Raindrop Size Distribution Characteristics of the Precipitation Process of 2216 Typhoon “Noru” in the Xisha Region
This study focuses on the comparative analysis and research of the raindrop size distribution (DSD) in the outer rainband and inner rainband of Typhoon “Noru” in 2022, using the OTT-Parsivel raindrop spectrometer deployed on Yongxing Island, Sansha City. The results indicate that precipitation inten...
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Veröffentlicht in: | Water (Basel) 2024-09, Vol.16 (18), p.2630 |
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description | This study focuses on the comparative analysis and research of the raindrop size distribution (DSD) in the outer rainband and inner rainband of Typhoon “Noru” in 2022, using the OTT-Parsivel raindrop spectrometer deployed on Yongxing Island, Sansha City. The results indicate that precipitation intensity is lower when composed mainly of small and medium raindrops and increases with the presence of larger raindrops. Stronger precipitation is associated with a higher number of large raindrops. Due to the interaction of cold and warm air masses, the raindrop concentration is higher, and the raindrop diameters are larger compared to Typhoons “LEKIMA” and “RUMBIA”. The entire process predominantly consists of numerous small- to medium-sized raindrops, characteristic of a tropical typhoon. The precipitation in the inner and outer rainbands exhibits consistent types, characterized by a unimodal raindrop size distribution with a narrow spectral width, typical of stratiform-mixed cloud precipitation, where stratiform precipitation constitutes a significant portion. Strong echo reflectivity factors are often associated with higher raindrop number concentrations and larger particle sizes. The Z-R relationship of the precipitation shows a smaller coefficient but a consistent exponent compared to the standard. The calculated shape parameter slope relationship is Λ=0.02μ[sup.2] +0.696μ+1.539, providing a reference for localizing the Z-R relationship in the South China Sea. |
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The results indicate that precipitation intensity is lower when composed mainly of small and medium raindrops and increases with the presence of larger raindrops. Stronger precipitation is associated with a higher number of large raindrops. Due to the interaction of cold and warm air masses, the raindrop concentration is higher, and the raindrop diameters are larger compared to Typhoons “LEKIMA” and “RUMBIA”. The entire process predominantly consists of numerous small- to medium-sized raindrops, characteristic of a tropical typhoon. The precipitation in the inner and outer rainbands exhibits consistent types, characterized by a unimodal raindrop size distribution with a narrow spectral width, typical of stratiform-mixed cloud precipitation, where stratiform precipitation constitutes a significant portion. Strong echo reflectivity factors are often associated with higher raindrop number concentrations and larger particle sizes. The Z-R relationship of the precipitation shows a smaller coefficient but a consistent exponent compared to the standard. The calculated shape parameter slope relationship is Λ=0.02μ[sup.2] +0.696μ+1.539, providing a reference for localizing the Z-R relationship in the South China Sea.</description><identifier>ISSN: 2073-4441</identifier><identifier>EISSN: 2073-4441</identifier><identifier>DOI: 10.3390/w16182630</identifier><language>eng</language><publisher>Basel: MDPI AG</publisher><subject>Environmental aspects ; Humidity ; Precipitation ; Quality control ; Rain ; Rain and rainfall ; Topography ; Typhoons ; Velocity ; Weather ; Wind</subject><ispartof>Water (Basel), 2024-09, Vol.16 (18), p.2630</ispartof><rights>COPYRIGHT 2024 MDPI AG</rights><rights>2024 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27922,27923</link.rule.ids></links><search><creatorcontrib>Wang, Guozhang</creatorcontrib><creatorcontrib>Li, Lei</creatorcontrib><creatorcontrib>Huang, Chaoying</creatorcontrib><creatorcontrib>Zhang, Lili</creatorcontrib><title>Raindrop Size Distribution Characteristics of the Precipitation Process of 2216 Typhoon “Noru” in the Xisha Region</title><title>Water (Basel)</title><description>This study focuses on the comparative analysis and research of the raindrop size distribution (DSD) in the outer rainband and inner rainband of Typhoon “Noru” in 2022, using the OTT-Parsivel raindrop spectrometer deployed on Yongxing Island, Sansha City. The results indicate that precipitation intensity is lower when composed mainly of small and medium raindrops and increases with the presence of larger raindrops. Stronger precipitation is associated with a higher number of large raindrops. Due to the interaction of cold and warm air masses, the raindrop concentration is higher, and the raindrop diameters are larger compared to Typhoons “LEKIMA” and “RUMBIA”. The entire process predominantly consists of numerous small- to medium-sized raindrops, characteristic of a tropical typhoon. The precipitation in the inner and outer rainbands exhibits consistent types, characterized by a unimodal raindrop size distribution with a narrow spectral width, typical of stratiform-mixed cloud precipitation, where stratiform precipitation constitutes a significant portion. Strong echo reflectivity factors are often associated with higher raindrop number concentrations and larger particle sizes. The Z-R relationship of the precipitation shows a smaller coefficient but a consistent exponent compared to the standard. The calculated shape parameter slope relationship is Λ=0.02μ[sup.2] +0.696μ+1.539, providing a reference for localizing the Z-R relationship in the South China Sea.</description><subject>Environmental aspects</subject><subject>Humidity</subject><subject>Precipitation</subject><subject>Quality control</subject><subject>Rain</subject><subject>Rain and rainfall</subject><subject>Topography</subject><subject>Typhoons</subject><subject>Velocity</subject><subject>Weather</subject><subject>Wind</subject><issn>2073-4441</issn><issn>2073-4441</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><recordid>eNpNT8tOwzAQtBBIVKUH_sAS5xQ_ktg5VuUpVVCVInGrnHTduCpxsB0QnPoh8HP9EqyWA7uHXc3OzGoQOqdkyHlBLj9oTiXLOTlCPUYET9I0pcf_9lM08H5NYqWFlBnpofeZMs3S2RY_mS_AV8YHZ8ouGNvgca2cqgK4CJrKY6txqAFPHVSmNUHtSVNnK_D7I2M0x_PPtrYR322_H6zrdtsfbJq97sX4WuEZrKLsDJ1otfEw-Jt99HxzPR_fJZPH2_vxaJKsqBQhobkucqpAxlycESBcqywXZcFYARp4oUpFSlACSp7lWSUEFUtWKqErkRas5H10cfBtnX3rwIfF2nauiS8XnFIiKGGSRNbwwFqpDSxMo22IwWMv4dVUtgFtIj6SlMpMUCr4L2_hb2k</recordid><startdate>20240901</startdate><enddate>20240901</enddate><creator>Wang, Guozhang</creator><creator>Li, Lei</creator><creator>Huang, Chaoying</creator><creator>Zhang, Lili</creator><general>MDPI AG</general><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope></search><sort><creationdate>20240901</creationdate><title>Raindrop Size Distribution Characteristics of the Precipitation Process of 2216 Typhoon “Noru” in the Xisha Region</title><author>Wang, Guozhang ; Li, Lei ; Huang, Chaoying ; Zhang, Lili</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-g187t-16f961ae8618320e03fa567b9229efe39aba0bea7eb3565c7717d2ba7fc7492b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>Environmental aspects</topic><topic>Humidity</topic><topic>Precipitation</topic><topic>Quality control</topic><topic>Rain</topic><topic>Rain and rainfall</topic><topic>Topography</topic><topic>Typhoons</topic><topic>Velocity</topic><topic>Weather</topic><topic>Wind</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Wang, Guozhang</creatorcontrib><creatorcontrib>Li, Lei</creatorcontrib><creatorcontrib>Huang, Chaoying</creatorcontrib><creatorcontrib>Zhang, Lili</creatorcontrib><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>Publicly Available Content Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><jtitle>Water (Basel)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Wang, Guozhang</au><au>Li, Lei</au><au>Huang, Chaoying</au><au>Zhang, Lili</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Raindrop Size Distribution Characteristics of the Precipitation Process of 2216 Typhoon “Noru” in the Xisha Region</atitle><jtitle>Water (Basel)</jtitle><date>2024-09-01</date><risdate>2024</risdate><volume>16</volume><issue>18</issue><spage>2630</spage><pages>2630-</pages><issn>2073-4441</issn><eissn>2073-4441</eissn><abstract>This study focuses on the comparative analysis and research of the raindrop size distribution (DSD) in the outer rainband and inner rainband of Typhoon “Noru” in 2022, using the OTT-Parsivel raindrop spectrometer deployed on Yongxing Island, Sansha City. The results indicate that precipitation intensity is lower when composed mainly of small and medium raindrops and increases with the presence of larger raindrops. Stronger precipitation is associated with a higher number of large raindrops. Due to the interaction of cold and warm air masses, the raindrop concentration is higher, and the raindrop diameters are larger compared to Typhoons “LEKIMA” and “RUMBIA”. The entire process predominantly consists of numerous small- to medium-sized raindrops, characteristic of a tropical typhoon. The precipitation in the inner and outer rainbands exhibits consistent types, characterized by a unimodal raindrop size distribution with a narrow spectral width, typical of stratiform-mixed cloud precipitation, where stratiform precipitation constitutes a significant portion. Strong echo reflectivity factors are often associated with higher raindrop number concentrations and larger particle sizes. The Z-R relationship of the precipitation shows a smaller coefficient but a consistent exponent compared to the standard. The calculated shape parameter slope relationship is Λ=0.02μ[sup.2] +0.696μ+1.539, providing a reference for localizing the Z-R relationship in the South China Sea.</abstract><cop>Basel</cop><pub>MDPI AG</pub><doi>10.3390/w16182630</doi><oa>free_for_read</oa></addata></record> |
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subjects | Environmental aspects Humidity Precipitation Quality control Rain Rain and rainfall Topography Typhoons Velocity Weather Wind |
title | Raindrop Size Distribution Characteristics of the Precipitation Process of 2216 Typhoon “Noru” in the Xisha Region |
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