On the Performance of Hot-Wire Water Content Probes in Supercooled Large Droplet (SLD) Conditions
ORAL
Abstract
Supercooled Large Droplet (SLD) icing conditions pose a significant risk to aviation, as the larger mass of impinging water can lead to complex ice accretions and runback into unprotected regions of an aircraft. A common method to measure the cloud’s liquid water content (LWC), a key parameter for icing, uses hot-wire probes. However, accurate in-flight measurement of LWC in SLD conditions is challenging due to physical effects like droplet splashing and deformation. This study provides a detailed performance evaluation of two hot-wire probes, the Science Engineering Associates (SEA) Multi-Element Probe and the SEA Ice Crystal Detector, by comparing their measurements against the Isokinetic Probe 2 as a reference standard.
Experiments were conducted in the NASA Icing Research Tunnel across a range of SLD conditions. Stokes number sweeps were performed at -10°C and -15°C, covering median volume diameters from 14.1 µm to 469 µm and airspeeds from 50 to 300 knots. Our analysis reveals a distinct drop-off in the collection efficiency of both hot-wire probes with increasing droplet size. High-speed video footage corroborates this finding, showing significant splashing off the hot-wire sensing elements, including the concave total water content element. Additionally, results show a persistent bias in the dry air power readings, likely caused by ice accumulation on the probe strut.
These findings provide crucial information on the effective operating range of modern hot-wire probes and suggest that new correction factors are needed for reliable measurements in high-droplet-size cases. While the observed collection efficiency trends can inform these corrections, the issue of dry air power bias warrants further investigation.
Experiments were conducted in the NASA Icing Research Tunnel across a range of SLD conditions. Stokes number sweeps were performed at -10°C and -15°C, covering median volume diameters from 14.1 µm to 469 µm and airspeeds from 50 to 300 knots. Our analysis reveals a distinct drop-off in the collection efficiency of both hot-wire probes with increasing droplet size. High-speed video footage corroborates this finding, showing significant splashing off the hot-wire sensing elements, including the concave total water content element. Additionally, results show a persistent bias in the dry air power readings, likely caused by ice accumulation on the probe strut.
These findings provide crucial information on the effective operating range of modern hot-wire probes and suggest that new correction factors are needed for reliable measurements in high-droplet-size cases. While the observed collection efficiency trends can inform these corrections, the issue of dry air power bias warrants further investigation.
–
Presenters
-
Ru-Ching Chen
NASA John H. Glenn Research Center
Authors
-
Ru-Ching Chen
NASA John H. Glenn Research Center
-
Emily Timko
Amentum
-
Judith Van Zante
NASA John H. Glenn Research Center