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7.25 Global distribution of antipodes

As promised in Section 7.23, we will study antipodes. The antipode of a point at is the point at . We seek an answer to the question that has plagued so many for so long: Given the distribution of land and ocean, how often is the antipode of a point on land also on land? And what about marine antipodes? We use grdlandmask and grdmath to map these distributions and calculate the area of the Earth (in percent) that goes with each of the three possibilities. To make sense of our grdmath equations below, note that we first calculate a grid that is +1 when a point and its antipode is on land, -1 if both are in the ocean, and 0 elsewhere. We then seek to calculate the area distribution of dry antipodes by only pulling out the nodes that equal +1. As each point represent an area approximated by where the term's actual dimension depends on , we need to allow for that shrinkage, normalize our sum to that of the whole area of the Earth, and finally convert that ratio to percent. Since the , terms appear twice in these expressions they cancel out, leaving the somewhat intractable expressions below where the sum of for all is known to equal :

    #!/bin/sh
    #               GMT EXAMPLE 25
    #
    # Purpose:      Display distribution of antipode types
    # GMT progs:    gmtset, grdlandmask, grdmath, grd2xyz, gmtmath, grdimage, pscoast, pslegend
    # Unix progs:   cat
    #
    # Create D minutes global grid with -1 over oceans and +1 over land
    ps=example_25.ps
    D=30
    grdlandmask -Rg -I${D}m -Dc -A500 -N-1/1/1/1/1 -F -Gwetdry.grd
    # Manipulate so -1 means ocean/ocean antipode, +1 = land/land, and 0 elsewhere
    grdmath wetdry.grd DUP 180 ROTX FLIPUD ADD 2 DIV = key.grd
    # Calculate percentage area of each type of antipode match.
    grdmath -Rg -I${D}m -F Y COSD 60 $D DIV 360 MUL DUP MUL PI DIV DIV 100 MUL = scale.grd
    grdmath key.grd -1 EQ 0 NAN scale.grd MUL = tmp.grd
    grd2xyz tmp.grd -S -ZTLf > key.b
    ocean=`gmtmath -bi1s -Ca -S key.b SUM UPPER RINT =`
    grdmath key.grd 1 EQ 0 NAN scale.grd MUL = tmp.grd
    grd2xyz tmp.grd -S -ZTLf > key.b
    land=`gmtmath -bi1s -Ca -S key.b SUM UPPER RINT =`
    grdmath key.grd 0 EQ 0 NAN scale.grd MUL = tmp.grd
    grd2xyz tmp.grd -S -ZTLf > key.b
    mixed=`gmtmath -bi1s -Ca -S key.b SUM UPPER RINT =`
    # Generate corresponding color table
    cat << END > key.cpt
    -1.5    blue    -0.5    blue
    -0.5    gray    0.5     gray
    0.5     red     1.5     red
    END
    # Create the final plot and overlay coastlines
    gmtset ANNOT_FONT_SIZE_PRIMARY +10p PLOT_DEGREE_FORMAT dddF
    grdimage key.grd -Sn -JKs180/9i -B60/30:."Antipodal comparisons":WsNE -K -Ckey.cpt -Y1.2i \
            -U/-0.75i/-0.95i/"Example 25 in Cookbook" > $ps
    pscoast -R -J -O -K -Wthinnest -Dc -A500 >> $ps
    # Place an explanatory legend below
    pslegend -R0/9/0/0.5 -Jx1i/-1i -O -Dx4.5/0/6i/0.3i/TC -Y-0.2i -Fthick >> $ps << END
    N 3
    S 0.15i s 0.2i red  0.25p 0.3i Terrestrial Antipodes [$land %]
    S 0.15i s 0.2i blue 0.25p 0.3i Oceanic Antipodes [$ocean %]
    S 0.15i s 0.2i gray 0.25p 0.3i Mixed Antipodes [$mixed %]
    END
    rm -f *.grd key.* .gmt*

In the end we obtain a funny-looking map depicting the antipodal distribution as well as displaying in legend form the requested percentages (Figure 7.25). Note that the script is set to evaluate a global 30 minute grid for expediency (), hence several smaller land masses that do have terrestrial antipodes do not show up. If you want a more accurate map you can set the parameter to a smaller increment (try 5 and wait a few minutes).

The call to grdimage includes the -Sn to suspend interpolation and only return the value of the nearest neighbor. This option is particularly practical for plotting categorical data, like these, that should not be interpolated.

Figure 7.25: Global distribution of antipodes.

Next: 7.26 General vertical perspective Up: 7. Creating GMT Graphics Previous: 7.24 Data selection based Contents Index