earthquake density map/grid/info
Sheila Peacock <[email protected]>
| Newsgroups | gmane.comp.gis.gmt.user |
|---|---|
| Organization | AWE Blacknest |
| Message-ID | <[email protected]> |
Dear all, I have been trying to use GMT to reproduce a processing step from a 1986 report on global seismic magnitude measurements. The author, wishing to overcome the problem that earthquakes are not evenly distributed, divided the surface of the Earth into 400 tessera of equal area and extracted the largest three earthquakes from each for his analysis. I haven't been able to find his original program, so I thought I'd use GMT (v. 4.5.12 on CentOS5 Linux). I don't need my tessera to be identical to his because I'm using a different dataset, but I do need them to be of equal area. My input file consists of a list of earthquakes for which I have (ID-number, latitude, longitude, magnitude). I adopted the following sequence, first of all to find the number of earthquakes per grid cell (many cells are empty!). 1. mapproject (on to a Lambert Azimuthal polar projection); 2. xyz2grd with -An option to count number in each cell; 3. grdproject to return the co-ordinates to lat/long; 4. grd2xyz to get ASCII output. These four steps are carried out separately for northern and southern hemispheres. The purpose of the initial mapproject is to convert the lats/longs into Cartesian co-ordinates on a plane in which areas on the surface of the Earth translate into equal areas on the plane regardless of their latitude/longitude. This is necessary since xyz2grd assumes a rectangular grid. There are two problems: 1. I can use -An in xyz2grd to get the number of earthquakes per cell, or -Au to find the largest-magnitude earthquake in each cell, but I can't, for instance, find the largest three earthquakes in each cell, or find the ID number of the largest earthquake - unless I have missed something in xyz2grd that would allow me to store an array as the "z" value; 2. Plotting is, so far, a travesty, because grdimage plots each grid cell as a square or rectangle centred on the grid node, rather than fitting the grid into the circular Lambert projection. Getting a nice plot of my tessera on a global map (colour-coded to represent number-of-earthquakes) is of secondary importance to extracting the right earthquakes to feed to the program featured in the 1986 report, but I know it will become of primary importance once I get the program to produce some publishable results. Advice welcome. Regards, Sheila Peacock, Blacknest. To unsubscribe, send the message "signoff gmt-help" to [email protected]