A differential emissivity imaging technique for measuring hydrometeor mass and type
Abstract
Abstract. The Differential Emissivity Imaging Disdrometer (DEID) is a new evaporation-based optical and thermal instrument designed to measure the mass, size, density and type of individual hydrometeors as well as their bulk properties. Hydrometeor spatial dimensions are measured on a heated metal plate using an infrared camera by exploiting the much higher thermal emissivity of water compared with metal. As a melted hydrometeor evaporates, its mass can be directly related to the loss of heat from the hotplate assuming energy conservation across the hydrometeor. The heat loss required to evaporate a hydrometeor is found to be independent of environmental conditions including ambient wind velocity, moisture level and temperature. The difference in heat loss for snow vs. rain for a given mass offers a method for discriminating precipitation phase. The DEID measures hydrometeors at sampling frequencies of up to 1 Hz with masses and effective diameters greater than 1 µg and 200 µm, respectively, determined by the size of the hotplate and the thermal camera specifications. Measurable snow water equivalent (SWE) precipitation rates range from 0.001 to 200 mm h−1, as validated against a standard weighing bucket. Preliminary field experiment measurements of snow and rain from the winters of 2019 and 2020 provided continuous automated measurementsmore »
- Authors:
- Publication Date:
- Research Org.:
- Particle Flux Analytics Inc., Salt Lake City, UT (United States)
- Sponsoring Org.:
- USDOE Office of Science (SC); National Science Foundation (NSF); Colorado Department of Transportation
- OSTI Identifier:
- 1829174
- Alternate Identifier(s):
- OSTI ID: 1830816
- Grant/Contract Number:
- SC-0017168; SC0017168
- Resource Type:
- Published Article
- Journal Name:
- Atmospheric Measurement Techniques (Online)
- Additional Journal Information:
- Journal Name: Atmospheric Measurement Techniques (Online) Journal Volume: 14 Journal Issue: 11; Journal ID: ISSN 1867-8548
- Publisher:
- Copernicus GmbH
- Country of Publication:
- Germany
- Language:
- English
- Subject:
- 54 ENVIRONMENTAL SCIENCES; 47 OTHER INSTRUMENTATION
Citation Formats
Singh, Dhiraj K., Donovan, Spencer, Pardyjak, Eric R., and Garrett, Timothy J. A differential emissivity imaging technique for measuring hydrometeor mass and type. Germany: N. p., 2021.
Web. doi:10.5194/amt-14-6973-2021.
Singh, Dhiraj K., Donovan, Spencer, Pardyjak, Eric R., & Garrett, Timothy J. A differential emissivity imaging technique for measuring hydrometeor mass and type. Germany. https://doi.org/10.5194/amt-14-6973-2021
Singh, Dhiraj K., Donovan, Spencer, Pardyjak, Eric R., and Garrett, Timothy J. Thu .
"A differential emissivity imaging technique for measuring hydrometeor mass and type". Germany. https://doi.org/10.5194/amt-14-6973-2021.
@article{osti_1829174,
title = {A differential emissivity imaging technique for measuring hydrometeor mass and type},
author = {Singh, Dhiraj K. and Donovan, Spencer and Pardyjak, Eric R. and Garrett, Timothy J.},
abstractNote = {Abstract. The Differential Emissivity Imaging Disdrometer (DEID) is a new evaporation-based optical and thermal instrument designed to measure the mass, size, density and type of individual hydrometeors as well as their bulk properties. Hydrometeor spatial dimensions are measured on a heated metal plate using an infrared camera by exploiting the much higher thermal emissivity of water compared with metal. As a melted hydrometeor evaporates, its mass can be directly related to the loss of heat from the hotplate assuming energy conservation across the hydrometeor. The heat loss required to evaporate a hydrometeor is found to be independent of environmental conditions including ambient wind velocity, moisture level and temperature. The difference in heat loss for snow vs. rain for a given mass offers a method for discriminating precipitation phase. The DEID measures hydrometeors at sampling frequencies of up to 1 Hz with masses and effective diameters greater than 1 µg and 200 µm, respectively, determined by the size of the hotplate and the thermal camera specifications. Measurable snow water equivalent (SWE) precipitation rates range from 0.001 to 200 mm h−1, as validated against a standard weighing bucket. Preliminary field experiment measurements of snow and rain from the winters of 2019 and 2020 provided continuous automated measurements of precipitation rate, snow density and visibility. Measured hydrometeor size distributions agree well with canonical results described in the literature.},
doi = {10.5194/amt-14-6973-2021},
journal = {Atmospheric Measurement Techniques (Online)},
number = 11,
volume = 14,
place = {Germany},
year = {2021},
month = {11}
}
https://doi.org/10.5194/amt-14-6973-2021
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