2021
DOI: 10.1016/j.jhydrol.2020.125931
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Relevance of merging radar and rainfall gauge data for rainfall nowcasting in urban hydrology

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Cited by 19 publications
(14 citation statements)
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“…Nevertheless, studies have found that, for fine spatial (1 km 2 ) and temporal (5 min) scales, the Lagrangian persistence can yield reliable results up to 20-30 min lead time, which is also known in the literature as the predictability limit of rainfall at such scales (Grecu and Krajewski, 2000;Kato et al, 2017;Ruzanski et al, 2011). In object-based radar nowcasting, this predictability limit can be extended up to 1 h for stratiform events and up to 30-45 min for convective events if a better radar product (merged with rain-gauge data) is fed into the nowcast model (Shehu and Haberlandt, 2021). Past these lead times, the errors due to the growth/decay and dissipation of the storms dominate.…”
Section: Introductionmentioning
confidence: 92%
“…Nevertheless, studies have found that, for fine spatial (1 km 2 ) and temporal (5 min) scales, the Lagrangian persistence can yield reliable results up to 20-30 min lead time, which is also known in the literature as the predictability limit of rainfall at such scales (Grecu and Krajewski, 2000;Kato et al, 2017;Ruzanski et al, 2011). In object-based radar nowcasting, this predictability limit can be extended up to 1 h for stratiform events and up to 30-45 min for convective events if a better radar product (merged with rain-gauge data) is fed into the nowcast model (Shehu and Haberlandt, 2021). Past these lead times, the errors due to the growth/decay and dissipation of the storms dominate.…”
Section: Introductionmentioning
confidence: 92%
“…Correspondingly, more studies are required to assess the performance of GPM IMERG against other satellite and reanalysis products to find the advantages and limitations of the GPM satellite. Furthermore, other precipitation specific properties such as spatial and temporal heterogeneity, spatial and temporal intermittence, extreme variability and multi-fractal comparisons is necessary to overcome substantial uncertainties rainfall estimations [57][58][59]. Cristiano et al [60] also depicted in their review that the rainfall variability may need wider range of conditions and scenario based in observational datasets for urban hydrological basins, which need proper analysis for development of better hydrological response system with higher sensitivity.…”
Section: Future Studies and Shortcomingsmentioning
confidence: 99%
“…The radar data were corrected from the static clutters and erroneous beams and then converted to Cartesian Coordinate system (1 km 2 and 5 min) as described in Berndt et al (2014). Additionally, following the results from Shehu & Haberlandt (2021), a conditional merging between the radar data and 100 gauge recording with the radar range at 5 min time steps was performed. The period from 2000 to 2018 was used as a basis for this investigation, from which 110 events with different characteristics were extracted (see Shehu & Haberlandt (2021) or Shehu (2020)).…”
Section: Study Area and Datamentioning
confidence: 99%
“…Additionally, following the results from Shehu & Haberlandt (2021), a conditional merging between the radar data and 100 gauge recording with the radar range at 5 min time steps was performed. The period from 2000 to 2018 was used as a basis for this investigation, from which 110 events with different characteristics were extracted (see Shehu & Haberlandt (2021) or Shehu (2020)). These events were selected for urban flood purposes, thus contain mainly convective events and few stratiform events.…”
Section: Study Area and Datamentioning
confidence: 99%
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