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<br />REPORT DOCUMENTATION PAGE I Form ApprOvl1d <br /> OM8 No. 0704.0188 <br />"""lIC:rlPO<t,ng tlur"""lo. In.C~'''''''ol "'1.""..'_....""""""0.__1 n...'!W'...l>O"....ncUcl""l"..t""'.or_""""o....U'Ue"G1\5....,C'""lI..o(I1"11 <br /><I...IO<ItC....II.II...""J_",...,!.IO<W>lI'...d.'._<I......comc>Io""II_~_......,,"'"f>I"'!tw"'/II,on s...llC.............'...'d"'9lnIlDu'......I.....'. <br />or .n~ (If"'" "~C1 of 111. cohc,_ Of onj",,,,,,toOn. tnekod"'ll_..t"",. r......,.,.,,,,o II'MS tIU"""'o W_""'91on ~""'"'''''''. s.Mcn. OotIK''''''.'''' Inlo"..._ <br />~'.'''''''.<><l~, 121$ Joolf.~O''''"Hogn...'.SUIl.1204.Atlol'l91on\lA22202.n02._to_Olfoceor~I_8ude'".P__~~t_ <br />lto1>o",0704-D\I"',W'L" o"OC1~] <br />1. AGENCY USE ONLY (b.... 81.nk, 2. REPORT DATE 3. REPORT TYPE AND DATES COVERED <br /> J''''' 1998 Final <br />4. mu AND SUalrrLE 5. FUNDING NUMBERS <br />Snow Accumulation AI......,.;lhm lor \he WSR-880 RADAR: Final Rennrt <br />6. AUTHOR(S) <br />Arlin B. SIJDPf and Edmond W. Holrovd, II! <br />7. PERFORMING ORGANIZATION NAME(S) AND ADDRESSeES) 8. PERFORMING ORGANlZAnON <br /> REPORT NUMBER <br />Bureau of ReclamaliOn <br />Water Resources Research Labomtory A.98.05 <br />Ted'mlcaJ Service Center <br />Denver, Colorado <br />9. SPONSORINGlMONrroR'NG AGENCY NAME(S) AND ADORESS(ES) 10, SPONSORINGlMONITORJNG <br /> AGENCY REPORT NUMBER <br />S.me <br />11. SUPPLEMENTARY NOnS <br />Hard conv available at the technical Sel'Vlce Cenler, Denver, Colorado <br />12.. DISTRIBUnoH/AVAllABlllTY STATEMENT 12b. DlSTRIBUTlON CODE <br />Available from the NallOnal techmcal Information service. OperallOns Division, <br />5285 Po" Roval Rood. -S-~;eId, VirQinia 22162 <br />13. ABSTRACT (M&nmum 2O(J words) <br />This !loal report mostly descnbes ttl8 final of three years 01 SM (Snow Accumulation Algorithm) development for NEXAAO <br />WSA-88D radars. An optimization technique applied to special snow/all observallons and Levell! reflectivtty rrn!8Surements <br />oelermined Z.-S (reflectivity.snowfall) r~hon&hips for radars in SfIveral climatic zones. These relationships were Similar for <br />most sites WI!h standard power law coeffICients near 150 and exponents near 2.0. Signiflcanl underestimation at longer ranqes <br />was evidenl at aR raaars, particularly WIth shallow stonns_ The SM now has a flInge correcliOn schernG and SUQgesbOllS are <br />gIVen lor determining appropriate coefficients lor 'I. <br />The SM was successfully field tested in real-time in Ohio, Minnesota, and New York. The SM produced reasonably accurate <br />estimates of storm-total snow water equivalent for all test areas, well correlated wrth surface observations. Customizad hybrid <br />scans W9fe requirlld in order 10 use the lowesf practical beam tilL The vertical profile of Z.changes the Z..S relationship WIth <br />higher elevation scamng. <br />The SM is operationally ready for use at those lew radars With suitable hardware. However, more powerful computers will be <br />needed belore SAA availability on all NEXRAD units. <br />Aecommendad SAA improvements include identificaoon 01 bright band contaminatIOn, handling far range virga, and adjusting for <br />longer range undefes1lmatton of snowfall. <br />14. SUBJECT TERMS 15. NUMBER OF PAGES <br /> 7' <br /> '5. PRICE CODE <br />17. SECURITY ClASSIFICATION 18. SECUArTY ClASSIFICATION 19. SECURTTY CLASSIFICATION 20. LIMITATION OF <br />OF REPORT OF THIS PAGE OF ABSTRACT ABSTRACT <br />UL UL UL UL <br /> <br />"'SN7S4O-(1I.2!lG-~ <br /> <br />SW1Ca'llformll'ifl(.....2-8a) <br />~c.dby"I'ISISrQ.2J{l..1I <br />".", <br />