaries need to be present and in an appropriate color.
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The data would be easier to visualize if the two sets of contours, one for each model, were in different colors. In addition, the 0 contour should be omitted, and the interval between contours should be larger. To customize a set of contours
To hide one set of contours in order to better see the other set.
To zoom and pan around the display: use the navigation buttons on the left edge of the, Unidata IDV, window. | |
A few questions to consider.
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Lab F Part b
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The IDV can take a snapshot of its current state, by creating a bundle file. This is done from the, Unidata IDV, window: choose the, File, menu; choose, Save As; choose a filename and directory; and click the, Save, button. This has many uses, one of which is to allow others to easily create the same display. If you did not follow the instructions for the first part of the lab, you can quickly catch up by opening a bundle file.
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Another way to compare the precipitation forecasts from two models is to actually subtract one model's values from the other, and display the resulting field. This is done by first creating a formula, and then defining the variables in the formula.
To create a formula to subtract two fields:
To choose data for a formula,
The ETA model forecasts do not extend as far into the future as those from the GFS model. As a result, the last few frames of the animation will have only the GFS precipitation forecast - there is no ETA precipitaton forecast nor a difference between the two models. | |
A few questions to reconsider.
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Lab F Part c
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Forecasters need to examine the change of temperature with height to determine the intensity of a precipitation event. Typically, vertical soundings of temperature, moisture, and horizontal wind are plotted on a special thermodynamic diagram, a skew-T. To prepare for this part of the lab:
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To display a forecast vertical sounding,
The display should appear soon in a new window, Sounding Data. No data will be plotted in the, Sounding Data, window if the sounding location is outside the Eta domain, which is a little bigger than North America. The location of the sounding is shown by a solid (colored) rectangle in the, Unidata IDV, window. To change the location of the sounding use the left mouse button and slowly drag the colored rectangle to a new location. As you do so, the sounding in the SkewT window should change. There will be one sounding shown, but you can loop through 10 soundings, one for each forecast time. Furthermore, you can coordinate the day/time of the sounding loop and the precipitation loop - in each display's control window, choose the, View, menu and then check the, Share, box. The SkewT display is too complex to fully describe here. For this lab, you need to know that the thick red curve shows the temperature at different pressure levels; temperature generally increases from left to right; and pressure increases top to bottom, as it does in the atmosphere. For more information please see the user's guide. To determine the intensity of rain events, it helps to compare the temperature of a rising surface parcel of air with the temperature of air at the same level.
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Can you find regions where the rain is likely to be steady? | |
Lab F Part d
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Although a sounding can tell a forecaster how the wind changes with height directly over head, it can not tell the forecaster where the jet stream is relative to a station: e.g., directly over head, to the north, or to the south. This is important because certain types of severe weather are more likely near the jet stream. Next, the jet stream will be displayed as an isosurface, or surface of constant wind speed. Furthermore, this display will be embedded as an interactive IDV display within an HTML document. To open an HTML document in the IDV's browser,
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A few questions to consider.
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