Abstract
Previous investigations within the shallow valleys east of Johannesburg revealed the presence of a number of anomalies in the mesometeorological regime. These were thought to be related to the juxtaposition of urban and topographically-induced circulation systems. Against the background of a more detailed specification of the mesoclimatology of the area, the possible influence of topography and the urban area on local climate is examined further.
Original language | English |
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Pages (from-to) | 147-164 |
Number of pages | 18 |
Journal | South African Geographical Journal |
Volume | 63 |
Issue number | 2 |
DOIs | |
State | Published - Sep 1981 |