| 8.─Absolute Range of the Thermometer. | |||
| Highest Extreme. | Lowest Extreme. | Greatest Range. | |
| Landsend, (12 years,) | 84° | 19° | 65° |
| London, (80 years,) | 96° | 5° | 91° |
| 9.─Mean Range of the Thermometer. | |||
| Annual Range. | Monthly Range. | Daily Range. | |
| Landsend, | 49° | 24° | 6.7° |
| London, | 64° | 34° | 11.0° |
| 10.─Variation of Temperature of sucessive Days for the whole Year. | ||
| Mean Variation. | Extreme Variation. | |
| Landsend, | 2.4° | 10° |
| London, | 4° | 18° |
The preceding results place, in a striking point of view, the great peculiarity of the climate of this district, as to temperature: possesses, as has been already remarked, all the habitues of a small island remote from any large continent: it exhibits, in a great measure, the qualities of what may be called the ocean climate. This is characterised essentially by a remarkable degree of equability of temperature or small extent of range above or below the mean. In this respect the district of the Landsend is superior to any other part of England, and, indeed, to any place in Europe of which we possess meteorological accounts. Madeira is the only climate which Dr. Clark considers as superior in regard to equability of temperature.[1]
As necessary consequences of the greater equability, it will be seen by the preceding statements that, although there is a difference of only 1½° between the mean annual temperature of this district and that of London, there is a remarkable
- ↑ Influence of Climate, p. 63.
