| Nathaniel Beardmore - 1852 - 240 стор.
...minimum readings and correcting it by the numbers in Table II. At all places the form of the dinrnal variation is a single progression, having one ascending...is therefore possible that the corrections in Table I. may not be of universal application, but as the form of the curve described by the daily march is... | |
| Edward Hughes - 1858 - 474 стор.
...unless they are made very accurately with respect to time, are not worthy of implicit confidence. 19. If we compare the mean temperatures of places that...temperature than those situated upon a clayey, wet soil. 20. At all places the form of the diurnal variation is a simple progression, having one ascending branch... | |
| William Kebbell - 1859 - 204 стор.
...compare," observes Mr Grlaisher, " places having the same latitude, we shall find that the mean temperature of those places situated inland will be higher in...temperature than those situated upon a clayey wet soil!'* The general effect of the sea upon the climate of Brighton is to raise the mean temperature of the... | |
| Nathaniel Beardmore - 1862 - 446 стор.
...locality, and geological formation of the country. If we compare the mean temperatures of places which differ considerably from each other in latitude, we...than those situated in the vicinity of the sea. If we com pare places differing only in their geological formations, we shall find that those places situated... | |
| Nathaniel Beardmore - 1906 - 502 стор.
...the same latitude, we shall find that the mean temperatures of those places situated inland will he higher in the summer months, and lower in the winter...is therefore possible that the corrections in Table I. may not be of universal application, but as the form of the curve described by the daily march is... | |
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