Title: RADIOSONDE TEMPERATURE, HUMIDITY, AND PRESSURE RESPONSE AT LOW TEMPERATURES
1RADIOSONDE TEMPERATURE, HUMIDITY, AND
PRESSURERESPONSE AT LOW TEMPERATURES
- Stephen R. Hudson, Michael S. Town,
- Von P. Walden, and Stephen G. Warren
- 24 June 2003
2Introduction
- Vaisala RS80 and AIR 4A and 5A radiosondes were
tested during summer and winter at South Pole. - Their response to sudden, large changes in
temperature and humidity was characterized. - Some data were collected with the RS80s to
characterize their response to smaller, more
gradual changes in temperature, humidity and
pressure.
3Large, Sudden Changes
- Moved sondes from inside to outside and recorded
response of reported temperature (T), humidity
(RH) and pressure (P). - Usually building was heated, with an indoor T of
5 to 25C.
- A couple tests were done with an unheated
building, with indoor T between 43 and 56C. - Outside T ranged from -24 to 71C.
- Range of T differences was 11 to 94 K.
4RS80 Temperature Response
5RS80 Temperature Response
- Reported temperature responded with a simple
- exponential decay.
Minimum 2.6 s
Median 5.4 s
Mean 5.9 s
Maximum 10.9 s
- Exponential-decay time
- constants ranged from 2.6
- to 10.9 seconds, with a
- mean of 5.9 seconds.
- There was no apparent difference in the
- character or time of the response between
- summer and winter.
6RS80 Humidity Response
7RS80 Humidity Response
- When moved outside, reported RH initially
decreased, then - increased with an exponential decay towards
the outside value. - The exponential decay began between 5 and 120
seconds after - being moved outside.
- E-folding time constants were between 13 and 420
seconds. - Response was significantly slower in winter
(Tlt-40C) than in - summer (T near 25C).
- Response in unheated winter cases (DT 17 K)
was similar to - winter cases using a heated building.
Summer Winter Unheated winter
of Tests 5 24 2
Outside T (C) -24 to -25 -45 to -71 -60
t1 (sec) 5-30 (30) 5-120 (33) 60-90
t (sec) 13-20 (15) 30-420 (146) 50-120
8RS80 Pressure Response
9RS80 Pressure Response
- When moved outside, the sonde initially reported
increasing P, - followed by a slow exponential decay back to
the correct P. - Reported P increased by 0.4 to 10.0 mb over a
period of 175 to - 450 seconds.
- E-folding time constants were between 230 and
600 seconds. - Magnitude of maximum error increased with
increasing thermal - shock.
Summer Winter Unheated Winter
of Tests 1 24 2
Outside T (C) -25 -45 to -71 -60
t1 (sec) 450 175 to 450 (300) 275 to 400
dP (mb) 3.3 3.5 to 10.0 (6.0) 0.4 to 1.6
t (sec) N/A 230 to 600 (380) N/A, 1500 to recover
10Small, Gradual Changes
- After equilibrating to conditions outside, sonde
was raised and lowered on a 22 m tower at speeds
of 0.4 to 1.0 ms-1.
- At the top of the tower, the temperature was 3
to 5 K warmer, the relative humidity was 3 to 5
higher, and the pressure was about 2 mb lower
than at the surface.
11Tower Tests
- Pressure responded to within the noise level by
the time descent was completed. Change (about
2.2 mb) is approximately correct, according to
hypsometric eqn. - Temperature responded fully within 8 to 15
seconds of completion of descent. - Relative Humidity took 15 to 20 seconds after
descent to fully equilibrate. The sonde was able
to correctly report the supersaturation with
respect to ice.
12Conclusions
- Radiosondes should be stored and prepared at
ambient temperatures - If sondes must be prepared inside, they should be
given at least 30 minutes to equilibrate to cold
environments before launching - Problems can arise even from small temperature
differences, so unheated buildings should be
avoided unless well ventilated
13Conclusions (continued)
- Tests on the tower indicate that the sondes are
capable of providing better data in cold
conditions when given time to equilibrate to
shock of being moved outside - Further work should be done in more controlled
environments, and with proper ventilation - Radiosonde instrumentation still remains sluggish
at low temperatures