Smithsonian Contributions to Knowledge, Volumen20 |
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Página xvi
The former may be regarded as the wind that would exist if the surface of the
earth were homogeneous , and the sun ever ... But the usual , and indeed the
only method of discussing observations of the winds , was to sum up the number
that ...
The former may be regarded as the wind that would exist if the surface of the
earth were homogeneous , and the sun ever ... But the usual , and indeed the
only method of discussing observations of the winds , was to sum up the number
that ...
Página 69
WINDS OF T II E GLOBE . ... Tuis zone having never been visited by man , direct
observations of its winds are wanting , and their character must necessarily be
very much a matter of ... Ratio of resultant to sum of winds .75 ( 69 ) ( No. 2. ) ...
WINDS OF T II E GLOBE . ... Tuis zone having never been visited by man , direct
observations of its winds are wanting , and their character must necessarily be
very much a matter of ... Ratio of resultant to sum of winds .75 ( 69 ) ( No. 2. ) ...
Página 70
... S. by E. 1. South 7 , S. by W. 3 , S. W. 10 , S. W. by W.1 , W.S. W.5 . West 3 , W.
by N. 2 , W.N. W. 3 , N. W. 3 , N. W. by N. 1 , calm 3 ; total 94 . Direction of
resultant S. 30 ° 7 ' E. Ratio of resultant to sum of winds .30 . Number of days 51 .
( No. 3. ) ...
... S. by E. 1. South 7 , S. by W. 3 , S. W. 10 , S. W. by W.1 , W.S. W.5 . West 3 , W.
by N. 2 , W.N. W. 3 , N. W. 3 , N. W. by N. 1 , calm 3 ; total 94 . Direction of
resultant S. 30 ° 7 ' E. Ratio of resultant to sum of winds .30 . Number of days 51 .
( No. 3. ) ...
Página 71
RELATIVE PREVALENCE OP WINDS FROM THE DIFFERENT POINT3 OP TI
COMPASS . Monsoon influences . Place of observation . Time of the ... Ratio of
Resultant to sum of winds . North . N. W. or beDirection , South . Number of days .
RELATIVE PREVALENCE OP WINDS FROM THE DIFFERENT POINT3 OP TI
COMPASS . Monsoon influences . Place of observation . Time of the ... Ratio of
Resultant to sum of winds . North . N. W. or beDirection , South . Number of days .
Página 72
At Port Foulke and Rensselaer Bay the estimated velocity of the wind was
indicated by a scale of numbers extending from 1 to 10 , as follows :Pressure in ...
Character of winds . per hour . per hour . 0 1 2 3 ... Ratio of Resultant to sum of
winds .
At Port Foulke and Rensselaer Bay the estimated velocity of the wind was
indicated by a scale of numbers extending from 1 to 10 , as follows :Pressure in ...
Character of winds . per hour . per hour . 0 1 2 3 ... Ratio of Resultant to sum of
winds .
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Términos y frases comunes
1869 inclusive Aggregate length aggregate period April May June Atlantic Ocean California Calm or variable Camp Central City clouds COMPASS Computed Continued Date December DIFFERENT POINTS Direction of resultant East England February March April Florida following places Force former Fort France giving Hill Illinois Iowa Island January February March John June July August kind of observations Latitude latter Long Maine Massachusetts mean direction Mexico Michigan miles per hour Missouri Monsoon influences months North Northeastern Northern November Number of days Observed as follows October November December Ohio Pacific Ocean Pennsylvania Place of observation Port Post Surgeon PREVALENCE OF WINDS Prof Ratio of resultant RELATIVE PREVALENCE resultant to sum Russia Saint Scotland seasons servations South Southern Spring Summer Autumn sum of winds Summer Autumn Winter Surface winds Switzerland Texas tween tween N Velocity in mean Virginia West Wisconsin York zone
Información bibliográfica
| Título | Smithsonian Contributions to Knowledge, Volumen20 Smithsonian Contributions to Knowledge, Smithsonian Institution |
| Autor | Smithsonian Institution |
| Editor | Smithsonian Institution, 1876 |
| Procedencia del original | Universidad de Minnesota |
| Digitalizado | 11 Jul. 2016 |
| Exportar cita | BiBTeX EndNote RefMan |