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The Law of Storms
The Law of Storms
The Law of Storms
Ebook47 pages20 minutes

The Law of Storms

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DigiCat Publishing presents to you this special edition of "The Law of Storms" by John Ross. DigiCat Publishing considers every written word to be a legacy of humankind. Every DigiCat book has been carefully reproduced for republishing in a new modern format. The books are available in print, as well as ebooks. DigiCat hopes you will treat this work with the acknowledgment and passion it deserves as a classic of world literature.
LanguageEnglish
PublisherDigiCat
Release dateSep 16, 2022
ISBN8596547370451
The Law of Storms

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    Book preview

    The Law of Storms - John Ross

    John Ross

    The Law of Storms

    EAN 8596547370451

    DigiCat, 2022

    Contact: DigiCat@okpublishing.info

    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 then advances

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