Cloudland: A Study on the Structure and Characters of CloudsE. Stanford, 1894 - 208 oldal |
Részletek a könyvből
1 - 5 találat összesen 25 találatból.
1. oldal
... ( usually about 1 per cent ) , a little carbonic acid and other gases , and lastly , a variable but im- portant amount of dust of various kinds . Now the most important of these constituents , as regards the subject of which we are going ...
... ( usually about 1 per cent ) , a little carbonic acid and other gases , and lastly , a variable but im- portant amount of dust of various kinds . Now the most important of these constituents , as regards the subject of which we are going ...
6. oldal
... usually but not happily tern tension of aqueous vapour . The proportion 66 the actual vapour - tension at any particula perature and the maximum vapour - tension at that temperature is called the " relative hun Hence the amount of ...
... usually but not happily tern tension of aqueous vapour . The proportion 66 the actual vapour - tension at any particula perature and the maximum vapour - tension at that temperature is called the " relative hun Hence the amount of ...
12. oldal
... usually be the case , and if the lower current contain water - vapour near its maximum COLDER CURRENT WARM MOIST CURRENT FIG . 2. - INTERFRET ACTION PRODUCING CLOUD . tension , it is evident that condensation will very likely take place ...
... usually be the case , and if the lower current contain water - vapour near its maximum COLDER CURRENT WARM MOIST CURRENT FIG . 2. - INTERFRET ACTION PRODUCING CLOUD . tension , it is evident that condensation will very likely take place ...
13. oldal
... once into ice . More usually , however , the vapour would first be condensed into water , and then , on decrease of temperature , this would be congealed into ice . Thus , if water - vapour , from any cause I 13 THE ATMOSPHERE.
... once into ice . More usually , however , the vapour would first be condensed into water , and then , on decrease of temperature , this would be congealed into ice . Thus , if water - vapour , from any cause I 13 THE ATMOSPHERE.
14. oldal
... usually presents a greater surface to the resistance of the air , also that in falling they meet with air of ever - increasing density , he will have no difficulty in understanding how clouds of this kind can exist for great lengths of ...
... usually presents a greater surface to the resistance of the air , also that in falling they meet with air of ever - increasing density , he will have no difficulty in understanding how clouds of this kind can exist for great lengths of ...
Más kiadások - Összes megtekintése
Cloudland; a Study on the Structure and Characters of Clouds William Clement Ley Nincs elérhető előnézet - 2013 |
Gyakori szavak és kifejezések
altitude anticyclones Anvil cloud appear Arabian Sea areas of high atmospheric circulation atmospheric pressure barometric pressure calm-belt cause Chart Cirro Cirro-filum Cirro-macula Cirrus cloud-forms clouds of Inclination clouds of Interfret clouds of Inversion colder condensation continent Cumuliform clouds Cumulo-nimbus Cumulo-rudimentum Cumulo-stratus Cumulus curve cyclonic disturbances deflected direction dust particles earth's surface effects elevation equator equatorial belt exist extensive formation forms of cloud frequently globe hail heat high pressure higher latitudes horizontal increase inversion movements isobaric land surfaces layers of air Lenticular cloud low pressure lower Mammatus monsoon motion mountain moving nearly Nebula Nimbus north-east northern hemisphere nubecules observer occurs oceanic surfaces poles poleward portion precipitation produced radiation rain regions rotation season seen shower cloud side snow southern sphere Stratus Maculosus Stratus Quietus summer summit takes place temperature thermal equator thunderstorms tion Trades tropical upper currents upward variety velocity vertical winds winter
Népszerű szakaszok
140. oldal - In whatever direction a body moves on the surface of the earth there is a force arising from the earth's rotation which deflects it to the right in the northern, but to the left in the southern hemisphere.
166. oldal - ... considerable. Hence the interior and most violent portion of a cyclone, always gyrating from right to left in the northern hemisphere, and the contrary in the southern, must always gradually move towards the pole of the hemisphere in which it is. While between the equator and the tropical calm belt, it is carried •westward by the general westward motion of the atmosphere there, but after passing the tropical calm belt, the general motion of the atmosphere carries it eastward, and hence the...
165. oldal - The motion of a cyclone toward the poles may be accounted for by the principle in § 5. The motion of the equatorial side of a cyclone in either hemisphere is always toward the east, and hence the deflecting force causes a pressure toward the equator, but that of the polar side being always toward the west, the deflecting force causes a pressure toward the pole. Now these deflecting forces being as the sine of the latitude, as may be seen from...
120. oldal - Cirrus moving from South is generally an indication of /Unsettled weather, especially in summer. The temperature is then usually above the mean for the time of year. " Cirrus from South-west indicates unsettled and sometimes stormy weather in winter. In summer it often precedes thunderstorms, but with a high barometric pressure and 'a high temperature it frequently has no disturbing influence, and is then usually replaced by Cirro macula.
120. oldal - Cirrux are held to be of service for forecasting purposes, the following rules by the author may be considered useful and instructive : — "Cirrus moving from North or North-east with a high barometer is a sign of settled weather in summer and of temporarily fine weather in winter. With a low barometer it is a sign of marked improvement in weather.
166. oldal - ... being greater on the polar side, where the deflecting forces which cause it are greatest, its action upon the atmosphere in advance of it is greater than on the equatorial side, where these forces are much less, and hence new portions of the atmosphere are being continually brought into action on the one side, while the resistance of the earth's surface, and the adjacent portions of atmosphere on the other side, are continually overcoming the comparatively weak forces there, and destroying the...
196. oldal - ... after the sea-breeze set in in the morning, which it did with wonderful regularity. The mountain stood in bold relief, and from where the ship lay its top could always be seen above the cloud, even when it was densest and blackest, with the lightning flashing and the thunder rolling as it did every day. I passed up through the cloud once, and I know therefore how heavily it rains, especially at the lower side of the cloud. This rain never extends beyond the base of the mountain, and all around...