Climate and Time in Their Geological Relations: A Theory of Secular Changes of the Earth's ClimateAppleton, 1890 - 577 páginas |
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Página viii
... Temperature . - Reason of the Low Summer Temperature of Polar Regions . - Deflection of Ocean - currents the chief ... Difference of Specific Gravity . - Difference of Specific Gravity resulting from Dif- ference of Temperature ...
... Temperature . - Reason of the Low Summer Temperature of Polar Regions . - Deflection of Ocean - currents the chief ... Difference of Specific Gravity . - Difference of Specific Gravity resulting from Dif- ference of Temperature ...
Página ix
... Difference of Specific Gravity . - Sir John Herschel's Estimate of the Force.- Maximum Density of Sea - Water . - Rate of Decrease of Temperature of Ocean at Equator . - The actual Amount of Force resulting from Difference of Specific ...
... Difference of Specific Gravity . - Sir John Herschel's Estimate of the Force.- Maximum Density of Sea - Water . - Rate of Decrease of Temperature of Ocean at Equator . - The actual Amount of Force resulting from Difference of Specific ...
Página xvi
... Difference of Reading between a Thermo- meter exposed to direct Sunshine and One Shaded diminishes as we ascend in the Atmosphere 548 • 552 IV . Remarks on Mr. J. Y. Buchanan's Theory of the Vertical Distribu- tion of Temperature of the ...
... Difference of Reading between a Thermo- meter exposed to direct Sunshine and One Shaded diminishes as we ascend in the Atmosphere 548 • 552 IV . Remarks on Mr. J. Y. Buchanan's Theory of the Vertical Distribu- tion of Temperature of the ...
Página 3
A Theory of Secular Changes of the Earth's Climate James Croll. difference of ... temperature of the water . In fact , so much is this the case , that warm ... temperature of the water . There are few , I presume , who reflect on the ...
A Theory of Secular Changes of the Earth's Climate James Croll. difference of ... temperature of the water . In fact , so much is this the case , that warm ... temperature of the water . There are few , I presume , who reflect on the ...
Página 9
... temperature would be lowered to an extent that would account for the glacial ... difference in the distribution of land and water would produce the effects ... difference in the distribution of sea and land would produce the effects ...
... temperature would be lowered to an extent that would account for the glacial ... difference in the distribution of land and water would produce the effects ... difference in the distribution of sea and land would produce the effects ...
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amount of heat antarctic aphelion arctic regions Atlantic beds bottom boulder clay Caithness Carboniferous cause consequently considerable density denudation deposits depth descend difference of specific difference of temperature earth's orbit eccentricity ecliptic effect Eocene equal equator equatorial column equatorial regions evidence extent fact feet flow foot-pounds force Geol geological geologists glacial epoch glacier globe Grangemouth greater Greenland Gulf-stream heat received ice-cap icebergs inter-tropical John Herschel land land-ice latitude lower mass mean temperature melting miles Miocene molecules motion North North Sea northern obliquity ocean-currents oceanic circulation perihelion polar column polar regions poles present probably produce Professor quantity of heat radiation regard result river rocks sand Scotland sea-bottom sea-level shear slope snow and ice southern hemisphere specific gravity Straits of Florida stratified stream striated submergence summer sun's supposed surface theory thickness tion tropical warm periods warm water winds winter