Articles | Volume 26, issue 6
https://doi.org/10.5194/hess-26-1631-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-26-1631-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Improving radar-based rainfall nowcasting by a nearest-neighbour approach – Part 1: Storm characteristics
Institute for Hydrology and Water Resources Management, Leibniz
University Hannover, Hanover, Germany
Uwe Haberlandt
Institute for Hydrology and Water Resources Management, Leibniz
University Hannover, Hanover, Germany
Related authors
Anne Bartens, Bora Shehu, and Uwe Haberlandt
Hydrol. Earth Syst. Sci., 28, 1687–1709, https://doi.org/10.5194/hess-28-1687-2024, https://doi.org/10.5194/hess-28-1687-2024, 2024
Short summary
Short summary
River flow data are often provided as mean daily flows (MDF), in which a lot of information is lost about the actual maximum flow or instantaneous peak flows (IPF) within a day. We investigate the error of using MDF instead of IPF and identify means to predict IPF when only MDF data are available. We find that the average ratio of daily flood peaks and volumes is a good predictor, which is easily and universally applicable and requires a minimum amount of data.
Bora Shehu and Uwe Haberlandt
Hydrol. Earth Syst. Sci., 27, 2075–2097, https://doi.org/10.5194/hess-27-2075-2023, https://doi.org/10.5194/hess-27-2075-2023, 2023
Short summary
Short summary
Design rainfall volumes at different duration and frequencies are necessary for the planning of water-related systems and facilities. As the procedure for deriving these values is subjected to different sources of uncertainty, here we explore different methods to estimate how precise these values are for different duration, locations and frequencies in Germany. Combining local and spatial simulations, we estimate tolerance ranges from approx. 10–60% for design rainfall volumes in Germany.
Bora Shehu, Winfried Willems, Henrike Stockel, Luisa-Bianca Thiele, and Uwe Haberlandt
Hydrol. Earth Syst. Sci., 27, 1109–1132, https://doi.org/10.5194/hess-27-1109-2023, https://doi.org/10.5194/hess-27-1109-2023, 2023
Short summary
Short summary
Rainfall volumes at varying duration and frequencies are required for many engineering water works. These design volumes have been provided by KOSTRA-DWD in Germany. However, a revision of the KOSTRA-DWD is required, in order to consider the recent state-of-the-art and additional data. For this purpose, in our study, we investigate different methods and data available to achieve the best procedure that will serve as a basis for the development of the new KOSTRA-DWD product.
Ross Pidoto, Nejc Bezak, Hannes Müller-Thomy, Bora Shehu, Ana Claudia Callau-Beyer, Katarina Zabret, and Uwe Haberlandt
Earth Surf. Dynam., 10, 851–863, https://doi.org/10.5194/esurf-10-851-2022, https://doi.org/10.5194/esurf-10-851-2022, 2022
Short summary
Short summary
Erosion is a threat for soils with rainfall as the driving force. The annual rainfall erosivity factor quantifies rainfall impact by analysing high-resolution rainfall time series (~ 5 min). Due to a lack of measuring stations, alternatives for its estimation are analysed in this study. The best results are obtained for regionalisation of the erosivity factor itself. However, the identified minimum of 60-year time series length suggests using rainfall generators as in this study as well.
Golbarg Goshtasbpour and Uwe Haberlandt
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2024-177, https://doi.org/10.5194/hess-2024-177, 2024
Preprint under review for HESS
Short summary
Short summary
We provide a method how to estimate extreme rainfall from radar observations. Extreme value statistic is applied for observed radar rainfall covering different areas from point size up to about 1000 km2. The rainfall extremes are supposed to be as higher as smaller the area is. This behaviour could not be confirmed by the radar observations. The reason is the limited single point sampling approach of the radar data. New multiple point sampling strategies are proposed to mitigate this problem.
Anne Bartens, Bora Shehu, and Uwe Haberlandt
Hydrol. Earth Syst. Sci., 28, 1687–1709, https://doi.org/10.5194/hess-28-1687-2024, https://doi.org/10.5194/hess-28-1687-2024, 2024
Short summary
Short summary
River flow data are often provided as mean daily flows (MDF), in which a lot of information is lost about the actual maximum flow or instantaneous peak flows (IPF) within a day. We investigate the error of using MDF instead of IPF and identify means to predict IPF when only MDF data are available. We find that the average ratio of daily flood peaks and volumes is a good predictor, which is easily and universally applicable and requires a minimum amount of data.
Ross Pidoto and Uwe Haberlandt
Hydrol. Earth Syst. Sci., 27, 3957–3975, https://doi.org/10.5194/hess-27-3957-2023, https://doi.org/10.5194/hess-27-3957-2023, 2023
Short summary
Short summary
Long continuous time series of meteorological variables (i.e. rainfall, temperature) are required for the modelling of floods. Observed time series are generally too short or not available. Weather generators are models that reproduce observed weather time series. This study extends an existing station-based rainfall model into space by enforcing observed spatial rainfall characteristics. To model other variables (i.e. temperature) the model is then coupled to a simple resampling approach.
Bora Shehu and Uwe Haberlandt
Hydrol. Earth Syst. Sci., 27, 2075–2097, https://doi.org/10.5194/hess-27-2075-2023, https://doi.org/10.5194/hess-27-2075-2023, 2023
Short summary
Short summary
Design rainfall volumes at different duration and frequencies are necessary for the planning of water-related systems and facilities. As the procedure for deriving these values is subjected to different sources of uncertainty, here we explore different methods to estimate how precise these values are for different duration, locations and frequencies in Germany. Combining local and spatial simulations, we estimate tolerance ranges from approx. 10–60% for design rainfall volumes in Germany.
Bora Shehu, Winfried Willems, Henrike Stockel, Luisa-Bianca Thiele, and Uwe Haberlandt
Hydrol. Earth Syst. Sci., 27, 1109–1132, https://doi.org/10.5194/hess-27-1109-2023, https://doi.org/10.5194/hess-27-1109-2023, 2023
Short summary
Short summary
Rainfall volumes at varying duration and frequencies are required for many engineering water works. These design volumes have been provided by KOSTRA-DWD in Germany. However, a revision of the KOSTRA-DWD is required, in order to consider the recent state-of-the-art and additional data. For this purpose, in our study, we investigate different methods and data available to achieve the best procedure that will serve as a basis for the development of the new KOSTRA-DWD product.
Ross Pidoto, Nejc Bezak, Hannes Müller-Thomy, Bora Shehu, Ana Claudia Callau-Beyer, Katarina Zabret, and Uwe Haberlandt
Earth Surf. Dynam., 10, 851–863, https://doi.org/10.5194/esurf-10-851-2022, https://doi.org/10.5194/esurf-10-851-2022, 2022
Short summary
Short summary
Erosion is a threat for soils with rainfall as the driving force. The annual rainfall erosivity factor quantifies rainfall impact by analysing high-resolution rainfall time series (~ 5 min). Due to a lack of measuring stations, alternatives for its estimation are analysed in this study. The best results are obtained for regionalisation of the erosivity factor itself. However, the identified minimum of 60-year time series length suggests using rainfall generators as in this study as well.
Anne Bartens and Uwe Haberlandt
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2021-466, https://doi.org/10.5194/hess-2021-466, 2021
Preprint withdrawn
Short summary
Short summary
River flow data is often provided as mean daily flow (MDF), in which a lot of information is lost about the actual maximum flow or instantaneous peak flow (IPF) within a day. We investigate the error of using MDFs instead of IPFs and identify means to predict IPFs when only MDF data is available. We find that the average ratio of daily flood peaks and volumes is a good predictor, which is easily and universally applicable and requires a minimum amount of data.
Anne Fangmann and Uwe Haberlandt
Hydrol. Earth Syst. Sci., 23, 447–463, https://doi.org/10.5194/hess-23-447-2019, https://doi.org/10.5194/hess-23-447-2019, 2019
Short summary
Short summary
Low-flow events are little dynamic in space and time. Thus, it is hypothesized that models can be found, based on simple statistical relationships between low-flow metrics and meteorological states, that can help identify potential low-flow drivers. In this study we assess whether such relationships exist and whether they can be applied to predict future low flow within regional climate change impact assessment in the northwestern part of Germany.
Ehsan Rabiei, Uwe Haberlandt, Monika Sester, Daniel Fitzner, and Markus Wallner
Hydrol. Earth Syst. Sci., 20, 3907–3922, https://doi.org/10.5194/hess-20-3907-2016, https://doi.org/10.5194/hess-20-3907-2016, 2016
Short summary
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The value of using moving cars for rainfall measurement purposes (RCs) was investigated with laboratory experiments by Rabiei et al. (2013). They analyzed the Hydreon and Xanonex optical sensors against different rainfall intensities. A continuous investigation of using RCs with the derived uncertainties from laboratory experiments for areal rainfall estimation as well as implementing the data in a hydrological model are addressed in this study.
Uwe Haberlandt and Christian Berndt
Proc. IAHS, 373, 81–85, https://doi.org/10.5194/piahs-373-81-2016, https://doi.org/10.5194/piahs-373-81-2016, 2016
U. Haberlandt and I. Radtke
Hydrol. Earth Syst. Sci., 18, 353–365, https://doi.org/10.5194/hess-18-353-2014, https://doi.org/10.5194/hess-18-353-2014, 2014
E. Rabiei, U. Haberlandt, M. Sester, and D. Fitzner
Hydrol. Earth Syst. Sci., 17, 4701–4712, https://doi.org/10.5194/hess-17-4701-2013, https://doi.org/10.5194/hess-17-4701-2013, 2013
Related subject area
Subject: Urban Hydrology | Techniques and Approaches: Stochastic approaches
The role of storm scale, position and movement in controlling urban flood response
Event-based stochastic point rainfall resampling for statistical replication and climate projection of historical rainfall series
Statistical analysis of hydrological response in urbanising catchments based on adaptive sampling using inter-amount times
Partitioning the impacts of spatial and climatological rainfall variability in urban drainage modeling
Local impact analysis of climate change on precipitation extremes: are high-resolution climate models needed for realistic simulations?
Downscaling future precipitation extremes to urban hydrology scales using a spatio-temporal Neyman–Scott weather generator
Stochastic rainfall analysis for storm tank performance evaluation
Marie-Claire ten Veldhuis, Zhengzheng Zhou, Long Yang, Shuguang Liu, and James Smith
Hydrol. Earth Syst. Sci., 22, 417–436, https://doi.org/10.5194/hess-22-417-2018, https://doi.org/10.5194/hess-22-417-2018, 2018
Short summary
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The effect of storm scale and movement on runoff flows in urban catchments remains poorly understood due to the complexity of urban land use and man-made infrastructure. In this study, interactions among rainfall, urbanisation and peak flows were analyzed based on 15 years of radar rainfall and flow observations. We found that flow-path networks strongly smoothed rainfall peaks. Unexpectedly, the storm position relative to impervious cover within the basins had little effect on flow peaks.
Søren Thorndahl, Aske Korup Andersen, and Anders Badsberg Larsen
Hydrol. Earth Syst. Sci., 21, 4433–4448, https://doi.org/10.5194/hess-21-4433-2017, https://doi.org/10.5194/hess-21-4433-2017, 2017
Short summary
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Time series of rainfall are developed in order to represent future climate conditions. These series can be used in design of, for example, drainage systems where future rainfall loads are important to account for. The climate projections are evaluated on a number of key statistical parameters of rainfall such as yearly and seasonal precipitation amounts, number of extreme events and rainfall intensities, specific duration, and return periods.
Marie-Claire ten Veldhuis and Marc Schleiss
Hydrol. Earth Syst. Sci., 21, 1991–2013, https://doi.org/10.5194/hess-21-1991-2017, https://doi.org/10.5194/hess-21-1991-2017, 2017
Short summary
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In this paper we analysed flow measurements from 17 watersheds in a (semi-)urban region, to characterise flow patterns according to basin features. Instead of sampling flows at fixed time intervals, we looked at how fast given amounts of flow were accumulated. By doing so, we could identify patterns of flow regulation in urban streams and quantify flashiness of hydrological response. We were able to show that in this region, higher urbanisation was clearly associated with lower basin flashiness.
Nadav Peleg, Frank Blumensaat, Peter Molnar, Simone Fatichi, and Paolo Burlando
Hydrol. Earth Syst. Sci., 21, 1559–1572, https://doi.org/10.5194/hess-21-1559-2017, https://doi.org/10.5194/hess-21-1559-2017, 2017
Short summary
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We investigated the relative contribution of the spatial versus climatic rainfall variability for flow peaks by applying an advanced stochastic rainfall generator to simulate rainfall for a small urban catchment and simulate flow dynamics in the sewer system. We found that the main contribution to the total flow variability originates from the natural climate variability. The contribution of spatial rainfall variability to the total flow variability was found to increase with return periods.
Hossein Tabari, Rozemien De Troch, Olivier Giot, Rafiq Hamdi, Piet Termonia, Sajjad Saeed, Erwan Brisson, Nicole Van Lipzig, and Patrick Willems
Hydrol. Earth Syst. Sci., 20, 3843–3857, https://doi.org/10.5194/hess-20-3843-2016, https://doi.org/10.5194/hess-20-3843-2016, 2016
Hjalte Jomo Danielsen Sørup, Ole Bøssing Christensen, Karsten Arnbjerg-Nielsen, and Peter Steen Mikkelsen
Hydrol. Earth Syst. Sci., 20, 1387–1403, https://doi.org/10.5194/hess-20-1387-2016, https://doi.org/10.5194/hess-20-1387-2016, 2016
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Fine-resolution spatio-temporal precipitation data are important as input to urban hydrological models to assess performance issues under all possible conditions. In the present study synthetic data at very fine spatial and temporal resolution are generated using a stochastic model. Data are generated for both present and future climate conditions. The results show that it is possible to generate spatially distributed data at resolutions relevant for urban hydrology.
I. Andrés-Doménech, A. Montanari, and J. B. Marco
Hydrol. Earth Syst. Sci., 14, 1221–1232, https://doi.org/10.5194/hess-14-1221-2010, https://doi.org/10.5194/hess-14-1221-2010, 2010
Cited articles
Ayzel, G., Scheffer, T., and Heistermann, M.: RainNet v1.0: a convolutional neural network for radar-based precipitation nowcasting, Geosci. Model Dev., 13, 2631–2644, https://doi.org/10.5194/gmd-13-2631-2020, 2020.
Bartels, H., Weigl, E., Reich, T., Lang, P., Wagner, A., Kohler, O.,
Gerlach, N., and MeteoSolutions GmbH: Projekt RADOLAN – Routineverfahren zur Online-Aneichung der Radarniederschlagsdaten mit Hilfe von automatischen Bodenniederschlagsstationen (Ombrometer), Zusammenfassender Abschlussbericht für die Projektlaufzeit von 1997 bis 2004, http://dwd.de (last access: 25 February 2022), 2004.
Berenguer, M., Surcel, M., Zawadzki, I., Xue, M., and Kong, F.: The diurnal
cycle of precipitation from continental radar mosaics and numerical weather
prediction models. Part II: Intercomparison among numerical models and with
Nowcasting, Mon. Weather Rev., 140, 2689–2705,
https://doi.org/10.1175/MWR-D-11-00181.1, 2012.
Berndt, C., Rabiei, E., and Haberlandt, U.: Geostatistical merging of rain
gauge and radar data for high temporal resolutions and various station
density scenarios, J. Hydrol., 508, 88–101,
https://doi.org/10.1016/j.jhydrol.2013.10.028, 2014.
Berne, A., Delrieu, G., Creutin, J. D., and Obled, C.: Temporal and spatial
resolution of rainfall measurements required for urban hydrology, J.
Hydrol., 299, 166–179, https://doi.org/10.1016/S0022-1694(04)00363-4, 2004.
Bowler, N. E., Pierce, C. E., and Seed, A. W.: STEPS: A probabilistic
precipitation forecasting scheme which merges an extrapolation nowcast with
downscaled NWP, Q. J. Roy. Meteor. Soc., 132, 2127–2155,
https://doi.org/10.1256/qj.04.100, 2006.
Codo, M. and Rico-Ramirez, M. A.: Ensemble radar-based rainfall forecasts
for urban hydrological applications, Geosci., 8, 297,
https://doi.org/10.3390/geosciences8080297, 2018.
Dixon, M. and Wiener, G.: TITAN: thunderstorm identification, tracking,
analysis, and nowcasting – a radar-based methodology, J. Atmos. Ocean.
Technol., 10, 785–797, https://doi.org/10.1175/1520-0426(1993)010<0785:TTITAA>2.0.CO;2, 1993.
Foresti, L. and Seed, A.: On the spatial distribution of rainfall nowcasting
errors due to orographic forcing, Meteorol. Appl., 22, 60–74, 2015.
Foresti, L., Reyniers, M., Seed, A., and Delobbe, L.: Development and verification of a real-time stochastic precipitation nowcasting system for urban hydrology in Belgium, Hydrol. Earth Syst. Sci., 20, 505–527, https://doi.org/10.5194/hess-20-505-2016, 2016.
Galeati, G.: A comparison of parametric and non-parametric methods for
runoff forecasting, Hydrol. Sci. J., 35, 79–94,
https://doi.org/10.1080/02626669009492406, 1990.
Germann, U. and Zawadzki, I.: Scale Dependence of the Predictability of
Precipitation from Continental Radar Images. Part II: Probability Forecasts,
J. Appl. Meteorol., 43, 74–89, https://doi.org/10.1175/1520-0450(2004)043<0074:SDOTPO>2.0.CO;2, 2004.
Germann, U., Zawadzki, I., and Turner, B.: Predictability of precipitation
from continental radar images. Part IV: Limits to prediction, J. Atmos.
Sci., 63, 2092–2108, https://doi.org/10.1175/JAS3735.1, 2006.
Gneiting, T. and Katzfuss, M.: Probabilistic Forecasting, Annu. Rev. Stat.
Its Appl., 1, 125–151, https://doi.org/10.1146/annurev-statistics-062713-085831,
2014.
Goudenhoofdt, E. and Delobbe, L.: Statistical Characteristics of Convective Storms in Belgium Derived from Volumetric Weather Radar Observations, J. Appl. Meteorol. Clim., 52, 918–934, https://doi.org/10.1175/JAMC-D-12-079.1, 2013.
Grecu, M. and Krajewski, W. F.: A large-sample investigation of statistical
procedures for radar based short-term quantitative precipitation
forecasting, J. Hydrol., 239, 69–84,
https://doi.org/10.1016/S0022-1694(00)00360-7, 2000.
Grünewald, U.: Zu Entstehung und Verlauf des extremen
Niederschlags-Abfluss-Ereignisses am 26.07.2008 im Stadtgebiet von Dortmund, Anlagen_13944-09.pdf,
Cottbus, Karlsruhe, Köln, http://dortmund.de (last access: 25 February 2022), 2009.
Han, L., Fu, S., Zhao, L., Zheng, Y., Wang, H., and Lin, Y.: 3D convective
storm identification, tracking, and forecasting – An enhanced TITAN
algorithm, J. Atmos. Ocean. Technol., 26, 719–732,
https://doi.org/10.1175/2008JTECHA1084.1, 2009.
Hand, W. H.: An object-oriented technique for nowcasting heavy showers and
thunderstorms, Meteorol. Appl., 3, 31–41, https://doi.org/10.1002/met.5060030104, 1996.
Hou, J. and Wang, P.: Storm tracking via tree structure representation of
radar data, J. Atmos. Ocean. Technol., 34, 729–747,
https://doi.org/10.1175/JTECH-D-15-0119.1, 2017.
Imhoff, R. O., Brauer, C. C., Overeem, A., Weerts, A. H., and Uijlenhoet, R.:
Spatial and Temporal Evaluation of Radar Rainfall Nowcasting Techniques on
1,533 Events, Water Resour. Res., 56, 1–22, https://doi.org/10.1029/2019WR026723,
2020.
Jacobson, C. R.: Identification and quantification of the hydrological
impacts of imperviousness in urban catchments: A review, J. Environ.
Manage., 92, 1438–1448, https://doi.org/10.1016/j.jenvman.2011.01.018, 2011.
Jasper-Tönnies, A., Hellmers, S., Einfalt, T., Strehz, A., and
Fröhle, P.: Ensembles of radar nowcasts and COSMO-DE-EPS for urban flood
management, Water Sci. Technol., 2017, 27–35, https://doi.org/10.2166/wst.2018.079,
2018.
Jensen, D. G., Petersen, C., and Rasmussen, M. R.: Assimilation of
radar-based nowcast into a HIRLAM NWP model, Meteorol. Appl., 22,
485–494, https://doi.org/10.1002/met.1479, 2015.
Jung, S. H. and Lee, G.: Radar-based cell tracking with fuzzy logic
approach, Meteorol. Appl., 22, 716–730, https://doi.org/10.1002/met.1509, 2015.
Kato, A. and Maki, M.: Localized heavy rainfall near Zoshigaya, Tokyo, Japan
on 5 August 2008 observed by X-band polarimetric radar - Preliminary
analysis, Sci. Online Lett. Atmos., 5, 89–92, https://doi.org/10.2151/sola.2009-023,
2009.
Kato, R., Shimizu, S., Shimose, K. I., Maesaka, T., Iwanami, K., and
Nakagaki, H.: Predictability of meso-ã-scale, localized, extreme heavy
rainfall during the warm season in Japan using high-resolution precipitation
nowcasts, Q. J. Roy. Meteor. Soc., 153, 1406–1420,
https://doi.org/10.1002/qj.3013, 2017.
Kober, K. and Tafferner, A.: Tracking and nowcasting of convective cells
using remote sensing data from radar and satellite, Meteorol. Z.,
18, 75–84, https://doi.org/10.1127/0941-2948/2009/359, 2009.
Krämer, S.: Quantitative Radardatenaufbereitung für die
Niederschlagsvorhersage und die Siedlungsentwässerung, Leibniz
Universität Hannover, ISSN 0343-8090, 2008.
Kyznarová, H. and Novák, P.: CELLTRACK – Convective cell tracking
algorithm and its use for deriving life cycle characteristics, Atmos. Res.,
93, 317–327, https://doi.org/10.1016/j.atmosres.2008.09.019, 2009.
Lall, U. and Sharma, A.: A Nearest Neighbor Bootstrap For Resampling
Hydrologic Time Series, Water Resour. Res., 32, 679–693,
https://doi.org/10.1029/95WR02966, 1996.
Lang, P.: Cell tracking and warning indicators derived from operational radar products, 30th Int. Conf. on Radar Meteorology, Munich, Germany, Amer. Meteor. Soc., 245–247, Paper21678.html, https://ams.confex.com/ (last access: 25 February 2022), 2001.
Lin, C., Vasiæ, S., Kilambi, A., Turner, B., and Zawadzki, I.:
Precipitation forecast skill of numerical weather prediction models and
radar nowcasts, Geophys. Res. Lett., 32, L14801, https://doi.org/10.1029/2005GL023451,
2005.
Lucas, B. and Kanade, T.: Iterative technique of image registration and its application to stereo, in Proceedings of International Joint Conference on Neural Networks, 24–28 August 1981, Vancouver, British Columbia, 674–679, http://www.clemson.edu/cecas/ (last access: 25 February 2022), 1981.
Moseley, C., Berg, P., and Haerter, J. O.: Probing the precipitation life
cycle by iterative rain cell tracking, J. Geophys. Res.-Atmos., 118,
13361–13370, https://doi.org/10.1002/2013JD020868, 2013.
Moseley, C., Henneberg, O., and Haerter, J. O.: A Statistical Model for
Isolated Convective Precipitation Events, J. Adv. Model. Earth Syst., 11, 360–375,
https://doi.org/10.1029/2018MS001383, 2019.
Panziera, L., Germann, U., Gabella, M., and Mandapaka, P. V.: NORA-Nowcasting
of Orographic Rainfall by means of analogues, Q. J. Roy. Meteor. Soc.,
137, 2106–2123, https://doi.org/10.1002/qj.878, 2011.
Pierce, C., Seed, A., Ballard, S., Simonin, D., and Li, Z.: Nowcasting.
Doppler Radar Observations – Weather Radar, Wind Profiler, Ionospheric
Radar, and Other Advanced Applications, edited by: Bech, J. and Chau, J. L., 97–142, https://doi.org/10.5772/39054, 2012.
Pierce, C. E., Ebert, E., Seed, A. W., Sleigh, M., Collier, C. G., Fox, N.
I., Donaldson, N., Wilson, J. W., Roberts, R., and Mueller, C. K.: The
nowcasting of precipitation during Sydney 2000: An appraisal of the QPF
algorithms, Weather Forecast., 19, 7–21,
https://doi.org/10.1175/1520-0434(2004)019<0007:TNOPDS>2.0.CO;2,
2004.
Rossi, P. J., Chandrasekar, V., Hasu, V., and Moisseev, D.: Kalman
filtering-based probabilistic nowcasting of object-oriented tracked
convective storms, J. Atmos. Ocean. Technol., 32, 461–477,
https://doi.org/10.1175/JTECH-D-14-00184.1, 2015.
Ruzanski, E., Chandrasekar, V., and Wang, Y.: The CASA nowcasting system, J.
Atmos. Ocean. Technol., 28, 640–655, https://doi.org/10.1175/2011JTECHA1496.1, 2011.
Schellart, A., Liguori, S., Krämer, S., Saul, A., and Rico-Ramirez, M.
A.: Comparing quantitative precipitation forecast methods for prediction of
sewer flows in a small urban area, Hydrol. Sci. J., 59, 1418–1436,
https://doi.org/10.1080/02626667.2014.920505, 2014.
Sharma, A. and Mehrotra, R.: An information theoretic alternative to model a
natural system using observational information alone, Water Resour. Res.,
50, 650–660, https://doi.org/10.1002/2013WR013845, 2014.
Sharma, A., Mehrotra, R., Li, J., and Jha, S.: A programming tool for
nonparametric system prediction using Partial Informational Correlation and
Partial Weights, Environ. Model. Softw., 83, 271–275, https://doi.org/10.1016/j.envsoft.2016.05.021, 2016.
Shehu, B.: Improving the rainfall nowcasting for fine temporal and spatial
scales suitable for urban hydrology, Leibniz Universität Hannover, ISSN 0343-8090,
2020.
Shehu, B. and Haberlandt, U.: Relevance of merging radar and rainfall gauge
data for rainfall nowcasting in urban hydrology, J. Hydrol., 594, 125931,
https://doi.org/10.1016/j.jhydrol.2020.125931, 2021.
Surcel, M., Zawadzki, I., and Yau, M. K.: A study on the scale dependence of
the predictability of precipitation patterns, J. Atmos. Sci., 72,
216–235, https://doi.org/10.1175/JAS-D-14-0071.1, 2015.
United Nations: World Urbanization Prospects The 2018 Revision, http://un.org (last access: 25 February 2022), 2018.
Van Dijk, E., Van Der Meulen, J., Kluck, J., and Straatman, J. H. M.:
Comparing modelling techniques for analysing urban pluvial flooding, Water
Sci. Technol., 69, 305, https://doi.org/10.2166/wst.2013.699, 2014.
Wilson, J. W., Crook, N. A., Mueller, C. K., Sun, J., and Dixon, M.:
Nowcasting Thunderstorms: A Status Report, B. Am. Meteorol. Soc., 79,
2079–2099, https://doi.org/10.1175/1520-0477(1998)079<2079:NTASR>2.0.CO;2, 1998.
Wilson, J. W., Feng, Y., Chen, M., and Roberts, R. D.: Nowcasting challenges
during the Beijing olympics: Successes, failures, and implications for
future nowcasting systems, Weather Forecast., 25, 1691–1714,
https://doi.org/10.1175/2010WAF2222417.1, 2010.
Winterrath, T., Rosenow, W., and Weigl, E.: On the DWD quantitative
precipitation analysis and nowcasting system for real-time application in
German flood risk management, IAHS-AISH Publ., 351, 323–329, 2012.
Zahraei, A., Hsu, K.-l., Sorooshian, S., Gourley, J. J., Lakshmanan, V.,
Hong, Y., and Bellerby, T.: Quantitative Precipitation Nowcasting: A
Lagrangian Pixel-Based Approach, Atmos. Res., 118, 418–434,
https://doi.org/10.1016/j.atmosres.2012.07.001, 2012.
Zahraei, A., Hsu, K.-l., Sorooshian, S., Gourley, J. J., Hong, Y., and
Behrangi, A.: Short-term quantitative precipitation forecasting using an
object-based approach, J. Hydrol., 483, 1–15,
https://doi.org/10.1016/j.jhydrol.2012.09.052, 2013.
Zawadzki, I. I.: Statistical Properties of Precipitation Patterns, J. Appl.
Meteorol., 12, 459–472, https://doi.org/10.1175/1520-0450(1973)012<0459:spopp>2.0.co;2, 1973.
Zou, X., Dai, Q., Wu, K., Yang, Q., and Zhang, S.: An empirical ensemble
rainfall nowcasting model using multi-scaled analogues, Nat. Hazards,
103, 165–188, https://doi.org/10.1007/s11069-020-03964-3, 2020.
Short summary
In this paper we investigate whether similar storms behave similarly and whether the information obtained from past similar storms can improve storm nowcast based on radar data. Here a nearest-neighbour approach is employed to first identify similar storms and later to issue either a single or an ensemble nowcast based on k most similar past storms. The results indicate that the information obtained from similar storms can reduce the errors considerably, especially for convective storm nowcast.
In this paper we investigate whether similar storms behave similarly and whether the information...