Ground-Based Remote Sensing of Cloud Particle Sizes during the 26 November 1991 FIRE II Cirrus Case: Comparisons with In Situ Data
The paper presents the results of retrieving characteristic particle sizes for the November 26 1991 FIRE II case using two methods that utilize ground-based remote sensors. The size information for the complete vertical depth of the cloud was obtained for a 3-hour period from 1830 to 2130 UTC using...
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Veröffentlicht in: | Journal of the atmospheric sciences 1995-12, Vol.52 (23), p.4128-4142 |
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container_title | Journal of the atmospheric sciences |
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creator | Matrosov, S Y Heymsfield, A J Intrieri, J M Orr, B W Snider, J B |
description | The paper presents the results of retrieving characteristic particle sizes for the November 26 1991 FIRE II case using two methods that utilize ground-based remote sensors. The size information for the complete vertical depth of the cloud was obtained for a 3-hour period from 1830 to 2130 UTC using combined Doppler radar and IR radiometer measurements and for two shorter periods using radar reflectivity and CO sub(2) lidar backscatter measurements. The results obtained with both remote sensing techniques are compared for these two periods. Possible retrieval uncertainties are discussed. Comparisons yielded an agreement with a relative standard deviation of 15%-20% between the two methods. Particle sizes retrieved by both methods were compared with 2D particle probe data sampled during 10 time intervals when a research aircraft was crossing the hub area. The relative standard deviation of particle sizes retrieved with the radar-radiometer method from those obtained from 2D probes is about 30% for nine compared times. The corresponding deviation for the lidar-radar method is about 35% for three compared times. The relative standard deviation between particle concentrations retrieved with the radar-radiometer method and those obtained from 2D probes is about 60% for nine compared times. |
doi_str_mv | 10.1175/1520-0469(1995)052<4128:GBRSOC>2.0.CO;2 |
format | Article |
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The size information for the complete vertical depth of the cloud was obtained for a 3-hour period from 1830 to 2130 UTC using combined Doppler radar and IR radiometer measurements and for two shorter periods using radar reflectivity and CO sub(2) lidar backscatter measurements. The results obtained with both remote sensing techniques are compared for these two periods. Possible retrieval uncertainties are discussed. Comparisons yielded an agreement with a relative standard deviation of 15%-20% between the two methods. Particle sizes retrieved by both methods were compared with 2D particle probe data sampled during 10 time intervals when a research aircraft was crossing the hub area. The relative standard deviation of particle sizes retrieved with the radar-radiometer method from those obtained from 2D probes is about 30% for nine compared times. The corresponding deviation for the lidar-radar method is about 35% for three compared times. The relative standard deviation between particle concentrations retrieved with the radar-radiometer method and those obtained from 2D probes is about 60% for nine compared times.</description><identifier>ISSN: 0022-4928</identifier><identifier>EISSN: 1520-0469</identifier><identifier>DOI: 10.1175/1520-0469(1995)052<4128:GBRSOC>2.0.CO;2</identifier><identifier>CODEN: JAHSAK</identifier><language>eng</language><publisher>Boston: American Meteorological Society</publisher><subject>Atmosphere ; Clouds ; Meteorology ; Remote sensing ; Remote sensors</subject><ispartof>Journal of the atmospheric sciences, 1995-12, Vol.52 (23), p.4128-4142</ispartof><rights>Copyright American Meteorological Society Dec 1, 1995</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>314,776,780,3668,27901,27902</link.rule.ids></links><search><creatorcontrib>Matrosov, S Y</creatorcontrib><creatorcontrib>Heymsfield, A J</creatorcontrib><creatorcontrib>Intrieri, J M</creatorcontrib><creatorcontrib>Orr, B W</creatorcontrib><creatorcontrib>Snider, J B</creatorcontrib><title>Ground-Based Remote Sensing of Cloud Particle Sizes during the 26 November 1991 FIRE II Cirrus Case: Comparisons with In Situ Data</title><title>Journal of the atmospheric sciences</title><description>The paper presents the results of retrieving characteristic particle sizes for the November 26 1991 FIRE II case using two methods that utilize ground-based remote sensors. The size information for the complete vertical depth of the cloud was obtained for a 3-hour period from 1830 to 2130 UTC using combined Doppler radar and IR radiometer measurements and for two shorter periods using radar reflectivity and CO sub(2) lidar backscatter measurements. The results obtained with both remote sensing techniques are compared for these two periods. Possible retrieval uncertainties are discussed. Comparisons yielded an agreement with a relative standard deviation of 15%-20% between the two methods. Particle sizes retrieved by both methods were compared with 2D particle probe data sampled during 10 time intervals when a research aircraft was crossing the hub area. The relative standard deviation of particle sizes retrieved with the radar-radiometer method from those obtained from 2D probes is about 30% for nine compared times. The corresponding deviation for the lidar-radar method is about 35% for three compared times. The relative standard deviation between particle concentrations retrieved with the radar-radiometer method and those obtained from 2D probes is about 60% for nine compared times.</description><subject>Atmosphere</subject><subject>Clouds</subject><subject>Meteorology</subject><subject>Remote sensing</subject><subject>Remote sensors</subject><issn>0022-4928</issn><issn>1520-0469</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1995</creationdate><recordtype>article</recordtype><recordid>eNqFkk1v1DAQhi0EEkvhP1gcEByy9Yw_4hSEREO7RKpYtIWz5U0cmiqJFzsBwZFfjqNFHLjsXOYwjx7ZMy8h58DWALk8B4ksY0IVL6Eo5Csm8Y0A1Beby93ttnyLa7Yut6_xAVn9Ix-SFWOImShQPyZPYrxnqTCHFfm9CX4em-zSRtfQnRv85OitG2M3fqW-pWXv54Z-smHq6j5Nul8u0mYOy3i6cxQV_ei_u2HvAk3vAXpd7a5oVdGyC2GOtEzeC1r64WBDF_0Y6Y9uuqPVmFTTTN_byT4lj1rbR_fsbz8jX66vPpcfspvtpirf3WS14HzKUNlC16pRTvEcVatFvrdCirrVaPcoHUpWO1CSW85yiw2m2kuuQOu0JM7PyIuj9xD8t9nFyQxdrF3f29H5ORouochBwEkQc56MQp0GAQUHpk-CoEFxrhbw-X_gvZ_DmNZikCshtBQLtDlCdfAxBteaQ-gGG34aYGbJiFkub5bLmyUjJn3fLBkxx4wYNMyU22T8A20crk8</recordid><startdate>19951201</startdate><enddate>19951201</enddate><creator>Matrosov, S Y</creator><creator>Heymsfield, A J</creator><creator>Intrieri, J M</creator><creator>Orr, B W</creator><creator>Snider, J B</creator><general>American Meteorological Society</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>H8D</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>L7M</scope></search><sort><creationdate>19951201</creationdate><title>Ground-Based Remote Sensing of Cloud Particle Sizes during the 26 November 1991 FIRE II Cirrus Case: Comparisons with In Situ Data</title><author>Matrosov, S Y ; Heymsfield, A J ; Intrieri, J M ; Orr, B W ; Snider, J B</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c433t-26a98c6d6e63726f847ba454cf82ab25e250ce1653a307a2d2222b53618805233</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1995</creationdate><topic>Atmosphere</topic><topic>Clouds</topic><topic>Meteorology</topic><topic>Remote sensing</topic><topic>Remote sensors</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Matrosov, S Y</creatorcontrib><creatorcontrib>Heymsfield, A J</creatorcontrib><creatorcontrib>Intrieri, J M</creatorcontrib><creatorcontrib>Orr, B W</creatorcontrib><creatorcontrib>Snider, J B</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Journal of the atmospheric sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Matrosov, S Y</au><au>Heymsfield, A J</au><au>Intrieri, J M</au><au>Orr, B W</au><au>Snider, J B</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Ground-Based Remote Sensing of Cloud Particle Sizes during the 26 November 1991 FIRE II Cirrus Case: Comparisons with In Situ Data</atitle><jtitle>Journal of the atmospheric sciences</jtitle><date>1995-12-01</date><risdate>1995</risdate><volume>52</volume><issue>23</issue><spage>4128</spage><epage>4142</epage><pages>4128-4142</pages><issn>0022-4928</issn><eissn>1520-0469</eissn><coden>JAHSAK</coden><abstract>The paper presents the results of retrieving characteristic particle sizes for the November 26 1991 FIRE II case using two methods that utilize ground-based remote sensors. The size information for the complete vertical depth of the cloud was obtained for a 3-hour period from 1830 to 2130 UTC using combined Doppler radar and IR radiometer measurements and for two shorter periods using radar reflectivity and CO sub(2) lidar backscatter measurements. The results obtained with both remote sensing techniques are compared for these two periods. Possible retrieval uncertainties are discussed. Comparisons yielded an agreement with a relative standard deviation of 15%-20% between the two methods. Particle sizes retrieved by both methods were compared with 2D particle probe data sampled during 10 time intervals when a research aircraft was crossing the hub area. The relative standard deviation of particle sizes retrieved with the radar-radiometer method from those obtained from 2D probes is about 30% for nine compared times. The corresponding deviation for the lidar-radar method is about 35% for three compared times. The relative standard deviation between particle concentrations retrieved with the radar-radiometer method and those obtained from 2D probes is about 60% for nine compared times.</abstract><cop>Boston</cop><pub>American Meteorological Society</pub><doi>10.1175/1520-0469(1995)052<4128:GBRSOC>2.0.CO;2</doi><tpages>15</tpages><oa>free_for_read</oa></addata></record> |
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language | eng |
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source | American Meteorological Society; EZB-FREE-00999 freely available EZB journals; Alma/SFX Local Collection |
subjects | Atmosphere Clouds Meteorology Remote sensing Remote sensors |
title | Ground-Based Remote Sensing of Cloud Particle Sizes during the 26 November 1991 FIRE II Cirrus Case: Comparisons with In Situ Data |
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