The Law of Storms Considered in Connection with the Ordinary Movements of the AtmosphereLongman, Green, Longman, Roberts, & Green, 1862 - 324 páginas |
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Página xi
... EARTH ON THE DIRECTION OF THE WIND I. THE PERMANENT WINDS . 1. THE UNDER TRADE - WIND 2. THE UPPER RETURN TRADE - WIND . II . THE YEARLY PERIODICAL WINDS . PAGE 3 7 18 36 1. THE MONSOONS OF THE EAST INDIES 43 • · THEIR CAUSE IS TO BE ...
... EARTH ON THE DIRECTION OF THE WIND I. THE PERMANENT WINDS . 1. THE UNDER TRADE - WIND 2. THE UPPER RETURN TRADE - WIND . II . THE YEARLY PERIODICAL WINDS . PAGE 3 7 18 36 1. THE MONSOONS OF THE EAST INDIES 43 • · THEIR CAUSE IS TO BE ...
Página 4
... they are three in number : 1. When the air flows from all sides towards one fixed point at which it rises , or flows away , INTRODUCTION . ORDINARY WINDS AND ROTATORY STORMS INFLUENCE OF THE ROTATION OF THE EARTH ON THE DIRECTION THE WIND.
... they are three in number : 1. When the air flows from all sides towards one fixed point at which it rises , or flows away , INTRODUCTION . ORDINARY WINDS AND ROTATORY STORMS INFLUENCE OF THE ROTATION OF THE EARTH ON THE DIRECTION THE WIND.
Página 5
... earth's surface to another , and consequently the indi- vidual particles move in parallel rectilinear paths . In the first case which we have just discussed , the paths are diverging and converging right lines , while in the second they ...
... earth's surface to another , and consequently the indi- vidual particles move in parallel rectilinear paths . In the first case which we have just discussed , the paths are diverging and converging right lines , while in the second they ...
Página 7
... earth's surface varies as the diameter of their lati- tude , and therefore increases from zero at the poles to a maximum at the equator . If the air be at rest , it partakes of the velocity of rotation of that portion of the globe over ...
... earth's surface varies as the diameter of their lati- tude , and therefore increases from zero at the poles to a maximum at the equator . If the air be at rest , it partakes of the velocity of rotation of that portion of the globe over ...
Página 8
... earth , inasmuch as the points on the earth's surface towards which it is moving have exactly the same velocity of rotation as those which it has left . If , on the other hand , the air be set in motion by any cause from the poles to ...
... earth , inasmuch as the points on the earth's surface towards which it is moving have exactly the same velocity of rotation as those which it has left . If , on the other hand , the air be set in motion by any cause from the poles to ...
Outras edições - Ver tudo
The Law of Storms Considered in Connection with the Ordinary Movements of ... Heinrich Wilhelm Dove,Robert Henry Scott Visualização integral - 1861 |
The Law of Storms: Considered in Connection with the Ordinary Movements of ... Heinrich Wilhelm Dove Visualização integral - 1862 |
The Law of Storms: Considered in Connection with the Ordinary Movements of ... Heinrich Wilhelm Dove Visualização integral - 1862 |
Palavras e frases frequentes
appears aqueous vapour Atlantic Ocean atmosphere August barometer falls barometer rises Bay of Bengal Berlin blow calm centre clouds coast cold commencement Crown 8vo cyclone December displacement district earth east easterly Edition equator equatorial current fact February fell following table gale height inches increase Indian Ocean Islands January JOHN TYNDALL July June Königsberg Kremsmünster latitude Law of Gyration maximum Meteorological miles minimum Monsoon months northerly current northern hemisphere November observations October opposite direction path phenomena polar current pressure prevalent R. A. PROCTOR rain rise rotatory motion September ship side snow southerly southern stations summer surface takes place temperate zone temperature theory thermometer tion torrid zone Trade Trade-wind Trade-wind zone Typhoons vane velocity of rotation violent vols weather westerly wind it ceases wind shifts winter Woodcuts وو
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