Abstract
Recent studies have shed new light on humidity conditions in the polar
atmospheric boundary layer, and cast doubt on the reliability of
humidity measurements above the frost point humidity. These issues are
addressed herein by considering the processes that affect humidity and
its measurement in cold climate conditions and by analyzing observations
from two sites, at which the relative humidity is frequently above 100%
at sub-freezing temperatures, as shown by repeatedly observed in-cloud
icing events. Humidity measurements were made at these two sites by the
commonly used Vaisala HMP35 probe and HMP233 capacitance probes
respectively and simultaneously by the same manufacturer’s HMP243 probe
that determines the frost point by a heated capacitance sensor. The
results confirm that the relative humidity is frequently well above the
frost point, both due to radiative cooling and to the advection of moist
air, and that the conventional humidity measurements are unable to
detect these events. Furthermore, after such events, the iced sensors
show too high a humidity. The false values occur due to ice growth on
the probe and cannot be corrected by any algorithm. Our results indicate
that these problems, inherent to conventional humidity measurements in
cold and humid environments, are avoided by the use of HMP243, which has
a heated humidity probe.
| Original language | English |
|---|---|
| Pages (from-to) | 131-147 |
| Journal | Boundary-Layer Meteorology |
| Volume | 116 |
| Issue number | 1 |
| DOIs | |
| Publication status | Published - 2005 |
| MoE publication type | A1 Journal article-refereed |
Keywords
- arctic boundary layer
- frost point
- humidity measurements
- hygrometers
- icing
- relative humidity
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