The Behavior of the Snow White Chilled-Mirror Hygrometer in Extremely Dry Conditions
- 1 November 2003
- journal article
- Published by American Meteorological Society in Journal of Atmospheric and Oceanic Technology
- Vol. 20 (11) , 1560-1567
- https://doi.org/10.1175/1520-0426(2003)020<1560:tbotsw>2.0.co;2
Abstract
The Snow White hygrometer, made by Meteolabor AG, Switzerland, is a new chilled-mirror instrument using a thermoelectric Peltier cooler to measure atmospheric water vapor. Its performance under dry conditions is evaluated in simultaneous measurements using the NOAA/CMDL frost-point hygrometer at Boulder, Colorado; San Cristóbal, Galápagos Islands, Ecuador; Watukosek, Indonesia; and Mauna Loa Observatory, Hawaii. The Snow White exhibits a lower detection limit of about 3%–6% relative humidity, depending on the sensor configuration. This detection limit is determined by the temperature depression attainable by the thermoelectric cooler. In some cases, loss of frost-point control within layers with relative humidity below this detection limit caused inaccurate measurements above these dry layers, where the relative humidity was within the detection range of the instrument. The sensor does not operate in the stratosphere because of the large frost-point depression and the large potential for outgassi... Abstract The Snow White hygrometer, made by Meteolabor AG, Switzerland, is a new chilled-mirror instrument using a thermoelectric Peltier cooler to measure atmospheric water vapor. Its performance under dry conditions is evaluated in simultaneous measurements using the NOAA/CMDL frost-point hygrometer at Boulder, Colorado; San Cristóbal, Galápagos Islands, Ecuador; Watukosek, Indonesia; and Mauna Loa Observatory, Hawaii. The Snow White exhibits a lower detection limit of about 3%–6% relative humidity, depending on the sensor configuration. This detection limit is determined by the temperature depression attainable by the thermoelectric cooler. In some cases, loss of frost-point control within layers with relative humidity below this detection limit caused inaccurate measurements above these dry layers, where the relative humidity was within the detection range of the instrument. The sensor does not operate in the stratosphere because of the large frost-point depression and the large potential for outgassi...Keywords
This publication has 5 references indexed in Scilit:
- Performance of the Meteolabor “Snow White” Chilled-Mirror Hygrometer in the Tropical Troposphere: Comparisons with the Vaisala RS80 A/H-Humicap SensorsJournal of Atmospheric and Oceanic Technology, 2003
- Corrections of Humidity Measurement Errors from the Vaisala RS80 Radiosonde—Application to TOGA COARE DataJournal of Atmospheric and Oceanic Technology, 2002
- Characterization and Correction of Relative Humidity Measurements from Vaisala RS80-A Radiosondes at Cold TemperaturesJournal of Atmospheric and Oceanic Technology, 2001
- The evolution of the dehydration in the Antarctic stratospheric vortexJournal of Geophysical Research: Atmospheres, 1995
- A Control System for Ascent-Descent Balloon Soundings of the AtmosphereJournal of Applied Meteorology, 1966