In recent years, climate change has intensified the frequency of severe rainfall events, raising concerns, particularly in urban areas where impervious surfaces dominate. The resultant reliance on man-made drainage increases pluvial flooding risks, threatening infrastructure and urban resilience. As the global population increasingly shifts to urban living, the vulnerability to flooding grows. Understanding how areas respond to rainfall is crucial for proactive flood risk mitigation. Available hydrological models offer insights and predictions, but are often linked with long simulation times and high computational cost. Semi-distributed models, like the Spatially Distributed Travel Time (SDTT) approach, offer simplified model formulations suitable for screening applications. This thesis extends Ekeroth's (2022) SDTT model for watershed delineation and travel time formulations, focusing on ensemble runs of multi-input rainfall/infiltration scenarios. As there is often many uncertain factors in hydrological modeling, there is a need for faster models capable of generating a distribution of scenarios to represent the uncertainty of real systems. Even a quick and simple model should account for the multifaceted aspects of urban flooding, including rainfall-infiltration dynamics and the variations in rainfall intensity. Script modules were developed to analyze rainfall severity, peak discharge distribution, and parameter impact efficiently. In three urban watersheds with an average size of 0.45 km2, 120 scenarios distinguished by intensity distribution, rainfall duration, soil composition of pervious areas, and antecedent moisture conditions, were simulated within approximately 3.5 minutes, enabling comprehensive hydrological analysis. The successful implementation of the new modules implicate a promising tool for hydrological risk-screening analysis in urban environments, although further research should investigate incorporating probability-based scenarios and bigger input rainfall datasets. / Under senare år har klimatförändringarna intensifierat förekomsten av skyfall, något som är särskilt oroväckande i stadsområden där marktäckningen huvudsakligen består av hårdgjorda ytor. Genom att asfaltera och bygga försvinner markens naturliga infiltrationsförmåga. Detta leder till ett ökat beroende av konstgjorda dräneringssystem som sällan är dimensionerade för särskilt intensiva regnhändelser. Urbana översvämningar innebär inte bara ett hot mot infrastruktur och den bebyggda miljön, men den globala befolkningens ökade bosättning i urbana områden medför att sårbarheten vid översvämningar ökar även den. För att kunna hantera översvämningsrisken i ett urbant område är förståelse för avrinningsområdets respons till ett skyfall viktigt. Det finns hydrologiska modeller på marknaden som erbjuder prognoser, men dessa är oftast baserade på komplexa fysiska beskrivningar som medför långa processtider och beräkningskostnader. Samtidigt finns nytänkande modeller som skär ner på processtiderna genom att minska den spatiala upplösningen på beräkningarna, såsom SDTT (Spatially Distributed Travel Time) formuleringen, som erbjuder förenklade analyser lämpliga som screeningverktyg. Denna studie utvidgar Ekeroths (2022) SDTT-modell med fokus på ensemblekörningar av regn- och infiltrationsscenarier. Eftersom det ofta finns flertalet osäkra faktorer i hydrologisk modellering finns ett behov av snabbare modeller som kan genera en fördelning av möjliga utfall givet olika scenarier. Samtidigt behöver även en snabb och enkel modell beakta de mångfacetterade aspekterna av urbana översvämningar, exempelvis gällande dynamiken mellan regn och infiltration och skyfallsegenskaper. Kodmoduler utvecklades för att effektivt analysera utfallen av regnscenarierna och att finna de mest allvarliga händelserna, fördelningen av värden inom de simulerade utfallen, samt inflytandet från parametrarna som definierar scenarierna. I tre urbana avrinningsområden med en genomsnittlig storlek på 0.45 km2 simulerades 120 scenarier inom 3,5 minuter, vilket möjliggör hydrologisk analys på en hanterbar tid. Implementeringen av de nya modulerna pekar mot ett lovande verktyg för hydrologisk risk-screeninganalys i urbana miljöer. Samtidigt bör framtida studier fortsatt undersöka möjligheten att inkludera sannolikhetsbaserade scenarier och körning av större dataset.

Water infrastructures have been implemented to support the vital activities of human society. The infrastructure developments at the same time have interrupted the natural catchment response characteristics, challenging society to implement effective water resources planning and management strategies. The Telemark area in southern Norway has seen a large number of water infrastructure developments, particularly hydropower, over more than a century. Recent developments in decision support tools for flood control and reservoir operation has raised the need to compute inflows from local catchments, most of which are regulated or have no observed data. This has contributed for the motivation of this PhD thesis work, with an aim of improving runoff estimation at ungauged catchments, and the research results are presented in four manuscript scientific papers.  The inverse distance weighting, inverse distance squared weighting, ordinary kriging, universal kriging and kriging with external drift were applied to analyse precipitation variability and estimate daily precipitation in the study area. The geostatistical based univariate and multivariate map-correlation concepts were applied to analyse and physically understand regional hydrological response patterns. The Sobol variance based sensitivity analysis (VBSA) method was used to investigate the HBV hydrological model parameterization significances on the model response variations and evaluate the model’s reliability as a prediction tool. The HBV hydrological model space transferability into ungauged catchments was also studied.  The analyses results showed that the inverse distance weighting variants are the preferred spatial data interpolation methods in areas where relatively dense precipitation station network can be found.  In mountainous areas and in areas where the precipitation station network is relatively sparse, the kriging variants are the preferred methods. The regional hydrological response correlation analyses suggested that geographic proximity alone cannot explain the entire hydrological response correlations in the study area. Besides, when the multivariate map-correlation analysis was applied, two distinct regional hydrological response patterns - the radial and elliptical-types were identified. The presence of these hydrological response patterns influenced the location of the best-correlated reference streamgauges to the ungauged catchments. As a result, the nearest streamgauge was found the best-correlated in areas where the radial-type hydrological response pattern is the dominant. In area where the elliptical-type hydrological response pattern is the dominant, the nearest reference streamgauge was not necessarily the best-correlated. The VBSA verified that varying up to a minimum of four to six influential HBV model parameters can sufficiently simulate the catchments' responses characteristics when emphasis is given to fit the high flows. Varying up to a minimum of six influential model parameters is necessary to sufficiently simulate the catchments’ responses and maintain the model performance when emphasis is given to fit the low flows. However, varying more than nine out of the fifteen HBV model parameters will not make any significant change on the model performance.  The hydrological model space transfer study indicated that estimation of representative runoff at ungauged catchments cannot be guaranteed by transferring model parameter sets from a single donor catchment. On the other hand, applying the ensemble based model space transferring approach and utilizing model parameter sets from multiple donor catchments improved the model performance at the ungauged catchments. The result also suggested that high model performance can be achieved by integrating model parameter sets from two to six donor catchments. Objectively minimizing the HBV model parametric dimensionality and only sampling the sensitive model parameters, maintained the model performance and limited the model prediction uncertainty.