Daidaiton mitar kwararar radar galibi yana shafar waɗannan abubuwa: Na farko, yanayin shigarwa - dole ne firikwensin ya kasance daidai da saman ruwa kuma an sanya shi a cikin sashin tashoshi madaidaiciya (babu cikas aƙalla sau 5 faɗin tashar sama da kuma sau 2 faɗin tashar ƙasa) don guje wa filayen kwarara masu rikitarwa (kamar vortices da backstreams). Na biyu, daidaiton sigogin giciye - kurakurai wajen shigar da girma da siffar sashin giciye na tashar (misali, murabba'i mai kusurwa huɗu, trapezoidal) kai tsaye suna shafar sakamakon lissafin kwarara. Na uku, tsangwama ga muhalli - ƙarfin hasken lantarki, ruwan sama mai yawa, hazo mai yawa, da adadi mai yawa na abubuwa masu iyo a saman ruwa na iya tsoma baki ga siginar radar. Na huɗu, nau'in kayan aiki - mitar kwararar radar da aka haɗa waɗanda ke auna gudu da matakin ruwa yawanci suna da daidaito mafi girma fiye da waɗanda ke auna matakin ruwa kawai. A ƙarƙashin yanayi mai kyau (sashi na yau da kullun, filin kwarara mai karko, kuma an daidaita shi da daidaitattun weirs/flumes), daidaiton zai iya isa cikin ±3%; a cikin yanayi masu rikitarwa kamar koguna na halitta, daidaito gabaɗaya shine ±5% zuwa ±10%.
Lokacin Saƙo: Satumba-28-2025