## Abstract A method of obtaining continuous records are discussed. The relations between surface and sub‐surface temperatures are briefly considered, and then, in more detail, the inter‐dependence of soil surface and air temperatures is examined. At all seasons the soil temperature is in phase wi
A comparison of the daily extremes of temperature at two stations in a Chiltern dry valley
✍ Scribed by M. B. King
- Publisher
- John Wiley and Sons
- Year
- 1952
- Tongue
- English
- Weight
- 116 KB
- Volume
- 78
- Category
- Article
- ISSN
- 0035-9009
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