The UV sensor aims to measure the intensity of the ultraviolet part of 
the sun’s spectrum (as opposed to the ‘solar’ sensor which measures the 
visible and near IR part of the spectrum).
UV readings are also expressed in a different format from the ‘solar’ 
sensor readings: For the solar sensor, straightforward irradiance values
 in units of W/sqm are recorded. But the prime practical reason for 
monitoring UV levels is to guide human skin exposure, preventing sunburn
 and possible skin cancer risks.Therefore UV readings are expressed on a
 UV Index scale of 0-16 which weights the intensity by the wavelengths 
of the UV light most likely to cause skin damage. This seems to be 
explained reasonably well on the relevant Wikipedia page, where one 
index unit corresponds to an irradiance value of about 25W/sqm. Maximum 
midsummer UVI readings in the UK rarely exceed 7-8,although 
substantially higher readings are commonly registered at lower latitudes
 than the UK. 
Davis Application Note #6 also provides further information on interpreting UV readings.
UV readings are technically difficult to make – the sensors need 
extensive individual calibration and the signal is low in amplitude 
hence causing noisy readings. This has two consequences. First, UV 
sensors are expensive because of the prolonged production and 
calibration process. (You may think that the Davis UV sensor is 
expensive, but sensitive high-end UV sensors are considerably more so.) 
The second consequence is that, without moving to a still more 
sophisticated and costly sensor design, there is unavoidably some noise 
and short-term fluctuation in the sensor output, even under dark 
conditions when of course there should be zero UV readings. When the UV 
sensor was first introduced, Davis was troubled by support calls 
reporting overnight UV readings of 0.1 or 0.2 UVI, even occasionally 
higher, which were simply a consequence of noise in the dark current 
circuitry. The consensus was that these very low but false readings 
overnight were more of a concern to users than having good sensitivity 
at low UV levels. So the decision was taken that there would be a 
threshold in the displayed UV reading of 0.4 and below which any reading
 would show as zero and this is the solution that remains in place.
The result is of course that wintertime readings in higher latitudes 
such as the UK will typically show as zero unless the UVI value is above
 0.3.
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