Bulletin of the American Meteorological Society, Volúmenes6-7American Meteorological Society, 1925 |
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Página 14
... surface is uneven , especially where alternating slopes and depressions obtain , in which cases the lower ground should be avoided . The impor- tance of this matter has been emphasized by some recent records made by the Weather Bureau ...
... surface is uneven , especially where alternating slopes and depressions obtain , in which cases the lower ground should be avoided . The impor- tance of this matter has been emphasized by some recent records made by the Weather Bureau ...
Página 17
... Surfaces of discontinuity between fluid layers cause a very rapid dissipation of energy and are therefore unstable on account of the total differences of velocity and the resulting stresses being confined entirely to the surface forming ...
... Surfaces of discontinuity between fluid layers cause a very rapid dissipation of energy and are therefore unstable on account of the total differences of velocity and the resulting stresses being confined entirely to the surface forming ...
Página 18
... surface , or they may under exceptional conditions , depend- ing on their height and the supply of energy involved , reach the earth's surface and assist in forming a whirling storm such as a tornado , or perhaps even a tropical cyclone ...
... surface , or they may under exceptional conditions , depend- ing on their height and the supply of energy involved , reach the earth's surface and assist in forming a whirling storm such as a tornado , or perhaps even a tropical cyclone ...
Página 20
... surface water in mid - ocean to drift at an angle of forty - five degrees to the right ( in the northern hemisphere , left in the southern ) of the direction of the wind with reference to that drifting surface : and to cause each deeper ...
... surface water in mid - ocean to drift at an angle of forty - five degrees to the right ( in the northern hemisphere , left in the southern ) of the direction of the wind with reference to that drifting surface : and to cause each deeper ...
Página 21
... surface should be drawn along under it at a fixed speed and direction , that being the equivalent of a wind , the Ekman oceanographic equations could be applied directly to give the relation between surface winds and gradient winds ...
... surface should be drawn along under it at a fixed speed and direction , that being the equivalent of a wind , the Ekman oceanographic equations could be applied directly to give the relation between surface winds and gradient winds ...
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A. E. Douglass aerological Agriculture American Meteorological Society amount anemometer annual anticyclones April atmosphere Author's Abstract average balloon BULLETIN C. F. Brooks California cent Clark University climate Climatological clouds coast cold crop cyclones daily damage December Dinsmore Alter discussion feet fire weather Forest frost Greenland heat hour inches increase indicated instruments intensity interest isobars June Kansas kite lightning Marvin meeting Meisinger meteorographs miles Milham Monthly Weather Review months normal observations Observatory occur ocean October Office Pacific paper period periodogram precipitation present pressure Prof published radio rain rainfall records region relative humidity reports River season Secretary Service snow solar constant solar radiation southern stations storm summer surface temperature thunderstorms tion tornado trees tropical U. S. Weather Bureau United variations warm Washington weather forecasting weather map wind velocity winter Worcester