J.A.E. ten Veldhuis
Please Note
31 records found
1
Blooming Boundaries
Zooming in on Plant-Atmosphere Energy Exchange
Impact of rural nature-based solutions in upstream catchments on downstream flood peaks
Using modified soil parameters in plot-scale and catchment-scale models for the Geul catchment
This study simulates the potential of rural nature-based solutions for flood mitigation under extreme rainfall, with a focus on river peak flows in the Geul during the July 2021 event. To this end, the combination of a physics-based plot-scale model (SWAP) and a conceptual distributed catchment model (wflow SBM) is used. The work proceeds by: (i) comparing soil–water process representations in both models ; (ii) performing sensitivity analyses of soil parameters; (iii) designing a rural NbS scenario by modifying soil-hydraulic parameters; and (iv) evaluating the effects of these scenarios on flood hydrographs at the catchment outlet.
SWAP results show that simulated infiltration and overland flow are most sensitive to saturated water content (𝜃𝑠𝑎𝑡) and saturated hydraulic conductivity (K𝑠𝑎𝑡). A two meter sandy soil column would have accommodated the entire July 2021 rainfall, resulting in negligible overland flow. In wflow SBM, sensitivity analysis indicated that simulated flood hydrographs are most influenced by KsatVer, 𝜃𝑟, and 𝜃𝑠. Adjusting 𝜃𝑟 and 𝜃𝑠 in downstream subcatchments could significantly improve the model’s ability to match the observed hydrographs.
Scenario simulations in wflow SBM reveal spatially dependent effects. Downstream interventions have a damping effect on peak flow magnitude, whereas interventions in the upstream part of the Netherlandscan increase it. A catchment-wide rural NbS scenario reduces the downstream peak by approximately 50% and delays the peak by approximately two hours relative to the default model. This modelled delay lies within the observed five-hour offset between the Geul and Meuse peaks in July 2021, suggesting such measures are unlikely to increase flood risk at the confluence via peak synchronization. ...
This study simulates the potential of rural nature-based solutions for flood mitigation under extreme rainfall, with a focus on river peak flows in the Geul during the July 2021 event. To this end, the combination of a physics-based plot-scale model (SWAP) and a conceptual distributed catchment model (wflow SBM) is used. The work proceeds by: (i) comparing soil–water process representations in both models ; (ii) performing sensitivity analyses of soil parameters; (iii) designing a rural NbS scenario by modifying soil-hydraulic parameters; and (iv) evaluating the effects of these scenarios on flood hydrographs at the catchment outlet.
SWAP results show that simulated infiltration and overland flow are most sensitive to saturated water content (𝜃𝑠𝑎𝑡) and saturated hydraulic conductivity (K𝑠𝑎𝑡). A two meter sandy soil column would have accommodated the entire July 2021 rainfall, resulting in negligible overland flow. In wflow SBM, sensitivity analysis indicated that simulated flood hydrographs are most influenced by KsatVer, 𝜃𝑟, and 𝜃𝑠. Adjusting 𝜃𝑟 and 𝜃𝑠 in downstream subcatchments could significantly improve the model’s ability to match the observed hydrographs.
Scenario simulations in wflow SBM reveal spatially dependent effects. Downstream interventions have a damping effect on peak flow magnitude, whereas interventions in the upstream part of the Netherlandscan increase it. A catchment-wide rural NbS scenario reduces the downstream peak by approximately 50% and delays the peak by approximately two hours relative to the default model. This modelled delay lies within the observed five-hour offset between the Geul and Meuse peaks in July 2021, suggesting such measures are unlikely to increase flood risk at the confluence via peak synchronization.
Wind Machines for Frost Damage Mitigation
Experimental and numerical investigations
Among various mitigation methods, wind machines are potentially cost-effective and energy-efficient. However, little is known about the warming effectiveness of wind machines and the physical mechanisms behind the warming process. Therefore, the primary motivation of this thesis is to investigate whether wind machines are effective warming devices for future frost damage mitigation. However, current physical understanding of machine-inducedwarming remains limited. Experimental studies often face challenges with the coverage and resolution of measurements, which are typically insufficient to fully capture the temporal and spatial variability of machine-induced air mixing in orchards. Furthermore, there are only a few numerical studies available. The dynamic interplay between turbulent warming plumes and canopy structure, as well as the heterogeneous plant-air heat exchange in the orchard, has not been investigated numerically so far.... ...
Among various mitigation methods, wind machines are potentially cost-effective and energy-efficient. However, little is known about the warming effectiveness of wind machines and the physical mechanisms behind the warming process. Therefore, the primary motivation of this thesis is to investigate whether wind machines are effective warming devices for future frost damage mitigation. However, current physical understanding of machine-inducedwarming remains limited. Experimental studies often face challenges with the coverage and resolution of measurements, which are typically insufficient to fully capture the temporal and spatial variability of machine-induced air mixing in orchards. Furthermore, there are only a few numerical studies available. The dynamic interplay between turbulent warming plumes and canopy structure, as well as the heterogeneous plant-air heat exchange in the orchard, has not been investigated numerically so far....
Deep Learning and Earth Observation for the Study of West African Rainfall
Observing rainfall processes through the lens of AI
This dissertation aims at improving rainfall information for farmers in the Sudanian Savanna bioclimatic region of West Africa. The Sudanian Savanna stretches across Africa as a broad belt, covering roughly from southern Mali in the north to northern Ghana in the south. Its West African area expands from Senegal in the west to Chad in the easte. Improving rainfall information will support climate resilience and food and economic safety in the region. This research leverages on the unique potential of Earth Observation satellites to provide rainfall information everywhere, due to their global coverage and ability to track atmospheric processes. To tackle the general poor performance of existing rainfall information products, this work proposes an alternative avenue. Particularly, it investigates the potential of Deep Learning (DL) methods to extract relationships between meteorological variables and raw satellite data that might be overlooked by traditional satellite rainfall retrieval methods.... ...
This dissertation aims at improving rainfall information for farmers in the Sudanian Savanna bioclimatic region of West Africa. The Sudanian Savanna stretches across Africa as a broad belt, covering roughly from southern Mali in the north to northern Ghana in the south. Its West African area expands from Senegal in the west to Chad in the easte. Improving rainfall information will support climate resilience and food and economic safety in the region. This research leverages on the unique potential of Earth Observation satellites to provide rainfall information everywhere, due to their global coverage and ability to track atmospheric processes. To tackle the general poor performance of existing rainfall information products, this work proposes an alternative avenue. Particularly, it investigates the potential of Deep Learning (DL) methods to extract relationships between meteorological variables and raw satellite data that might be overlooked by traditional satellite rainfall retrieval methods....
First, it provides an overview of local farming practices in the Sudanian region of West Africa, alongside farmers' perspectives on climate change and the adaptive measures they use. The findings are based on interviews with local farmers in the region and discussions with research institutes and regional agencies involved in climate change, adaptation, and agricultural water management. Two main approaches were used during the interviews: semi-structured individual interviews based on a questionnaire and group discussions. The investigation revealed that farmers are acutely aware of the changing climate and its negative impact on crop production. The traditional practice of sowing after the first two rainfalls has become increasingly unreliable under current climate conditions. There is a consensus among farmers that the rainfall total has decreased, the duration of the season is shortening, and there is a high frequency of dry spells throughout the rainy season. Additionally, there is a notable lack of climate-based services to support farmers' decision-making processes. Consequently, smallholder farmers expressed a strong interest in receiving not only weather forecasts but also climate risk information, which is crucial for making agriculture in the region more resilient to climate change.
Chapter 3 examines various sowing strategies used in the rainfed farming system of West Africa, where intermittent dry spells during the rainy season exacerbate challenges and affect crop yield response. In the context of a changing climate, we hypothesize that the traditional focus on the onset of the season to start sowing leads to crop losses in years of high rainfall intermittency. Using AquaCrop, an FAO crop model, we simulate the crop response to varying water availability to sowing dates ranging from the 1st of May to the 30th of November at 20 locations in WA. The crop we focus on is maize (Zea mays L.). The analysis revealed that sowing directly after the first rains carries a higher risk of yield loss due to insufficient buildup of soil water storage to overcome dry spells. Based on three years of data per station on average between 2016 and 2020, various sowing strategies were evaluated. We identified safe sowing windows across the Sudanian region that secure optimal yield in 97% of all cases. We find that delaying sowing to mid-June (savanna and western part of the region) and to July (semi-arid region) ensures optimal yields. Of the three commonly applied local onset approaches covered in our evaluation, only the local onset LO10mm, defined as four consecutive days with 10 mm/day, achieves a similar yield result. The advantage of the safe sowing window approach is that it is easily accessible for smallholder farmers, who in many cases do not have access to local rainfall information.
Chapter 4 focuses on identifying sowing strategies that minimize yield losses at the regional level. Climate variability poses great challenges to farmers in the region who are heavily dependent on rainfall for farming. Hence, we investigate three sowing strategies available in the Sudanian region of West Africa (WA) to assess their ability to ensure crop yields for smallholder farmers under a changing climate. AquaCrop-GIS, the GIS version of the FAO crop model, is used to simulate the yield response of maize (Zea mays L.) to varying sowing dates (1st of May to 30th of November) throughout the rainy season across WA. Based on an average of 38 years of data per grid cell from the Global Precipitation Climatology Centre (GPCC), we identify safe sowing windows across the Sudanian region that secure at least 90% of maximal yield. The analysis revealed that the current sowing strategies, based on minimum thresholds for rainfall accumulated over a period, widely applied in the region, carry a higher risk of yield failure than the safe sowing window strategy, especially at the beginning of the rainy season. It also appears that delaying sowing for a month to mid-June in the central region (east of Lon 8.5°W), and to early August in the semi-arid areas is a safe strategy for smallholder farmers that ensures optimal yields. A long-term comparison between the periods 1982-1991 and 1992-2019 reveals earlier sowing dates for both LO10mm and LO20mm, indicating a shift towards a wetter regime relative to the reference period. In contrast, the safe sowing window strategy shows later sowing dates, underscoring the need for caution due to erratic early-season rainfall and variability beyond the control period defined by local sowing practices. The precipitation-based strategies hold a higher risk of yield failure compared to the safe sowing window strategy, which is more accessible to smallholder farmers and better suited to the current climate conditions.
The key findings of this dissertation contribute to regional efforts in building a climate-resilient agricultural system by equipping smallholder farmers with simple yet effective sowing strategies. The research recommendations offer practical, easily implementable solutions for smallholder farmers across West Africa. Given the dynamic nature of rainfall distribution and the uncertainty in future climate projections for West Africa, it is essential to strengthen regional initiatives that improve access to rainfall data and climate services. These efforts will equip farmers with the tools and knowledge needed to make informed decisions. As our understanding of rainfall patterns evolves, updating these recommendations will be crucial to mitigating the negative effects of dry spells and enhancing crop productivity across the region. Additionally, regional efforts should prioritize enhancing and expanding climate and weather monitoring infrastructure to improve our understanding of the region’s complex weather systems at a finer scale. This will enable more precise modeling of the intricate weather-crop-soil interactions and provide localized information to smallholder farmers. Leveraging crop simulation models will facilitate the exploration of both current and future scenarios, helping to identify the most efficient farming practices. This will ultimately improve water use efficiency and contribute to closing the food security gap. ...
First, it provides an overview of local farming practices in the Sudanian region of West Africa, alongside farmers' perspectives on climate change and the adaptive measures they use. The findings are based on interviews with local farmers in the region and discussions with research institutes and regional agencies involved in climate change, adaptation, and agricultural water management. Two main approaches were used during the interviews: semi-structured individual interviews based on a questionnaire and group discussions. The investigation revealed that farmers are acutely aware of the changing climate and its negative impact on crop production. The traditional practice of sowing after the first two rainfalls has become increasingly unreliable under current climate conditions. There is a consensus among farmers that the rainfall total has decreased, the duration of the season is shortening, and there is a high frequency of dry spells throughout the rainy season. Additionally, there is a notable lack of climate-based services to support farmers' decision-making processes. Consequently, smallholder farmers expressed a strong interest in receiving not only weather forecasts but also climate risk information, which is crucial for making agriculture in the region more resilient to climate change.
Chapter 3 examines various sowing strategies used in the rainfed farming system of West Africa, where intermittent dry spells during the rainy season exacerbate challenges and affect crop yield response. In the context of a changing climate, we hypothesize that the traditional focus on the onset of the season to start sowing leads to crop losses in years of high rainfall intermittency. Using AquaCrop, an FAO crop model, we simulate the crop response to varying water availability to sowing dates ranging from the 1st of May to the 30th of November at 20 locations in WA. The crop we focus on is maize (Zea mays L.). The analysis revealed that sowing directly after the first rains carries a higher risk of yield loss due to insufficient buildup of soil water storage to overcome dry spells. Based on three years of data per station on average between 2016 and 2020, various sowing strategies were evaluated. We identified safe sowing windows across the Sudanian region that secure optimal yield in 97% of all cases. We find that delaying sowing to mid-June (savanna and western part of the region) and to July (semi-arid region) ensures optimal yields. Of the three commonly applied local onset approaches covered in our evaluation, only the local onset LO10mm, defined as four consecutive days with 10 mm/day, achieves a similar yield result. The advantage of the safe sowing window approach is that it is easily accessible for smallholder farmers, who in many cases do not have access to local rainfall information.
Chapter 4 focuses on identifying sowing strategies that minimize yield losses at the regional level. Climate variability poses great challenges to farmers in the region who are heavily dependent on rainfall for farming. Hence, we investigate three sowing strategies available in the Sudanian region of West Africa (WA) to assess their ability to ensure crop yields for smallholder farmers under a changing climate. AquaCrop-GIS, the GIS version of the FAO crop model, is used to simulate the yield response of maize (Zea mays L.) to varying sowing dates (1st of May to 30th of November) throughout the rainy season across WA. Based on an average of 38 years of data per grid cell from the Global Precipitation Climatology Centre (GPCC), we identify safe sowing windows across the Sudanian region that secure at least 90% of maximal yield. The analysis revealed that the current sowing strategies, based on minimum thresholds for rainfall accumulated over a period, widely applied in the region, carry a higher risk of yield failure than the safe sowing window strategy, especially at the beginning of the rainy season. It also appears that delaying sowing for a month to mid-June in the central region (east of Lon 8.5°W), and to early August in the semi-arid areas is a safe strategy for smallholder farmers that ensures optimal yields. A long-term comparison between the periods 1982-1991 and 1992-2019 reveals earlier sowing dates for both LO10mm and LO20mm, indicating a shift towards a wetter regime relative to the reference period. In contrast, the safe sowing window strategy shows later sowing dates, underscoring the need for caution due to erratic early-season rainfall and variability beyond the control period defined by local sowing practices. The precipitation-based strategies hold a higher risk of yield failure compared to the safe sowing window strategy, which is more accessible to smallholder farmers and better suited to the current climate conditions.
The key findings of this dissertation contribute to regional efforts in building a climate-resilient agricultural system by equipping smallholder farmers with simple yet effective sowing strategies. The research recommendations offer practical, easily implementable solutions for smallholder farmers across West Africa. Given the dynamic nature of rainfall distribution and the uncertainty in future climate projections for West Africa, it is essential to strengthen regional initiatives that improve access to rainfall data and climate services. These efforts will equip farmers with the tools and knowledge needed to make informed decisions. As our understanding of rainfall patterns evolves, updating these recommendations will be crucial to mitigating the negative effects of dry spells and enhancing crop productivity across the region. Additionally, regional efforts should prioritize enhancing and expanding climate and weather monitoring infrastructure to improve our understanding of the region’s complex weather systems at a finer scale. This will enable more precise modeling of the intricate weather-crop-soil interactions and provide localized information to smallholder farmers. Leveraging crop simulation models will facilitate the exploration of both current and future scenarios, helping to identify the most efficient farming practices. This will ultimately improve water use efficiency and contribute to closing the food security gap.
The objective of this report is to calibrate the sap flow and subsequently investigate the effects of stresses, such as salinity, drought and leaf removal on transpiration in order to enhance irrigation strategies. Calibration was initially conducted by comparing daily sap flow with transpiration estimated by a water balance model using linear regression analysis. The corrected sap flow for the controlled and treated gutter was then compared to investigate the impact of stresses on transpiration.
The corrected sap flow coefficients were 2.30, 1.76, 1.64 and 3.58 for the controlled plants (1 and 2) and the treated plants (1 and 2), respectively. The corrected sap flow may be employed as an indicator of transpiration. It has been observed that salinity levels and a reduction in leaf area result in a decrease in transpiration, particularly when transpiration rates are already high. There was no significant difference in transpiration even when irrigation was reduced to 33% of the original amount. In the event of salinity, drought and leaf area reduction, it is recommended that the irrigation frequency be increased and the irrigation amount be reduced. Furthermore, it is recommended that salt leaching during the non-planting period be undertaken. ...
The objective of this report is to calibrate the sap flow and subsequently investigate the effects of stresses, such as salinity, drought and leaf removal on transpiration in order to enhance irrigation strategies. Calibration was initially conducted by comparing daily sap flow with transpiration estimated by a water balance model using linear regression analysis. The corrected sap flow for the controlled and treated gutter was then compared to investigate the impact of stresses on transpiration.
The corrected sap flow coefficients were 2.30, 1.76, 1.64 and 3.58 for the controlled plants (1 and 2) and the treated plants (1 and 2), respectively. The corrected sap flow may be employed as an indicator of transpiration. It has been observed that salinity levels and a reduction in leaf area result in a decrease in transpiration, particularly when transpiration rates are already high. There was no significant difference in transpiration even when irrigation was reduced to 33% of the original amount. In the event of salinity, drought and leaf area reduction, it is recommended that the irrigation frequency be increased and the irrigation amount be reduced. Furthermore, it is recommended that salt leaching during the non-planting period be undertaken.
The Penman-Monteith model was originally designed for open-field conditions, while the Stanghellini model was specifically developed for greenhouse environments. In this study, the accuracy of these models in estimating transpiration was evaluated by comparing their estimated values with measured transpiration data. By affecting the VPD and stomatal resistance, temperature directly impacts the rate of transpiration in plants. This research also addresses a significant gap in previous studies by determining the optimal observation height for temperature data, which is essential for accurate modeling of transpiration.
Linear regression analysis was employed to assess the performances of the models. The results show that the Stanghellini model provides more precise estimations of transpiration compared to the Penman-Monteith model under greenhouse conditions. Moreover, using temperatures measured above the top of the plant canopy improves the accuracy of tran- spiration estimations in both models. Enhancing the accuracy of transpiration models in greenhouse conditions is critical for promoting efficient water management practices. ...
The Penman-Monteith model was originally designed for open-field conditions, while the Stanghellini model was specifically developed for greenhouse environments. In this study, the accuracy of these models in estimating transpiration was evaluated by comparing their estimated values with measured transpiration data. By affecting the VPD and stomatal resistance, temperature directly impacts the rate of transpiration in plants. This research also addresses a significant gap in previous studies by determining the optimal observation height for temperature data, which is essential for accurate modeling of transpiration.
Linear regression analysis was employed to assess the performances of the models. The results show that the Stanghellini model provides more precise estimations of transpiration compared to the Penman-Monteith model under greenhouse conditions. Moreover, using temperatures measured above the top of the plant canopy improves the accuracy of tran- spiration estimations in both models. Enhancing the accuracy of transpiration models in greenhouse conditions is critical for promoting efficient water management practices.
...
method which is a widely applied statistical technique by satellite rainfall products like Climate Hazards Group InfraRed Precipitation with Station data (CHIRPS) and Tropical Applications of
Meteorology using SATellite data (TAMSAT) that are specifically designed for Africa.
WV inhibition of low-level features assures the correct depiction of strong convective motions usually related to heavy rainfall which is crucial in tropical areas where convective rainfall is dominant. The addition of WV 7.3m is particularly beneficial in North Ghana as tropical systems
are advecting dry air from the nearby Sahara desert creating discontinuities in precipitation events which translates into dry intrusions and dry slots seen in the images of the WV channel.
The developed Deep learning model showed strong performances in binary classification where it outperformed IMERG-Final false alarms count resulting in lower rainfall overestimation (FBias < 2.0), although further research is needed to overcome the very poor relation between GEO-IR images and actual rainfall estimates at the surface. ...
method which is a widely applied statistical technique by satellite rainfall products like Climate Hazards Group InfraRed Precipitation with Station data (CHIRPS) and Tropical Applications of
Meteorology using SATellite data (TAMSAT) that are specifically designed for Africa.
WV inhibition of low-level features assures the correct depiction of strong convective motions usually related to heavy rainfall which is crucial in tropical areas where convective rainfall is dominant. The addition of WV 7.3m is particularly beneficial in North Ghana as tropical systems
are advecting dry air from the nearby Sahara desert creating discontinuities in precipitation events which translates into dry intrusions and dry slots seen in the images of the WV channel.
The developed Deep learning model showed strong performances in binary classification where it outperformed IMERG-Final false alarms count resulting in lower rainfall overestimation (FBias < 2.0), although further research is needed to overcome the very poor relation between GEO-IR images and actual rainfall estimates at the surface.
This research constitutes an attempt to assess the dry spell patterns in the northern region of Ghana, near Burkina Faso. We aim to develop a model which by exploiting satellite products overcomes the poor temporal and spatial coverage of existing ground precipitation measurements. For this purpose 14 meteorological stations featuring different temporal coverage are used together with satellite-based precipitation products.
Conventional machine-learning and deep-learning algorithms were compared in an attempt to establish a link between satellite products and field rainfall data for dry spell assessment. The deep-learning architecture used should be able to efficiently manipulate spatial data. Hence, Convolutional Neural Networks were used in order to detect spatial patterns in the satellite data.
Using these models we will attempt to exploit the long temporal coverage of the satellite products in order to overcome the poor temporal and spatial coverage of existing ground precipitation measurements. Doing that, our final objective is to enhance our knowledge about the dry spell characteristics and, thus, provide more reliable climatic information to the farmers in the area of Northern Ghana. ...
This research constitutes an attempt to assess the dry spell patterns in the northern region of Ghana, near Burkina Faso. We aim to develop a model which by exploiting satellite products overcomes the poor temporal and spatial coverage of existing ground precipitation measurements. For this purpose 14 meteorological stations featuring different temporal coverage are used together with satellite-based precipitation products.
Conventional machine-learning and deep-learning algorithms were compared in an attempt to establish a link between satellite products and field rainfall data for dry spell assessment. The deep-learning architecture used should be able to efficiently manipulate spatial data. Hence, Convolutional Neural Networks were used in order to detect spatial patterns in the satellite data.
Using these models we will attempt to exploit the long temporal coverage of the satellite products in order to overcome the poor temporal and spatial coverage of existing ground precipitation measurements. Doing that, our final objective is to enhance our knowledge about the dry spell characteristics and, thus, provide more reliable climatic information to the farmers in the area of Northern Ghana.
Soccer Fields as Rainfall Detectors using Machine Learning
The case of Ghana
In this study, the problems in representing discharge in HTESSEL can be summarized in three aspects: mismatch in peaks, slower recession,and the monthly delay. Thus, the aim of this research is to investigate the reasons of the poor performance in HTESSEL, and provide possible suggestions for a better fit. Therefore, the hydrological models HBV and GR4J (that operate on catchment scales) are introduced to identify the problems in HTESSEL by model comparison.
HTESSEL, HBV and GR4J models are used to simulate river discharge in 15 catchments are compared in terms of structure and parameterization. HTESSEL use tabulated parameter values, while HBV and GR4J are calibrated to match observations firstly. In order to investigate the influence of different model processes and parameters, a second calibration of the HBV and GR4J parameters is applied. Here, the model parameters are calibrated to the HTESSEL model output. Comparing the two calibration results, the parameter differences can be identified.
The results show that the soil column in HTESSEL is a key factor that influences the surface and subsurface runoff. On the one hand, HBV and GR4J can reproduce the slower falling limb in humid region by increasing their slow reservoirs. On the other hand, the top 50 cm of soil column is the effective depth that influences maximum infiltration rate. Thus, the changing of effective depth and the parameterization of orography variable b, which influences the fast runoff in HTESSEL, are necessary in temperate and mediterranean catchments.
According to this study, to solve the problem of mismatch in peaks this 50cm should be a spatial variable firstly. The increase of effective depth could overcome the overestimation in some places and the decrease of effective depth could overcome the underestimation of peaks in other places. In addition to effective depth, optimizing parameter b is also necessary, because it influences the fast runoff. Moreover, for the problem of slower recession and monthly delay, decreasing the size of soil column in HTESSEL is one way to get a better fit. Thus, in future, more study could focus on the interplay of the soil infiltration capacity and the fast runoff parameters. It might be helpful to improve the simulation.
...
In this study, the problems in representing discharge in HTESSEL can be summarized in three aspects: mismatch in peaks, slower recession,and the monthly delay. Thus, the aim of this research is to investigate the reasons of the poor performance in HTESSEL, and provide possible suggestions for a better fit. Therefore, the hydrological models HBV and GR4J (that operate on catchment scales) are introduced to identify the problems in HTESSEL by model comparison.
HTESSEL, HBV and GR4J models are used to simulate river discharge in 15 catchments are compared in terms of structure and parameterization. HTESSEL use tabulated parameter values, while HBV and GR4J are calibrated to match observations firstly. In order to investigate the influence of different model processes and parameters, a second calibration of the HBV and GR4J parameters is applied. Here, the model parameters are calibrated to the HTESSEL model output. Comparing the two calibration results, the parameter differences can be identified.
The results show that the soil column in HTESSEL is a key factor that influences the surface and subsurface runoff. On the one hand, HBV and GR4J can reproduce the slower falling limb in humid region by increasing their slow reservoirs. On the other hand, the top 50 cm of soil column is the effective depth that influences maximum infiltration rate. Thus, the changing of effective depth and the parameterization of orography variable b, which influences the fast runoff in HTESSEL, are necessary in temperate and mediterranean catchments.
According to this study, to solve the problem of mismatch in peaks this 50cm should be a spatial variable firstly. The increase of effective depth could overcome the overestimation in some places and the decrease of effective depth could overcome the underestimation of peaks in other places. In addition to effective depth, optimizing parameter b is also necessary, because it influences the fast runoff. Moreover, for the problem of slower recession and monthly delay, decreasing the size of soil column in HTESSEL is one way to get a better fit. Thus, in future, more study could focus on the interplay of the soil infiltration capacity and the fast runoff parameters. It might be helpful to improve the simulation.
Delft Meet Regen
Onderzoek naar de dagelijkse neerslagspreiding in Delft op basis van de neerslagdata van Delft Meet Regen
Hierna is het onderzoeksgebied ingedeeld in de volgende vier gebieden: noordwest, noordoost, zuidwest en zuidoost. Van deze gebieden zijn de dagelijkse gemiddelden, aantal metingen, standaard afwijkingen en de dagelijkse gemiddelden cumulatief met elkaar vergeleken. Dit is gedaan doormiddel van grafieken, staafdiagrammen en ruimtelijke plots. Hieruit is geconcludeerd dat er sprake is van gemiddelde dagelijkse neerslagverschillen tussen de gebieden, maar dat er geen sprake is van een patroon. Het aantal metingen per gebied verschilt per dag en dit heeft invloed op de nauwkeurigheid van de resultaten. Hoe meer metingen er beschikbaar zijn, hoe nauwkeuriger de resultaten zullen zijn... ...
Hierna is het onderzoeksgebied ingedeeld in de volgende vier gebieden: noordwest, noordoost, zuidwest en zuidoost. Van deze gebieden zijn de dagelijkse gemiddelden, aantal metingen, standaard afwijkingen en de dagelijkse gemiddelden cumulatief met elkaar vergeleken. Dit is gedaan doormiddel van grafieken, staafdiagrammen en ruimtelijke plots. Hieruit is geconcludeerd dat er sprake is van gemiddelde dagelijkse neerslagverschillen tussen de gebieden, maar dat er geen sprake is van een patroon. Het aantal metingen per gebied verschilt per dag en dit heeft invloed op de nauwkeurigheid van de resultaten. Hoe meer metingen er beschikbaar zijn, hoe nauwkeuriger de resultaten zullen zijn...
Quantifying flood damage
A case-study in Kumasi, Ghana