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Data: Visualization: Hurricane Data SetThe following data set has been made available to TeraGrid Visualization users. It is used in various examples and provided for users to make use of as they experiment with the visualization capabilities of the TeraGrid. It is stored in the Storage Resource Broker (SRB). For more information on accessing the SRB from TeraGrid, see the SRB web page. Hurricane Isabel, September 2003 WRF Model DataThe Weather Research and Forecasting (WRF) Model is developed by NCAR and its partners, and the simulation of Hurricane Isabel and data processing was performed by Wei Wang, Cindy Bruyere, and Bill Kuo of Mesoscale and Microscale Meteorology Division, NCAR, and the SCD visualization group. The Hurricane Isabel data can be found in the following directory in the Storage Resource Broker (SRB): /home/ux454089.teragrid/tgViz/DATA/HURRICANE_ISABEL This directory contains several datasets of compressed "bricks" of floats. Each file represents a single atmospheric variable for one timestep. The file naming convention is There is also a single 2D file ( File CompressionEach file is a compressed (gzip) brick of floats. Each file will expand to 100000000 bytes when uncompressed. The byte order is Big Endian. Variable Dimensions for Each File
The height data file ( Array OrderingThe data can be accessed as follows: fread((float *) data, TDIM*ZDIM*XDIM*YDIM*sizeof(float),1, fp); Where XDIM=YDIM=500, ZDIM=100, TDIM=1, and fp is a FILE pointer (fopen) to the input dataset. A single element that has an index of x,y,z, and t, is accessed as: data[x + y*XDIM + z*XDIM*YDIM + t*XDIM*YDIM*ZDIM]; Note: If you are reading a file with a single timestep, Data CoordinatesThe coordinates for the data are: x (Longitude) coordinate runs from 83 W to 62 W (approx) Missing ValuesLand values, where there is no valid atmospheric data, are designated with the value of 1.0e35. Variable Descriptions
Note: All of the "Q" variables represent moisture in the atmosphere in one form or another. For example, rain water differs from cloud water in terms of their particle sizes. Rain water has larger drop sizes so they can fall through the air, while cloud water has smaller drop sizes so they stay in the air. Rain water differs from snow and graupel in terms of their densities, and so does cloud water from cloud ice. |
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