| APL Weather
Historical APL weather observations are archived from June 13, 1996 to January 31, 2012. APL archived observations are available as:
APL Extreme Precipitation Statistics A table
of extreme precipitation statistics based on regional climatological studies performed at Cornell University is available for APL's location in Laurel, MD. The data in the table express extreme precipitation amounts corresponding to
"average return periods" for 15-minute, 30-minute, 1-hour, 2-hour, 3-hour, 6-hour, 12-hour, 18-hour, 24-hour, and 48-hour precipitation totals.
Click here to see this table.
The APL weather station closed on January 30, 2012. Listed below is a compilation of useful physical data about APL. Latitude and Longitude The point of reference for APL's geographical location is the original 1954 geodetic survey marker located within the ellipse in front of Building 1. This reference point was surveyed at:
Plant
Engineering can provide more specific latitude and longitude coordinates for other
locations within APL's borders if more detail is required.
In
our hemisphere, magnetic compasses point to the magnetic north pole, not the geographical
north pole or "true north." (The magnetic north pole is located in northern Canada
at about 73° N latitude, 100° W longitude. This location varies very slowly over
time.) Therefore, in the majority of locations in this hemisphere, the magnetic
variation or angular difference between magnetic and geographic north is nonzero.
For APL, the magnetic variation is approximately 10.5° west. This means that our
compass here points in a direction approximately 10.5° west of true north. Therefore,
true north is located about 10.5° east ("to the right") of where our compass points.
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