06 Fakultät Luft- und Raumfahrttechnik und Geodäsie
Permanent URI for this collectionhttps://elib.uni-stuttgart.de/handle/11682/7
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Item Open Access Development of a model predictive controller for floating offshore wind turbines(2020) Nann, SamuelIn this work, an Economic Model Predictive Controller for a floating offshore wind turbine is presented. The classical Model Predictive Control for floating offshore wind turbines provides promising results. In addition, research on onshore wind turbines revealed the potential of the economic control method, which can improve the closed-loop behavior and simplify the control design in comparison to the classical version of this control method. The aim of this work is, to develop a novel Economic Model Predictive Controller for a floating offshore wind turbine based on these two research results. A simplified low order model of a floating offshore wind turbine serves as a basis for the controller design. Including the disturbance preview and constraints, the controller computes optimal trajectories for the blade pitch and the generator torque. To apply the control technique to a floating offshore wind turbine two things have to be done: Firstly, the cost function is designed, to fulfill the main objectives of, maximizing the generated power and alleviating the structural fatigues. Secondly, the constraints are integrated into the control problem. After selecting a suitable solver, the controller is discretized and scaled, thus a proper implementation and smooth operation is possible. Afterwards, the successful functioning of the algorithm, a multi-objective optimization is done, to find appropriate weights to adjust the cost function for the required objectives. Finally, the developed controller is tested with realistic wind and wave disturbances. A significant reduction of the standard deviation of the generated power can be shown, while maintaining real time capability. Furthermore, the structural fatigues of the tower and the platform are decreased.Item Open Access Exploring the performances of SAR altimetry and improvements offered by fully focused SAR(2021) Wu, YuweiWith the development of the altimetry techniques, the measurement principle has been changed from the conventional pulse-limited principle to the delay-Doppler principle since CryoSat-2. The delay-Doppler altimetry presents scientists with the chance to develop new processing schemes and improve products that maximize the benefits of the measurements. Nevertheless, one of the challenges for delay-Doppler Altimetry lies in the complexity of the post-processing, especially the Delay-Doppler processing. The focus of this thesis is to better understand delay-Doppler and fully focused SAR altimetry. This thesis compares the retrieved waveforms and resultant water level time series with different altimetry principles, processing options and retracking methods. By using platform SARvatore for delay-Doppler altimetry and SMAP for fully focused SAR altimetry, different processing options (data posting rate, Hamming window and zero padding) and different retrackers (SAMOSA family for SARvatore, PTR for SMAP) can be applied and compared. Our results reveal that the waveforms generated by different configurations have different peaks for SARvatore. For SMAP, with or without zero padding or Hamming window had very little impact, with more differences mainly coming from the different retracking methods. Our results also show that fully focused SAR does not bring a significant improvement when applied to Sentinel-3 data. In summary, different configurations and retracking methods can significantly affect the shape of waveforms and their derived ranges. According to this thesis's experiments, the configuration with 80 Hz data posting rate, Hamming window, zero padding, extended receiving window and retracker SAMOSA++ offers the best performance.Item Open Access Characterizing storage-based drought using satellite gravimetry(2021) Saemian, PeymanDrought is a complex phenomenon leading to a wide range of socio-economic, environmental, and political problems. The storage-based drought which represents the persistent lack of water in different levels of the Total Water Storage (TWS) from deep groundwater to surface water plays a vital role in proactive drought management. Despite its necessity, TWS could not be monitored due to the lack of consistent measurements from regional to continental scale. Since its launch in 2002, the Gravity Recovery and Climate Experiment (grace) mission and its successor GRACE Follow-On have provided unique observations of the TWS change at the global scale. In this study, we have investigated characterizing the storage-based drought at the global scale using GRACE measurements. To this end, the Equivalent Water Height (EWH) has been retrieved from GRACE level 02 solutions. We have addressed the short record of GRACE observations in capturing the full hydroclimate variations. Based on our analysis, regions with a considerable direct human intervention like overexploitation of groundwater in the Middle East, regions that were affected by climate change like ice-melting over the Mackenzie river basin in Canada, or extreme precipitation events over the Ob river basin in the boreal regions are more sensitive to the length of ewh time series. Due to the crucial need for a long (at least 30 years) record of EWH, we have extended GRACE observations back to 1980 using an ensemble of models. The extended dataset has been developed using a pixel-wise selection of best-performed models among global hydrological models, land surface models, and atmospheric reanalysis models. The extended dataset has been used in the study for drought characterization over the grac period. The proposed Storage-based Drought Index (SDI) successfully captured the documented drought events globally in terms of intensity and spatio-temporal distribution. Moreover, the analysis of SDI over the five classes of drought from D0 as abnormally dry to D4 as exceptional drought showed that most regions have suffered at least once from the storage-based drought over the GRACE period (2002–2016). Besides, the map of exceptional drought frequency highlights regions with significant groundwater extraction like California, the Middle East, and north of India and regions with exceptional shifts in the precipitation and temperature pattern and intensity like Amazon in South America and China. Finally, our comparison of SDI with three most widely used drought indices namely the Standardized Precipitation Index (SPI), the Standardized Precipitation Evapotranspiration Index (SPEI), and the Palmer Drought Severity Index (PDSI) reveals that despite their high correlation over climate-driven regions, these indices failed to characterize anthropogenic drought events, especially over regions with considerable groundwater withdraws. The study allows for a more informative storage-based drought with a more robust climatology as the reference, thus enabling a more realistic risk assessment.Item Open Access Analysis of water volume change of the lakes and reservoirs in the Mississippi River basin using Landsat imagery and satellite altimetry(2021) Wang, LingkeIn recent years, the demand for freshwater has been steadily increasing owing to population growth and economic expansion. Surface waters such as lakes and reservoirs function as a dominant factor in mankind's freshwater provision. Analysis of changes in their water storage is consequently vital for understanding of the global water cycle and water resources. However, the water volume changes in lakes or reservoirs cannot be measured directly from space, but can be inferred from lake areas and lake water levels. Lake area can be measured globally from space but lake water level is not easy to be obtained globally. Because the number of in situ stations is few, and in situ data are only accessible for some lakes with few measurement epochs, despite in situ stations can measure lake water level and provide high accuracy observations. Although the altimetry technique can generate the time series of the water level for the majority of lakes, they are not global coverage due to the distance between satellite tracks and the gap between different missions. Therefore, in situ data and satellite altimetry measurements of water levels of lakes and reservoirs are not always available. For example, there are only 22 lakes or reservoirs in this study covered by satellite altimetry or in situ stations out of 90 research cases in Mississippi River Basin. Then, in case of unavailable in situ data or altimetry measurements, this research proposes an alternative method to estimate the water level through Digital Elevation Model (DEM). Because satellite imagery offers global coverage and DEM is the global digital representation of the land surface elevation with respect to any reference datum, this study allows for the evaluation of global water volume changes by acquiring lake area data from space and lake height data from DEM. Therefore, the objective of this study is that changes in water volume in lakes or reservoirs can be successfully monitored even when in situ data and satellite altimetry measurements are not available for lakes or reservoirs. Hereby, we investigate 90 lakes and reservoirs in the Mississippi River Basin and develop an alternative remote sensing technique to monitor the water volume changes by combining the improved water mask with DEM. Meanwhile, we propose practical methods to detect the shoreline pixels of the water body from improved water mask. Given the assumption that all pixels in the shoreline should have the same height, four water level estimation models are developed, including water level estimation model based on statistical analysis, frequency maps, change pixels and pixel pair analysis. To this end, the study estimates the time series of lake height from water level estimation model and obtains the time series of lake surface area from HydroSat. Subsequently, this study builds the unique function between the lake water level and the lake surface area and then develops the function between the lake water volume change and the lake surface area. Finally, this study analyses the water volume changes of lakes and reservoirs in the Mississippi River Basin using this alternative remote sensing method. Four water level estimation models are proposed and evaluated. They are respectively based on statistical analysis, frequency maps, change pixels and pixel pair analysis. As a result of their actions, the first model based on statistical analysis, with an average correlation of 0.62 and an average RMSE of 0.91 meters, functions in the majority of situations and demonstrates excessive outlier removal in some cases. The second model based on frequency maps is more general than the first, with an average correlation of 0.66 and an average RMSE of 1.11 meters. The average correlation for the third model based on change pixels is 0.71, and the average RMSE is 0.99 meters. The resulting model based on pixel pair analysis obtains a mean correlation of 0.67 and a mean RMSE of 1.00 meters. Finally, these models behave differently in different seasons, so they exhibit distinct monthly behaviour. To conclude, the above validation results show that this alternative method can be used in different lakes and reservoirs in case of absence of water level observation data, and achieve to monitor the water volume changes during a long period.Item Open Access Item Open Access Evaluate the performance of a camber controlled cycloidal rotor(2022) Huang, DoudouThe curvature of the airfoil has a significant effect on the performance of the cycloidal rotor system. This paper aims to improve the aerodynamic performance of the cycloidal rotor system by utilizing dynamical morphing blades in a CFD model. Particularly, three different camber morphing concepts, including leading edge deflection, trailing edge deformation, and cambered NACA profile, are employed to a baseline 2-bladed system with rotating and pitching NACA0015 aerofoils. Based on these three camber concepts, a series of URANS 2-D numerical simulations in OpenFOAM are conducted for blades with different morphing degrees and positions. The simulation results verified that the flow field condition could be optimized and thus significant improvement in thrust and efficiency could be achieved by properly tuning the morphing control.Item Open Access Gravity gradients of prompt elasto-gravity signals : Aspects of their simulation and the possibility to measure them : A case study for the Tohoku-Oki earthquake(2020) Bützler, ClaraSobald der Bruch eines Erdbebens beginnt, fangen seismische Wellen an, sich auszubreiten. Diese verändern die Dichteverteilung in der Erde, was zu einer Änderung der Gravitation führt. Diese Änderung breitet sich mit Lichtgeschwindigkeit aus und ist somit viel schneller als die seismischen Wellen. Das führt dazu, dass bereits vor dem Einsatz der P-Welle so genannte prompt elasto-gravity Signale (PEGS) mit Gravimetern und Seismometern gemessen werden können. Die Detektion dieser Signale wird allerdings dadurch erschwert, dass Gravimeter und Seismometer nicht nur die genannte Änderung der Schwere messen, sondern auch eine Bodenbeschleunigung, die durch eben diese Schwereänderung verursacht wird. Diese Signale heben sich teilweise gegenseitig auf. Daher wäre es von Vorteil, Messinstrumente zu verwenden, die sensitiv für Schwereänderungen, aber nicht für Bodenbeschleunigungen sind. Diese Eigenschaft erfüllen Gravitationsdehnungsmesser (gravity strainmeter) und Schweregradiometer (gravity gradiometer). In dieser Arbeit geht es um das Potential von Schweregradiometern für die Detektion von PEGS. Es werden zunächst zwei Methoden zur Modellierung von Schweregradienten von PEGS untersucht und getestet: Die Methode von Harms (2016), welche ein stark vereinfachtes Erdmodell verwendet, kann erfolgreich angewendet werden. Die Umsetzung einer abgewandelten Form der Normalmodensummation, mit der Schweregradienten von PEGS für ein deutlich genaueres Erdmodell berechnet werden können, scheitert hingegen an der Berechnung von Normalmoden für hohe Frequenzen. Daher wird die Methode von Harms (2016) verwendet, um Schweregradienten von PEGS für das Tohoku-Oki Beben zu simulieren. Die Ergebnisse werden mit den Rauschspektren aktueller Schweregradiometer verglichen. Es zeigt sich, dass die Detektion von PEGS des Tohoku-Oki Bebens auf Grund der unzureichenden Genauigkeit der Instrumente mit aktuellen Schweregradiometern nicht möglich gewesen wäre. Auch mit solchen Schweregradiometern, welche gerade in der Entwicklung sind, stellt sich die Detektion von PEGS als sehr schwierig heraus. Für eine eindeutige Detektion von PEGS müsste die Genauigkeit von Schweregradiometern ungefähr zehnmal höher sein als die derer, welche aktuell entwickelt werden. Zurzeit sollten daher für die Untersuchung von PEGS die Messdaten von Seismometern und Gravimetern verwendet werden. In Zukunft können eventuell außerdem Gravitationsdehnungsmesser verwendet werden. Diese werden vor allem für die Detektion von Gravitationswellen entwickelt. Ihr Potential für die Detektion von PEGS wurde bereits in anderen Arbeiten untersucht.Item Open Access Item Open Access Understanding the hydrological signature in gravity data(2023) Schollmeier, PhilippOver the past two decades, the subsequent advancements in Superconducting Gravimeters (SGs) have ushered in a level of precision that enables the measurement of the impact of ground water and soil water on gravity. Because of the challenging nature of monitoring the total water volume and the relatively subtle amplitude of the hydrological signal, a comprehensive understanding of the precise hydrological signature in continuous gravity data remains elusive. In this study, I use SG data in conjunction with hydrological measurements from a geoscientific observatory in Germany to find the signature of hydrological signals in gravity data. I scrutinize the various steps involved in extracting this signal, presenting new methodologies, including a technique to eliminate oscillations in gravity residuals that are likely attributed to remaining tidal signals due to an imperfect tidal model. A major contribution of this work involves constructing a data-driven model that incorporates precipitation and soil moisture measurements to elucidate gravity variations. I address critical questions such as the impact of utilizing soil moisture data on the model’s performance, determining the optimal model for achieving the closest fit with gravity measurements, and assessing the applicability of computed model parameters to new epochs. Furthermore, I provide recommendations for refining the model-building process in future investigations. Results show that a convolution of the different hydrological timeseries with one half of a Gaussian bell curve leads to a strong agreement with the gravity measurements. The use of soil moisture data significantly improves the fit, especially when the measurement stations are spatially well distributed. This fit becomes less strong when the computed parameters are applied to new events, but the approach showed promise for some of the events. Enhancing our comprehension of the hydrological influence on gravity measurements holds promising implications, potentially positioning SGs as instruments for monitoring soil and ground water in the future. Moreover, this improved understanding could elevate the pre cision of analyzing other subtle signals, such as the effects of Polar Motion.Item Open Access Understanding the limitations of Sentinel-3 inland altimetry through validation over the Rhine River(2022) Schneider, Nicholas M.Satellite altimetry is developing into one of the most powerful measurement techniques for long-term water body monitoring thanks to its high spatial resolution and its increasing level of precision. Although the principle of satellite altimetry is very straightforward, the retrieval of correct water levels remains rather difficult due to various factors. Waveform retracking is an approach to optimize the initially determined range between the satellite and the water body on Earth by exploiting the information within the power-signal of the returned radar pulse to the altimeter. Several so-called retrackers have been designed to this end, yet remain one of the most open study areas in satellite altimetry due to their crucial role they play in water level retrieval. Moreover, geophysical properties of the stratified atmosphere and the target on Earth have an effect on the travel time of the transmitted radar pulse and can amount to severalmeters in range. In this study we provide an overall analysis of the performances of the retrackers dedicated to the Sentinel-3 mission and the applied geophysical corrections. For this matter, we focus on nine different locations within the Rhine River basin where locally gauged data is available to validate the Sentinel-3 level-2 products. Furthermore, we present a reverse retracking approach in the sense that we use the given in-situ data to determine the offset to each altimetry-derived measurement of every epoch. Under the assumption that these offsets are legitimate, they can be seen as an a-posteriori correction which we project onto the range and thus on a waveform level. Further analyses consist in the investigation of the relationship these a-posteriori corrections have to the waveform properties of the same epoch. Later, the question whether the a-posteriori corrections to the initial retracking gates are appropriate for the retrieval of correct water levels, drives us to assign a probability to each and every bin of the waveform. Following this idea, we design stochastic-based retrackers which determine the retracking gate for water level retrieval from the bin with the highest probability assigned to it. To distribute the probabilities across all bins of the waveform, we consider three empirical approaches that take both the waveform itself and its first derivative into account: Addition, multiplication and maximum of both signals. For all three of the new retrackers, we generate the water level timeseries over the aforementioned sites and validate them against in-situ data and the retrackers dedicated to the Sentinel-3 mission.