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  • Two models for nowcasting of 1-h, 2-h and 3-h precipitation in the warm part of the year were evaluated. The first model was based on the extrapolation of observed radar reflectivity (COTREC-IPA) and the second one combined the extrapolation with the application of a statistical model (SAMR). The accuracy of the model forecasts was evaluated on independent data using the standard measures of root-mean-squared-error, absolute error, bias and correlation coefficient as well as by spatial verification methods Fractions Skill Score and SAL technique. The results show that SAMR yields slightly better forecasts during the afternoon period. On the other hand very small or no improvement is realized at night and in the very early morning. COTREC-IPA and SAMR forecast a very similar horizontal structure of precipitation patterns but the model forecasts differ in values. SAMR, similarly as COTREC-IPA, is not able to develop new storms or significantly intensify already existing storms. This is caused by a large uncertainty regarding future development. On the other hand, the SAMR model can reliably predict decreases in precipitation intensity.
  • Two models for nowcasting of 1-h, 2-h and 3-h precipitation in the warm part of the year were evaluated. The first model was based on the extrapolation of observed radar reflectivity (COTREC-IPA) and the second one combined the extrapolation with the application of a statistical model (SAMR). The accuracy of the model forecasts was evaluated on independent data using the standard measures of root-mean-squared-error, absolute error, bias and correlation coefficient as well as by spatial verification methods Fractions Skill Score and SAL technique. The results show that SAMR yields slightly better forecasts during the afternoon period. On the other hand very small or no improvement is realized at night and in the very early morning. COTREC-IPA and SAMR forecast a very similar horizontal structure of precipitation patterns but the model forecasts differ in values. SAMR, similarly as COTREC-IPA, is not able to develop new storms or significantly intensify already existing storms. This is caused by a large uncertainty regarding future development. On the other hand, the SAMR model can reliably predict decreases in precipitation intensity. (en)
Title
  • Comparison of precipitation nowcasting by extrapolation and statistical-advection methods
  • Comparison of precipitation nowcasting by extrapolation and statistical-advection methods (en)
skos:prefLabel
  • Comparison of precipitation nowcasting by extrapolation and statistical-advection methods
  • Comparison of precipitation nowcasting by extrapolation and statistical-advection methods (en)
skos:notation
  • RIV/68378289:_____/13:00390563!RIV13-AV0-68378289
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • I, P(ME09033)
http://linked.open...iv/cisloPeriodika
  • 1 April
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 66281
http://linked.open...ai/riv/idVysledku
  • RIV/68378289:_____/13:00390563
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • Precipitation forecast; Statistical models; Regression; Quantitative precipitation forecast; Extrapolation forecast (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • NL - Nizozemsko
http://linked.open...ontrolniKodProRIV
  • [BB5DF769E38C]
http://linked.open...i/riv/nazevZdroje
  • Atmospheric Research
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 123
http://linked.open...iv/tvurceVysledku
  • Pešice, Petr
  • Sokol, Zbyněk
  • Mejsnar, Jan
  • Kitzmiller, D.
http://linked.open...ain/vavai/riv/wos
  • 000316580600003
issn
  • 0169-8095
number of pages
http://bibframe.org/vocab/doi
  • 10.1016/j.atmosres.2012.10.013
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