The ATMOS 41 is very durable, even in below-freezing and snowy conditions. There is no need to winterize the sensor suite, though we caution users about effects of snow and ice in the anemometer or on top of the pyranometer. There is no heater in the ATMOS 41, so liquid water will only be measured once the ice and snow melt, and snow that might have overflowed the rain gauge funnel will not be accounted for. The air temperature sensor and correction model both perform well. See data below, recorded at METER’s rooftop testbed during winter of 2019.
What to expect when the pyranometer is covered with a blanket of snow
Solar radiation reaches the pyranometer as diffuse radiation and is suppressed until snow is removed or melts.
What to expect when the anemometer contains ice/snow
A couple of things may be observed when snow/ice are in the anemometer. One observation is that a blanket of snow shelters the opening of the anemometer, which dampens wind speed data.
A second observation is that there could be wind speed spikes (we cap this at 30 m/s) or no sensor output (#N/A). In this case, a little data cleanup may be needed until the ice/snow buildup is removed or melts.
Air temperature and correction model performance
We observed that a blanket of snow covering the ATMOS 41 insulates the unit, and a warmer air temperature will result until the snow is removed.
Overall, air temperatures track well when compared to a non-METER reference sensor (Apogee TS-110 fan-aspirated radiation shield with ST-100 thermistor), which was colocated on METER’s rooftop testbed and connected to a CR1000 data logger. Air temperature measurements over snow on clear-sky days range up to about 2 °C high under low wind speed conditions. This magnitude of error is expected due to the substantial increase in reflected shortwave radiation from snow with albedo near 1, and is much smaller than the error expected from air temperature measurements in a non-aspirated radiation shield (Figure 6).