Interpretation of reasons for equal summer-time sunny and shady slope temperatures in an east-west oriented high-latitude valley, NW Russia
This paper seeks for an answer to a question why a north-facing shady slope may provide equal or even higher daily temperatures than a south-facing sunny slope. Findings are based on data collected in 1998-2000 with the aid of data loggers (type Minilog-TX) which were located on opposite sides of a...
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Format: | Article |
Language: | English |
Published: |
The Geographical Society of Northern Finland
2009-01-01
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Series: | Nordia Geographical Publications |
Online Access: | https://nordia.journal.fi/article/view/75970 |