You get an actual vapor pressure of @###.## millibars or @.#### $edewp $edewp1 inches of Mercury over water. . format VP3 = With an air temperature of @###.# degrees @<<<<<<<<<: $vp{airtemp} $vp{corf1}
You get a saturated vapor pressure of @###.## millibars or @.#### $etemp $etemp1 inches of Mercury over water. . format VP5 = With an air temperature of @###.# degrees @<<<<<<<<< and a dewpoint of $vp{airtemp} $vp{corf1} @###.# degrees @<<<<<<<<<: $vp{dewtemp} $vp{corf2}
You get a vapor pressure of @###.## millibars or @.#### inches of $edewp $edewp1 Mercury and a saturated vapor pressure of @###.## millibars or $etemp @.#### inches of Mercury all over water. You also get a relative $etemp1 humidity of @##.# percent. $rh . if ($vp{dewtemp} > $vp{airtemp}) { if ($temp =~ null) { } else { print "
The dewpoint temperature is greater than the air temperature, this only rarely occurs in the atmosphere. You may want to go back and double check your entries.
"; } }