Estimation of liquid water path below the melting layer in stratiform precipitation systems using radar measurements during MC3E
Abstract
In this study, the liquid water path (LWP) below the melting layer in stratiform precipitation systems is retrieved, which is a combination of rain liquid water path (RLWP) and cloud liquid water path (CLWP). The retrieval algorithm uses measurements from the vertically pointing radars (VPRs) at 35 and 3 GHz operated by the US Department of Energy Atmospheric Radiation Measurement (ARM) and National Oceanic and Atmospheric Administration (NOAA) during the field campaign Midlatitude Continental Convective Clouds Experiment (MC3E). The measured radar reflectivity and mean Doppler velocity from both VPRs and spectrum width from the 35 GHz radar are utilized. With the aid of the cloud base detected by a ceilometer, the LWP in the liquid layer is retrieved under two different situations: (I) no cloud exists below the melting base, and (II) cloud exists below the melting base. In (I), LWP is primarily contributed from raindrops only, i.e., RLWP, which is estimated by analyzing the Doppler velocity differences between two VPRs. In (II), cloud particles and raindrops coexist below the melting base. The CLWP is estimated using a modified attenuation-based algorithm. Two stratiform precipitation cases (20 and 11 May 2011) during MC3E are illustrated for two situations, respectively. With amore »
- Authors:
-
- Univ. of Arizona, Tucson, AZ (United States)
- Univ. of Colorado, Boulder, CO (United States)
- Publication Date:
- Research Org.:
- Univ. of Colorado, Boulder, CO (United States); Univ. of Arizona, Tucson, AZ (United States)
- Sponsoring Org.:
- USDOE Office of Science (SC)
- OSTI Identifier:
- 1612133
- Grant/Contract Number:
- SC0014294; SC0017015
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Atmospheric Measurement Techniques (Online)
- Additional Journal Information:
- Journal Name: Atmospheric Measurement Techniques (Online); Journal Volume: 12; Journal Issue: 7; Journal ID: ISSN 1867-8548
- Publisher:
- European Geosciences Union
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 54 ENVIRONMENTAL SCIENCES; Meteorology & Atmospheric Sciences
Citation Formats
Tian, Jingjing, Dong, Xiquan, Xi, Baike, Williams, Christopher R., and Wu, Peng. Estimation of liquid water path below the melting layer in stratiform precipitation systems using radar measurements during MC3E. United States: N. p., 2019.
Web. doi:10.5194/amt-12-3743-2019.
Tian, Jingjing, Dong, Xiquan, Xi, Baike, Williams, Christopher R., & Wu, Peng. Estimation of liquid water path below the melting layer in stratiform precipitation systems using radar measurements during MC3E. United States. https://doi.org/10.5194/amt-12-3743-2019
Tian, Jingjing, Dong, Xiquan, Xi, Baike, Williams, Christopher R., and Wu, Peng. Thu .
"Estimation of liquid water path below the melting layer in stratiform precipitation systems using radar measurements during MC3E". United States. https://doi.org/10.5194/amt-12-3743-2019. https://www.osti.gov/servlets/purl/1612133.
@article{osti_1612133,
title = {Estimation of liquid water path below the melting layer in stratiform precipitation systems using radar measurements during MC3E},
author = {Tian, Jingjing and Dong, Xiquan and Xi, Baike and Williams, Christopher R. and Wu, Peng},
abstractNote = {In this study, the liquid water path (LWP) below the melting layer in stratiform precipitation systems is retrieved, which is a combination of rain liquid water path (RLWP) and cloud liquid water path (CLWP). The retrieval algorithm uses measurements from the vertically pointing radars (VPRs) at 35 and 3 GHz operated by the US Department of Energy Atmospheric Radiation Measurement (ARM) and National Oceanic and Atmospheric Administration (NOAA) during the field campaign Midlatitude Continental Convective Clouds Experiment (MC3E). The measured radar reflectivity and mean Doppler velocity from both VPRs and spectrum width from the 35 GHz radar are utilized. With the aid of the cloud base detected by a ceilometer, the LWP in the liquid layer is retrieved under two different situations: (I) no cloud exists below the melting base, and (II) cloud exists below the melting base. In (I), LWP is primarily contributed from raindrops only, i.e., RLWP, which is estimated by analyzing the Doppler velocity differences between two VPRs. In (II), cloud particles and raindrops coexist below the melting base. The CLWP is estimated using a modified attenuation-based algorithm. Two stratiform precipitation cases (20 and 11 May 2011) during MC3E are illustrated for two situations, respectively. With a total of 13 h of samples during MC3E, statistical results show that the occurrence of cloud particles below the melting base is low (9 %); however, the mean CLWP value can be up to 0.56 kg m-2, which is much larger than the RLWP (0.10 kg m-2). When only raindrops exist below the melting base, the average RLWP value is larger (0.32 kg m-2) than the with-cloud situation. The overall mean LWP below the melting base is 0.34 kg m-2 for stratiform systems during MC3E.},
doi = {10.5194/amt-12-3743-2019},
journal = {Atmospheric Measurement Techniques (Online)},
number = 7,
volume = 12,
place = {United States},
year = {Thu Jul 11 00:00:00 EDT 2019},
month = {Thu Jul 11 00:00:00 EDT 2019}
}
Web of Science
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