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Last modified
7/28/2009 2:38:56 PM
Creation date
4/18/2008 9:58:55 AM
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Template:
Weather Modification
Title
Computer Processing of Digital Radar Data Gathered During HIPLEX
Date
4/4/1978
Weather Modification - Doc Type
Report
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<br />'"" <br /> <br />504 <br /> <br />JOURNAL OF APPLIED METEOROLOGY <br /> <br />.. ... .... ............ ..... ...... ....... .............. ......... ............. ....... .... .............. ...... <br />.. ..... ...................... ...... ...............,........ ....... ..... .,............. .......... ....... <br />................................................ .............h.................................. <br />........................................ ....h....~.......................... <br />..................................... .h...............................~. <br />..... ... .......... ... ......... ................ .......... ..... <br />............................ .......................... <br />............ ............ ........................ <br /> <br />................ <br />................ <br /> <br />.... <br /> <br />......... <br />......... <br />.......... <br /> <br />............. <br />.............. <br />............... <br />................ <br />................. <br />.................. <br />.................... <br />...................... <br />........................ <br />.......................... <br />............................. <br />.................................. <br /> <br />RC OROf.l <br /> <br />c.OMPOSITE F'pr <br /> <br />RAOAR SITE <br />OATE <br />START T I~IE <br />ENO T If'lr( <br /> <br />LOW OBI THRESHOLO . <br />MAXIMUM TIL.T <br /> <br />...................... <br />.................... <br /> <br />.................. <br />................ . <br /> <br />................ ~AOAR H[IGHT-"'SL <br />................ RANGE OEL.AY <br />.............. RANGE I'1ARKER I <br />............ RANGE "'ARKER 2 <br />........... RANGE (NO <br /> <br />......... . <br />......... <br /> <br />......... CATFGORY-OBZ <br />( -20 <br />-20 TO (10 <br />IOTa < 20 <br />20 TO <30 <br />30 TO (1t0 <br />ItO ra (50 <br />!to TO (60 <br />). 60 <br />"jRCRA.F f <br /> <br />....... <br />........ <br />......... <br />......... <br />.......... <br />........... <br />............ <br />.............. <br />............... <br />................ <br />................. <br />.................. <br />......... ...... ..... <br />..................... . <br />....................... . <br />......................... . <br />.. .... .......... ... .......... <br />. .... ..... ............... ........ <br /> <br />T lL T <br />1.0 <br />2.0 <br />3.0 <br />".0 <br />'.0 <br />6.0 <br />7,0 <br />B.a <br />9.0 <br />10.0 <br />, , .0 <br />12'.0 <br />'3.0 <br />TOTALS <br /> <br />BINS A80V[ <br />NOISE L.Ev[L <br />1707 <br />13"" <br />1015 <br />6B7 <br />39' <br />33.. <br />2"6 <br />'2 <br />I~ <br />,.. <br />3 <br />o <br />o <br />'BIB <br /> <br />................................... ................................... <br />............. ........... ......... ..... .... . ...... .............. ..... ..... ........ ... <br />....... ........ ......... ..... .......... ........... .. ...... ...... .................. ......... ........ <br />................................................................................................... <br /> <br />FIG. 4. Composite PPI for 0247 GMT 11 May 1976. <br /> <br />c. Data conversion and processing (program RADPROC) <br /> <br />At this stage of processing, the radar data are still <br />in their original DVIP units. A modified version of the <br />Probert-Jones (1962) radar equation is used to convert <br />the DVIP value to meteorological units. Errors due to <br />high reflectivity gradients are not considered although <br />they could be appreciable in some instances. <br />For each 3600 sweep and volume scan, study cases <br />are summarized in report form and on magnetic tape <br />files. A B-scan optionally output on microfiche displays <br />the measured radar intensity using a 14-character <br />alphanumeric code representing 14 levels of 5 dBZ each, <br />ranging from less than 5 to greater than 65 dBZ. In <br />addition, a variable length record file containing re- <br />flectivity data is written on magnetic tape, and on <br />microfiche as an option. A report of internal program <br />information is also supplied with every run of the pro- <br />gram. Whenever tables need to be recomputed due to <br />changes in switch settings of the radar, a message is <br />written to inform the user. <br /> <br />VOLUME 1 i <br /> <br />PAGE I I <br /> <br />.. MONTANA <br />76. 132 <br />21t702 <br />2'0'" <br /> <br />20.0 OBI <br />13.0 OEG <br /> <br />.80 I 1(1'1 <br />25.00 1(", <br />75.00 "'M <br />125.00 101 <br />1!t0.00 I(M <br /> <br />CH,UUC TEA <br /> <br />.. <br />5 <br />6 <br /> <br />OBI' S ABOVE <br />THRESHOLO <br />'9B <br />7B <br />100 <br />B' <br />32 <br />2 <br />o <br />o <br />o <br />o <br />o <br />o <br />o <br />"9' <br /> <br />In addition to the four reports generated by the <br />edit program, the one report and four displays produced <br />by the composite B-scan and error correction program, <br />RADPROC has the option to produce two reports, <br />two magnetic tape files, and one display. A B-scan <br />display, Z. report and status report can be generated <br />directly from RADPROC. The two magnetic tape <br />files are described below. <br /> <br />1) COMPRESSED Z. FILE <br /> <br />The purpose of this file is to supply the user com- <br />munity with equivalent reflectivity (Z.) data already <br />edited and preprocessed in an easily accessible, com- <br />pressed form. <br />This file has variable length records containing the <br />information shown in Table 4. Data are compressed for <br />optimum utilization of tape. Bin information consists <br />of the location of the first and last data bin. A B-scan <br />may be reconstructed from this file even though each <br />record contains only bin information defined for a <br />
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