Automated rain rate estimates using the Ka-band ARM zenith radar (KAZR)
-
Published:2015-09-14
Issue:9
Volume:8
Page:3685-3699
-
ISSN:1867-8548
-
Container-title:Atmospheric Measurement Techniques
-
language:en
-
Short-container-title:Atmos. Meas. Tech.
Author:
Chandra A.ORCID, Zhang C.ORCID, Kollias P., Matrosov S., Szyrmer W.
Abstract
Abstract. The use of millimeter wavelength radars for probing precipitation has recently gained interest. However, estimation of precipitation variables is not straightforward due to strong signal attenuation, radar receiver saturation, antenna wet radome effects and natural microphysical variability. Here, an automated algorithm is developed for routinely retrieving rain rates from the profiling Ka-band (35-GHz) ARM (Atmospheric Radiation Measurement) zenith radars (KAZR). A 1-dimensional, simple, steady state microphysical model is used to estimate impacts of microphysical processes and attenuation on the profiles of radar observables at 35-GHz and thus provide criteria for identifying situations when attenuation or microphysical processes dominate KAZR observations. KAZR observations are also screened for signal saturation and wet radome effects. The algorithm is implemented in two steps: high rain rates are retrieved by using the amount of attenuation in rain layers, while low rain rates are retrieved from the reflectivity–rain rate (Ze–R) relation. Observations collected by the KAZR, rain gauge, disdrometer and scanning precipitating radars during the DYNAMO/AMIE field campaign at the Gan Island of the tropical Indian Ocean are used to validate the proposed approach. The differences in the rain accumulation from the proposed algorithm are quantified. The results indicate that the proposed algorithm has a potential for deriving continuous rain rate statistics in the tropics.
Publisher
Copernicus GmbH
Subject
Atmospheric Science
Reference31 articles.
1. Aydin, K. and Daisley, S. E. A.: Relationships between rainfall rate and 35 GHz attenuation and differential attenuation: modeling the effects of raindrop size distribution, canting, and oscillation, IEEE T. Geosci. Remote, 40, 2343–2351, 2002. 2. Bohren, C. F. and Huffman, D. R.: Absorption and Scattering of Light by Small Particles, Wiley, New York, USA, 530 pp., 1983. 3. Feng, Z., McFarlane, S. A., Schumacher, C., Ellis, S., and Bharadwaj, N.: Constructing a merged cloud-precipitation radar dataset for tropical convective clouds during the DY- NAMO/AMIE Experiment at Addu Atoll, J. Atmos. Ocean. Technol., 31, 1021–1042, https://doi.org/10.1175/JTECH-D-13-00132.1, 2014. 4. Geerts, B. and Dawei, Y.: Classification and characterization of tropical precipitation based on high-resolution airborne vertical incidence radar, Part I: Classification, J. Appl. Meteorol., 43, 1554–1566, 2004. 5. Huffman, G. J., Bolvin, D. T., Nelkin, E. J., Wolff, D. B., Adler, R. F., Gu, G., Hong, Y., Bowman, K. P., and Stocker, E. F.: The TRMM Multisatellite Precipitation Analysis (TMPA): quasi-global, multiyear, combined-sensor precipitation estimates at fine scales, J. Hydrometeorol., 8, 38–55, 2007.
Cited by
18 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
|
|