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The Law of Storms
The Law of Storms
The Law of Storms
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The Law of Storms

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"The Law of Storms" by John Ross
Ross was an explorer from Scotland. His experience traveling put him in a unique position to be able to discuss some of the most terrifying meteorological events: hurricanes. Using the, at the time, most up-to-date theories, he was able to discuss the patterns of hurricanes, including the typical weather that comes along with the storms and the paths these storms often take.
LanguageEnglish
PublisherGood Press
Release dateDec 18, 2019
ISBN4064066151515
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    Book preview

    The Law of Storms - John Ross

    John Ross

    The Law of Storms

    Published by Good Press, 2019

    goodpress@okpublishing.info

    EAN 4064066151515

    Table of Contents

    On Hurricanes or Cyclones.

    METEOROLOGICAL SIGNS RECOGNIZED BY THE FEELINGS.

    METEOROLOGICAL SIGNS RECOGNIZED BY THE EYE.

    METEOROLOGICAL SIGNS RECOGNIZED BY THE EAR.

    THE METEOROLOGICAL PHENOMENA ACCOMPANYING A REVOLVING STORM MAY ALSO BE ENUMERATED THUS

    INDICATIONS OF APPROACHING OR EXISTING HURRICANES, MANIFESTED BY THE OCEAN, OF ESPECIAL UTILITY TO VESSELS AT ANCHOR IN ROADSTEADS.

    RULES FOR TRIMMING THE SHIP IN A HURRICANE.

    ADMIRAL FITZROY’S INSTRUCTIONS ON THE USE OF THE BAROMETER IN NORTH LATITUDE.

    The Barometer Rises

    A Thermometer Falls

    A Thermometer Rises

    On Hurricanes or Cyclones.

    Table of Contents

    Thus, in both Hemispheres, the passage of an equatorial whirlwind storm on the west side of the place of observation produces normal revolutions in accordance with the law of gyration; while, on the other hand, its passage on the east side produces anomalous revolutions contrary to the law of gyration. When the vortex of a whirlwind storm passes over the place of observation, the vane may shift from one direction to that immediately opposite to it.

    Generally, if the whirlwind storm is an equatorial one in the Northern Hemisphere, it progresses from S.E. to N.W. in the Torrid Zone; it recurves at the outer edge of the N.E. trade wind, and thence moves from S.W. to N.E. But in the Southern Hemisphere an equatorial storm moves first from N.E. to S.W.; recurves at the outer edge of the S.E. trade wind, and

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