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 9
Heinrich Wilhelm Dove. that from B B as a north - east wind ; while that from A A , will reach it still more as an east wind . In this case an observer in the latitude DD , will see the vane gradually move from N. through NE . towards E ...
Heinrich Wilhelm Dove. that from B B as a north - east wind ; while that from A A , will reach it still more as an east wind . In this case an observer in the latitude DD , will see the vane gradually move from N. through NE . towards E ...
Página 10
... wind , will displace the polar current , which has become more or less easterly , in the direction E. , SE . , S .; in the southern hemisphere , as a north wind , it will displace the polar current , which has be- come easterly like the ...
... wind , will displace the polar current , which has become more or less easterly , in the direction E. , SE . , S .; in the southern hemisphere , as a north wind , it will displace the polar current , which has be- come easterly like the ...
Página 11
... wind from e e ,,, nearly as N .; that from ff more as NW .; and that from 9 9 nearly as W. A west wind , in either hemisphere , will interfere with fresh equatorial currents , and bring them to a state of relative rest . If the tendency ...
... wind from e e ,,, nearly as N .; that from ff more as NW .; and that from 9 9 nearly as W. A west wind , in either hemisphere , will interfere with fresh equatorial currents , and bring them to a state of relative rest . If the tendency ...
Página 12
... winds and the Monsoons may be considered as special cases of this law . In the torrid zone , the only atmospherical current which is felt at the surface of the ground is the polar current ; and consequently a complete shift of the wind ...
... winds and the Monsoons may be considered as special cases of this law . In the torrid zone , the only atmospherical current which is felt at the surface of the ground is the polar current ; and consequently a complete shift of the wind ...
Página 13
... wind enters the northern hemisphere as the SW . Monsoon during our summer , and the NE . Trade- wind enters the southern hemisphere as the NW . Mon- soon during our winter . The conversion of an equatorial into a polar current can only ...
... wind enters the northern hemisphere as the SW . Monsoon during our summer , and the NE . Trade- wind enters the southern hemisphere as the NW . Mon- soon during our winter . The conversion of an equatorial into a polar current can only ...
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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