I have been rather disappointed about the Barani performance compared to a lot of both professional and amateur weather stations around my area, none of which (as far as I know) use the Barani.
This feeling has been amplified around the hours during sunrise and sunset. That is why the SmartCellino has peaked my interest. Or maybe the correct choice at 60° N is an active shield like the Davis?
There is not much wind at my location either, which I think is part of the problem...
So for fun one week ago I put up an old TFA outdoor sensor on the north side of my property where it is shielded from the sun all day, just behind a shed in the garden.
Today after days of clouds there is finally a clear sky now and a good time to compare the two.
Barani vs always-shaded TFA sensor:
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0.9 degree C is too big a difference for me to feel comfortable about my setup.
At first I thought I had the Barani mounted too close to the ground at 185 cm so I raised it to 200 cm (also to be at the WMO recommended height) but I can't really see any difference - which makes sense if the height wasn't the problem to begin with, but rather the radiation hitting inside the shield at low sun altitudes.
edit: I will add that the picture was taken at 12:47 today and that puts the sun at 22 degrees above the horizon (60° N). The Meridian was just a minute before at 12:46 so the sun is already getting lower from this point onward.
To be more precise and exhaustive, I will better explain the two different types of problem trying to be very practical and apologizing for any errors due to my rather approximate English.
- the comparison with nearby stations is useless, different positioning, different orography, different height and/or exposure, different roughness of the terrain and relative impact on ventilation etc. etc. make the comparison useless
- a sensor constantly in the shade will never be able to provide data on the air temperature if not in a frighteningly approximate way.
Solar screens were born with two main functions, to protect the sensor from rain, hail etc and to protect it from direct, diffuse and reflected solar radiation.
The air is transparent to radiation, it does not heat up in the sun, what heats up is everything it hits, lawns, roads, houses, water and obviously the screens and, if these are not of adequate quality, the sensors inside them.
Each of these components, and many others, has its own thermal characteristics, the soil and the sea, in particular, are the most important, they are those that determine, by convection, the temperature of the air already in the first layers above the ground, in decreasing measure as one moves away from it
If an area of the ground is totally in shadow, the data on the temperature of the air above it are totally useless except for personal research purposes.
M.