Raindrop Size Distributions and Rain Characteristics Observed by a PARSIVEL Disdrometer in Beijing, Northern China
Fourteen-month precipitation measurements from a second-generation PARSIVEL disdrometer deployed in Beijing, northern China, were analyzed to investigate the microphysical structure of raindrop size distribution and its implications on polarimetric radar applications. Rainfall types are classified a...
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doaj-9fdc92373b4143509ac26724505d4e512020-11-25T02:01:17ZengMDPI AGRemote Sensing2072-42922019-06-011112147910.3390/rs11121479rs11121479Raindrop Size Distributions and Rain Characteristics Observed by a PARSIVEL Disdrometer in Beijing, Northern ChinaLei Ji0Haonan Chen1Lin Li2Baojun Chen3Xian Xiao4Min Chen5Guifu Zhang6Institute of Urban Meteorology (IUM), Beijing 100089, ChinaCooperative Institute for Research in the Atmosphere, Fort Collins, CO 80523, USAInstitute of Urban Meteorology (IUM), Beijing 100089, ChinaKey Laboratory of Mesoscale Severe Weather (MOE), and School of Atmospheric Sciences, Nanjing University, Nanjing 210023, ChinaInstitute of Urban Meteorology (IUM), Beijing 100089, ChinaInstitute of Urban Meteorology (IUM), Beijing 100089, ChinaSchool of Meteorology and Advanced Radar Research Center, University of Oklahoma, Norman, OK 73019, USAFourteen-month precipitation measurements from a second-generation PARSIVEL disdrometer deployed in Beijing, northern China, were analyzed to investigate the microphysical structure of raindrop size distribution and its implications on polarimetric radar applications. Rainfall types are classified and analyzed in the domain of median volume diameter <inline-formula> <math display="inline"> <semantics> <mrow> <msub> <mi>D</mi> <mn>0</mn> </msub> </mrow> </semantics> </math> </inline-formula> and the normalized intercept parameter <inline-formula> <math display="inline"> <semantics> <mrow> <msub> <mi>N</mi> <mi>w</mi> </msub> </mrow> </semantics> </math> </inline-formula>. The separation line between convective and stratiform rain is almost equivalent to rain rate at 8.6 mm h<sup>−1</sup> and radar reflectivity at 36.8 dBZ. Convective rain in Beijing shows distinct seasonal variations in <inline-formula> <math display="inline"> <semantics> <mrow> <msub> <mrow> <mi>log</mi> </mrow> <mrow> <mn>10</mn> </mrow> </msub> <msub> <mi>N</mi> <mi>w</mi> </msub> <mo>−</mo> <msub> <mi>D</mi> <mn>0</mn> </msub> </mrow> </semantics> </math> </inline-formula> domain. X-band dual-polarization variables are simulated using the <i>T</i>-matrix method to derive radar-based quantitative precipitation estimation (QPE) estimators, and rainfall products at hourly scale are evaluated for four radar QPE estimators using collocated but independent rain gauge observations. This study also combines the advantages of individual estimators based on the thresholds on polarimetric variables. Results show that the blended QPE estimator has better performance than others. The rainfall microphysical analysis presented in this study is expected to facilitate the development of a high-resolution X-band radar network for urban QPE applications.https://www.mdpi.com/2072-4292/11/12/1479Northern Chinaraindrop size distribution (DSD)microphysical processesquantitative precipitation estimation (QPE) |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Lei Ji Haonan Chen Lin Li Baojun Chen Xian Xiao Min Chen Guifu Zhang |
spellingShingle |
Lei Ji Haonan Chen Lin Li Baojun Chen Xian Xiao Min Chen Guifu Zhang Raindrop Size Distributions and Rain Characteristics Observed by a PARSIVEL Disdrometer in Beijing, Northern China Remote Sensing Northern China raindrop size distribution (DSD) microphysical processes quantitative precipitation estimation (QPE) |
author_facet |
Lei Ji Haonan Chen Lin Li Baojun Chen Xian Xiao Min Chen Guifu Zhang |
author_sort |
Lei Ji |
title |
Raindrop Size Distributions and Rain Characteristics Observed by a PARSIVEL Disdrometer in Beijing, Northern China |
title_short |
Raindrop Size Distributions and Rain Characteristics Observed by a PARSIVEL Disdrometer in Beijing, Northern China |
title_full |
Raindrop Size Distributions and Rain Characteristics Observed by a PARSIVEL Disdrometer in Beijing, Northern China |
title_fullStr |
Raindrop Size Distributions and Rain Characteristics Observed by a PARSIVEL Disdrometer in Beijing, Northern China |
title_full_unstemmed |
Raindrop Size Distributions and Rain Characteristics Observed by a PARSIVEL Disdrometer in Beijing, Northern China |
title_sort |
raindrop size distributions and rain characteristics observed by a parsivel disdrometer in beijing, northern china |
publisher |
MDPI AG |
series |
Remote Sensing |
issn |
2072-4292 |
publishDate |
2019-06-01 |
description |
Fourteen-month precipitation measurements from a second-generation PARSIVEL disdrometer deployed in Beijing, northern China, were analyzed to investigate the microphysical structure of raindrop size distribution and its implications on polarimetric radar applications. Rainfall types are classified and analyzed in the domain of median volume diameter <inline-formula> <math display="inline"> <semantics> <mrow> <msub> <mi>D</mi> <mn>0</mn> </msub> </mrow> </semantics> </math> </inline-formula> and the normalized intercept parameter <inline-formula> <math display="inline"> <semantics> <mrow> <msub> <mi>N</mi> <mi>w</mi> </msub> </mrow> </semantics> </math> </inline-formula>. The separation line between convective and stratiform rain is almost equivalent to rain rate at 8.6 mm h<sup>−1</sup> and radar reflectivity at 36.8 dBZ. Convective rain in Beijing shows distinct seasonal variations in <inline-formula> <math display="inline"> <semantics> <mrow> <msub> <mrow> <mi>log</mi> </mrow> <mrow> <mn>10</mn> </mrow> </msub> <msub> <mi>N</mi> <mi>w</mi> </msub> <mo>−</mo> <msub> <mi>D</mi> <mn>0</mn> </msub> </mrow> </semantics> </math> </inline-formula> domain. X-band dual-polarization variables are simulated using the <i>T</i>-matrix method to derive radar-based quantitative precipitation estimation (QPE) estimators, and rainfall products at hourly scale are evaluated for four radar QPE estimators using collocated but independent rain gauge observations. This study also combines the advantages of individual estimators based on the thresholds on polarimetric variables. Results show that the blended QPE estimator has better performance than others. The rainfall microphysical analysis presented in this study is expected to facilitate the development of a high-resolution X-band radar network for urban QPE applications. |
topic |
Northern China raindrop size distribution (DSD) microphysical processes quantitative precipitation estimation (QPE) |
url |
https://www.mdpi.com/2072-4292/11/12/1479 |
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