The Utilization of Nimbus-7 SMMR Measurements to Delineate Rainfall over Land
In light of previous theoretical calculations, an empirical-statistical analysis using satellite multifrequency dual polarized passive microwave data to detect rainfall areas over land was performed. The addition of information from a lower frequency channel (18.0 or 10.7 GHz) was shown to improve t...
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Veröffentlicht in: | Journal of climate and applied meteorology 1983-10, Vol.22 (10), p.1753-1763 |
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description | In light of previous theoretical calculations, an empirical-statistical analysis using satellite multifrequency dual polarized passive microwave data to detect rainfall areas over land was performed. The addition of information from a lower frequency channel (18.0 or 10.7 GHz) was shown to improve the discrimination of rain from wet ground achieved by using a single frequency dual polarized (37 GHz) channel alone. The algorithm was developed and independently tested using data from the Nimbus-7 Scanning Multichannel Microwave Radiometer (SMMR). Horizontally and vertically polarized brightness temperature pairs (TH, TV) at 37, 18, 10.7 GHz were sampled for rain areas over land (determined from ground-based radar), wet ground areas (adjacent and upwind from rain areas determined from radar), and dry land regions (areas where rain had not fallen during a previous 24 h period) over the central and eastern United States. Surface thermodynamic temperatures were both above and below 15°C. An examination of the data from each separate channel indicated that the probability (using the F test) for the mean vectors of any two populations being identical is less than 0.01 for classes sampled with surface thermodynamic temperatures ≥15°C except for the rain over land and wet ground classes observed with the SMMR 37 GHz channel. For the classes sampled with surface thermodynamic temperatures < 15°C, none of the classes were significantly different. Since most of the categories were significantly different for the warmer (≥15°C) land surface cases, a Fisher linear discriminant classifier was then developed for each channel and independently tested. The results from one test case showed that for areas of large-scale heavy rainfall, the lower frequency SMMR channels were better able to delineate rain from wet ground than the 37 GHz channel. However, in areas of light rain and/or where the rain area did not fill the lower frequency instantaneous field of view these channels were not able to differentiate rain from wet ground. |
doi_str_mv | 10.1175/1520-0450(1983)022<1753:TUONSM>2.0.CO;2 |
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The addition of information from a lower frequency channel (18.0 or 10.7 GHz) was shown to improve the discrimination of rain from wet ground achieved by using a single frequency dual polarized (37 GHz) channel alone. The algorithm was developed and independently tested using data from the Nimbus-7 Scanning Multichannel Microwave Radiometer (SMMR). Horizontally and vertically polarized brightness temperature pairs (TH, TV) at 37, 18, 10.7 GHz were sampled for rain areas over land (determined from ground-based radar), wet ground areas (adjacent and upwind from rain areas determined from radar), and dry land regions (areas where rain had not fallen during a previous 24 h period) over the central and eastern United States. Surface thermodynamic temperatures were both above and below 15°C. An examination of the data from each separate channel indicated that the probability (using the F test) for the mean vectors of any two populations being identical is less than 0.01 for classes sampled with surface thermodynamic temperatures ≥15°C except for the rain over land and wet ground classes observed with the SMMR 37 GHz channel. For the classes sampled with surface thermodynamic temperatures < 15°C, none of the classes were significantly different. Since most of the categories were significantly different for the warmer (≥15°C) land surface cases, a Fisher linear discriminant classifier was then developed for each channel and independently tested. The results from one test case showed that for areas of large-scale heavy rainfall, the lower frequency SMMR channels were better able to delineate rain from wet ground than the 37 GHz channel. However, in areas of light rain and/or where the rain area did not fill the lower frequency instantaneous field of view these channels were not able to differentiate rain from wet ground.</description><identifier>ISSN: 0733-3021</identifier><identifier>EISSN: 2163-5366</identifier><identifier>DOI: 10.1175/1520-0450(1983)022<1753:TUONSM>2.0.CO;2</identifier><language>eng</language><publisher>Legacy CDMS: American Meteorological Society</publisher><subject>Arid zones ; Clouds ; Data sampling ; Earth, ocean, space ; Exact sciences and technology ; External geophysics ; Meteorology ; Meteorology And Climatology ; Pixels ; Radar ; Radiance ; Rain ; Statistics ; Surface temperature ; Thermodynamics ; Water in the atmosphere (humidity, clouds, evaporation, precipitation)</subject><ispartof>Journal of climate and applied meteorology, 1983-10, Vol.22 (10), p.1753-1763</ispartof><rights>Copyright 1983, American Meteorological Society (AMS)</rights><rights>1984 INIST-CNRS</rights><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/26181250$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/26181250$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,776,780,799,27901,27902,57992,58225</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=9550279$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Rodgers, Edward</creatorcontrib><creatorcontrib>Siddalingaiah, Honnappa</creatorcontrib><title>The Utilization of Nimbus-7 SMMR Measurements to Delineate Rainfall over Land</title><title>Journal of climate and applied meteorology</title><description>In light of previous theoretical calculations, an empirical-statistical analysis using satellite multifrequency dual polarized passive microwave data to detect rainfall areas over land was performed. The addition of information from a lower frequency channel (18.0 or 10.7 GHz) was shown to improve the discrimination of rain from wet ground achieved by using a single frequency dual polarized (37 GHz) channel alone. The algorithm was developed and independently tested using data from the Nimbus-7 Scanning Multichannel Microwave Radiometer (SMMR). Horizontally and vertically polarized brightness temperature pairs (TH, TV) at 37, 18, 10.7 GHz were sampled for rain areas over land (determined from ground-based radar), wet ground areas (adjacent and upwind from rain areas determined from radar), and dry land regions (areas where rain had not fallen during a previous 24 h period) over the central and eastern United States. Surface thermodynamic temperatures were both above and below 15°C. An examination of the data from each separate channel indicated that the probability (using the F test) for the mean vectors of any two populations being identical is less than 0.01 for classes sampled with surface thermodynamic temperatures ≥15°C except for the rain over land and wet ground classes observed with the SMMR 37 GHz channel. For the classes sampled with surface thermodynamic temperatures < 15°C, none of the classes were significantly different. Since most of the categories were significantly different for the warmer (≥15°C) land surface cases, a Fisher linear discriminant classifier was then developed for each channel and independently tested. The results from one test case showed that for areas of large-scale heavy rainfall, the lower frequency SMMR channels were better able to delineate rain from wet ground than the 37 GHz channel. However, in areas of light rain and/or where the rain area did not fill the lower frequency instantaneous field of view these channels were not able to differentiate rain from wet ground.</description><subject>Arid zones</subject><subject>Clouds</subject><subject>Data sampling</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Meteorology</subject><subject>Meteorology And Climatology</subject><subject>Pixels</subject><subject>Radar</subject><subject>Radiance</subject><subject>Rain</subject><subject>Statistics</subject><subject>Surface temperature</subject><subject>Thermodynamics</subject><subject>Water in the atmosphere (humidity, clouds, evaporation, precipitation)</subject><issn>0733-3021</issn><issn>2163-5366</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1983</creationdate><recordtype>article</recordtype><sourceid>CYI</sourceid><recordid>eNo9kF1rFDEUhoNYcK39Bwq5ENGL2Z58nEzGilBWbQs7XWh3r0M6TTBlNlOTbEF_vTNM6dWB8z7nPfAQcspgyViNpww5VCARPrNGiy_A-bdxLb5ud5vr2_Y7X8JytTnjr8iCMyUqFEq9JguohagEcPaGvM35AUCAFrgg7fa3o7sS-vDPljBEOnh6HfZ3h1zV9LZtb2jrbD4kt3exZFoG-sP1ITpbHL2xIXrb93R4comubbx_R47GRXYnz_OY7H793K4uq_Xm4mp1vq46obFUEpRGKTqmascBAa1mElG4O47eaQde3DcKUSotXSNE0yHqGlBb6b1QXhyTT3PvYxr-HFwuZh9y5_reRjccsuESGo6Mj-DFDHZpyDk5bx5T2Nv01zAwk04z6TSTTjPpNKNOM-k0s07DDZjVxkxNH59f2tzZ3icbu5Bf6hpE4HUzYu9nLNpsTSwpT71y9K0U02P8YY4fchnSyzUfM8YRxH9mNIgj</recordid><startdate>19831001</startdate><enddate>19831001</enddate><creator>Rodgers, Edward</creator><creator>Siddalingaiah, Honnappa</creator><general>American Meteorological Society</general><scope>CYE</scope><scope>CYI</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TB</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>L7M</scope></search><sort><creationdate>19831001</creationdate><title>The Utilization of Nimbus-7 SMMR Measurements to Delineate Rainfall over Land</title><author>Rodgers, Edward ; Siddalingaiah, Honnappa</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c385t-4068543c167e20505a814553eb25fe8e0f3d96554684e9339c5587058a4ff36f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1983</creationdate><topic>Arid zones</topic><topic>Clouds</topic><topic>Data sampling</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Meteorology</topic><topic>Meteorology And Climatology</topic><topic>Pixels</topic><topic>Radar</topic><topic>Radiance</topic><topic>Rain</topic><topic>Statistics</topic><topic>Surface temperature</topic><topic>Thermodynamics</topic><topic>Water in the atmosphere (humidity, clouds, evaporation, precipitation)</topic><toplevel>online_resources</toplevel><creatorcontrib>Rodgers, Edward</creatorcontrib><creatorcontrib>Siddalingaiah, Honnappa</creatorcontrib><collection>NASA Scientific and Technical Information</collection><collection>NASA Technical Reports Server</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Mechanical & Transportation Engineering Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Journal of climate and applied meteorology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Rodgers, Edward</au><au>Siddalingaiah, Honnappa</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The Utilization of Nimbus-7 SMMR Measurements to Delineate Rainfall over Land</atitle><jtitle>Journal of climate and applied meteorology</jtitle><date>1983-10-01</date><risdate>1983</risdate><volume>22</volume><issue>10</issue><spage>1753</spage><epage>1763</epage><pages>1753-1763</pages><issn>0733-3021</issn><eissn>2163-5366</eissn><abstract>In light of previous theoretical calculations, an empirical-statistical analysis using satellite multifrequency dual polarized passive microwave data to detect rainfall areas over land was performed. The addition of information from a lower frequency channel (18.0 or 10.7 GHz) was shown to improve the discrimination of rain from wet ground achieved by using a single frequency dual polarized (37 GHz) channel alone. The algorithm was developed and independently tested using data from the Nimbus-7 Scanning Multichannel Microwave Radiometer (SMMR). Horizontally and vertically polarized brightness temperature pairs (TH, TV) at 37, 18, 10.7 GHz were sampled for rain areas over land (determined from ground-based radar), wet ground areas (adjacent and upwind from rain areas determined from radar), and dry land regions (areas where rain had not fallen during a previous 24 h period) over the central and eastern United States. Surface thermodynamic temperatures were both above and below 15°C. An examination of the data from each separate channel indicated that the probability (using the F test) for the mean vectors of any two populations being identical is less than 0.01 for classes sampled with surface thermodynamic temperatures ≥15°C except for the rain over land and wet ground classes observed with the SMMR 37 GHz channel. For the classes sampled with surface thermodynamic temperatures < 15°C, none of the classes were significantly different. Since most of the categories were significantly different for the warmer (≥15°C) land surface cases, a Fisher linear discriminant classifier was then developed for each channel and independently tested. The results from one test case showed that for areas of large-scale heavy rainfall, the lower frequency SMMR channels were better able to delineate rain from wet ground than the 37 GHz channel. However, in areas of light rain and/or where the rain area did not fill the lower frequency instantaneous field of view these channels were not able to differentiate rain from wet ground.</abstract><cop>Legacy CDMS</cop><pub>American Meteorological Society</pub><doi>10.1175/1520-0450(1983)022<1753:TUONSM>2.0.CO;2</doi><tpages>11</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Arid zones Clouds Data sampling Earth, ocean, space Exact sciences and technology External geophysics Meteorology Meteorology And Climatology Pixels Radar Radiance Rain Statistics Surface temperature Thermodynamics Water in the atmosphere (humidity, clouds, evaporation, precipitation) |
title | The Utilization of Nimbus-7 SMMR Measurements to Delineate Rainfall over Land |
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