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 5
... 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 are concentrical circles . The ...
... 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 are concentrical circles . The ...
Página 6
... consequently the velocity of rotation of the surface with which the air is in contact , be not constant , the vane can preserve its direction unchanged , solely on the condition that the interval between the extreme points of its course ...
... consequently the velocity of rotation of the surface with which the air is in contact , be not constant , the vane can preserve its direction unchanged , solely on the condition that the interval between the extreme points of its course ...
Página 12
... consequently a complete shift of the wind round the compass can never be ob- served . The deviation of the vane which is observed is proportional to the distance of the point of observation from the initial point of the current , and is ...
... consequently a complete shift of the wind round the compass can never be ob- served . The deviation of the vane which is observed is proportional to the distance of the point of observation from the initial point of the current , and is ...
Página 18
... consequently , instead of one heated point , we have a zone of maximum temperature on which the air is at rest . This zone separates the areas of the northern and southern currents of cold air , each of which is thus forced to perform ...
... consequently , instead of one heated point , we have a zone of maximum temperature on which the air is at rest . This zone separates the areas of the northern and southern currents of cold air , each of which is thus forced to perform ...
Página 24
... consequently much closer than it would appear to be if we were to neglect the Monsoons . In the same way the same causes affect the approach of the interior southern limit of the NE . Trade to the equator , inasmuch as that wind in the ...
... consequently much closer than it would appear to be if we were to neglect the Monsoons . In the same way the same causes affect the approach of the interior southern limit of the NE . Trade to the equator , inasmuch as that wind in the ...
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Términos y frases comunes
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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