Observation


falling on its surface. To speedup drying of the sensor



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meteorological elements
falling on its surface. To speedup drying of the sensor
after the rainfall, heating devices can be builtin.


17
2.4.25 Measurement of dew
Dew, being essentially a nocturnal phenomenon, and relatively
small in amount, is nevertheless of much interest in arid
zones. The amount of dew deposited on a given surface in ab bstated period is usually expressed in the same units as
rainfall: mm depth of dew.
A direct method of measuring dew is to expose a weighted
plate of hygrosopic material (gypsum, blotting paper) at
sunset and re-weight it after sunrise. This method requires
accurate weighing and protection at sunrise to prevent
evaporation. Qualitative assessment of dew is obtained by
exposing filter paper "sensors" with dew spots. When wetted
by dew, the spots will spread to an extent which depends on

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