[Illustration: _Part of scope showing typhoon by radar. Eye is above
center at right with spiral bands showing. Radar is located at center
of picture with surrounding clouds showing as dense white mass due to
heavy nearby echo return. Echo from opposite side of typhoon is faint._]
[Illustration: _Official U. S. Navy Photograph_
_Looking down into the eye of Hurricane Edna (foreground) on September
7, 1954._]
[Illustration: _U. S. Air Force Photo_
_Looking down at the central region of Typhoon Marge in 1951._]
[Illustration: _Weather officer in nose of aircraft talking to pilot
(left) and radar operator._]
[Illustration: _Official Photo U. S. A. F._
_The engineer in a B-29 on hurricane reconnaissance._]
_The two scanners ready to signal engine trouble the instant it shows
up._
[Illustration: _Official Defense Department Photograph_]
[Illustration: _Official Photo U. S. A. F._]
[Illustration: _The new plane (B-50) to be used by the Air Force for
hurricane reconnaissance._]
Some of the most dangerous of the extratropical storms begin as small
companions or secondary centers of huge disturbances, generally on the
south side, where they grow rapidly in fury and merge with the original
cyclones to produce winds of tremendous destructive power. This often
happens in the so-called “windy corners” of the world. One of these, and
a good example, is Cape Hatteras, on the eastern coast of North
Carolina. It is a sort of way station for both the tropical and
extratropical varieties. Hurricanes heading northwestward from the
Caribbean and curving to follow the coastline, sweep over the Cape,
which juts into the ocean at the point where the northward-moving storms
still retain great force. In winter, big extratropical cyclones passing
eastward across the region of the Great Lakes tend to produce small
companions or secondaries in the southeastern states and some of them
develop gales of hurricane force by the time they reach Hatteras. Here
the cold air masses of the continent, guided by storm winds, are thrown
against the warm, moist air from the Gulf Stream. In the reaction, there
are towering seas and hazardous gales that are well known to seamen.
Public-domain text, read in full here on John Shaqi.
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