Abstract
ABSTRACT Intermittent water temperature measurements collected during the 1961–1972 period at 60 sites on Pakistan streams were analysed for annual variability and regional patterns. Sixty-four per cent or more of the variability in stream temperatures was explained by a simple-harmonic function in 43 of the 60 cases. Regional patterns showed a negative correlation of 0.84 between the harmonic mean coefficient and measurement site altitude.
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