This document provides a summary of a doctoral thesis focused on uncertainty quantification in structural responses of offshore monopile wind turbines. The thesis contains six main parts: (1) introduction to the context, (2) stochastic vs. deterministic approaches, (3) aspects of the research, (4) results, (5) contributions to existing knowledge, and (6) conclusions and future agenda. Three papers are developed as part of the research, focusing on the influence of uncertainties in wave parameters, wind shear, and simulation length on extreme turbine responses. The research finds wave loading to be an important factor and develops methods to quantify sensitivity to input parameter uncertainties and flexible soil modeling.
Meteorological conditions in northern indiaECRD IN
1. The document discusses meteorological conditions and air pollution dispersion modelling in northern India. It emphasizes the importance of understanding local meteorology and collecting location-specific data for accurate modelling.
2. Key meteorological parameters like wind speed, direction, temperature and stability class that influence pollutant dispersion are identified. Reliable modelling requires data on these parameters, especially at the point of emission.
3. Thermal stratification and inversions are significant as they can limit vertical mixing and dispersion of pollutants. Understanding local inversion characteristics is critical for meaningful pollution modelling.
This document discusses meteorological conditions and air pollution dispersion modeling in northern India. It makes three key points:
1) Meteorological conditions are the most critical factor for accurate air pollution dispersion modeling, as they define the movement and spread of pollutants in the atmosphere.
2) Common air pollution dispersion models use a Gaussian equation that requires meteorological data like wind speed, wind direction, and atmospheric stability to calculate pollution concentrations.
3) Thermal stratification and inversions in the lower atmosphere, especially ground-based inversions at night, significantly impact pollutant dispersion and must be understood and characterized for meaningful pollution modeling.
Nuclear winter revisited with a modern climate model and current nuclear arse...Lex Pit
1) A modern climate model was used to simulate the climate effects of injecting 50 Tg and 150 Tg of smoke aerosols into the atmosphere from simulated nuclear conflicts.
2) For the 150 Tg scenario, the black carbon aerosols were lofted into the upper stratosphere where they had an e-folding lifetime of 4.6 years, much longer than previous estimates, producing significant surface cooling for over a decade.
3) Both scenarios produced globally catastrophic consequences according to the researchers, with the 150 Tg scenario still qualifying as a "nuclear winter," though of a longer duration than previously thought.
This research article describes a new method called Surface Temperature Initiated Closure (STIC) that reintroduces radiometric surface temperature into the Penman-Monteith equation for estimating surface sensible and latent heat fluxes. STIC derives analytical solutions for surface and atmospheric conductances, eliminating the need for external submodels. It was tested using high-temporal resolution data from four experimental sites, comparing estimates of latent and sensible heat fluxes to eddy covariance measurements. Results showed root mean square deviations between 7-16% for latent heat flux and 40-74% for sensible heat flux estimates compared to measurements.
The document is Karl Nilsson's doctoral thesis which uses numerical modeling to study wind turbine wakes and wake interactions. It summarizes the key findings of the research which included: 1) validating numerical simulations of the Lillgrund wind farm against power production data, 2) analyzing uncertainties in the rotor modeling approach, and 3) evaluating the impact of including a power controller in the simulations. The research provides insights into modeling wind farm flows and optimizing wind farm layouts.
The document describes models developed to predict soiling-caused photovoltaic (PV) power output degradation in Doha, Qatar based on environmental variables. Field data on PV performance and dust concentration, wind speed, and relative humidity were collected. A linear model and a semi-physical model were developed to correlate daily changes in PV performance (∆CI) with the daily average environmental conditions. The semi-physical model, which considers dust deposition and resuspension processes, predicted daily ∆CI slightly more accurately than the linear model based on R-squared values. However, both models performed roughly the same in predicting ∆CI over longer periods. The results suggest it is possible to use the models to estimate PV
Climate change is projected to impact drastically in southern African during the 21st century
under low mitigation futures (Niang et al., 2014). African temperatures are projected to rise
rapidly, in the subtropics at least at 1.5 times the global rate of temperature increase (James
and Washington, 2013; Engelbrecht et al., 2015). Moreover, the southern African region is
projected to become generally drier under enhanced anthropogenic forcing (Christensen et
al., 2007; Engelbrecht et al., 2009; James and Washington, 2013; Niang et al., 2014). These
changes in temperature and rainfall patterns will plausibly have a range of impacts in South
Africa, including impacts on energy demand (in terms of achieving human comfort within
buildings and factories), agriculture (e.g. reductions of yield in the maize crop under higher
temperatures and reduced soil moisture), livestock production (e.g. higher cattle mortality as
a result of oppressive temperatures) and water security (through reduced rainfall and
enhanced evapotranspiration) (Engelbrecht et al., 2015).
Meteorological conditions in northern indiaECRD IN
1. The document discusses meteorological conditions and air pollution dispersion modelling in northern India. It emphasizes the importance of understanding local meteorology and collecting location-specific data for accurate modelling.
2. Key meteorological parameters like wind speed, direction, temperature and stability class that influence pollutant dispersion are identified. Reliable modelling requires data on these parameters, especially at the point of emission.
3. Thermal stratification and inversions are significant as they can limit vertical mixing and dispersion of pollutants. Understanding local inversion characteristics is critical for meaningful pollution modelling.
This document discusses meteorological conditions and air pollution dispersion modeling in northern India. It makes three key points:
1) Meteorological conditions are the most critical factor for accurate air pollution dispersion modeling, as they define the movement and spread of pollutants in the atmosphere.
2) Common air pollution dispersion models use a Gaussian equation that requires meteorological data like wind speed, wind direction, and atmospheric stability to calculate pollution concentrations.
3) Thermal stratification and inversions in the lower atmosphere, especially ground-based inversions at night, significantly impact pollutant dispersion and must be understood and characterized for meaningful pollution modeling.
Nuclear winter revisited with a modern climate model and current nuclear arse...Lex Pit
1) A modern climate model was used to simulate the climate effects of injecting 50 Tg and 150 Tg of smoke aerosols into the atmosphere from simulated nuclear conflicts.
2) For the 150 Tg scenario, the black carbon aerosols were lofted into the upper stratosphere where they had an e-folding lifetime of 4.6 years, much longer than previous estimates, producing significant surface cooling for over a decade.
3) Both scenarios produced globally catastrophic consequences according to the researchers, with the 150 Tg scenario still qualifying as a "nuclear winter," though of a longer duration than previously thought.
This research article describes a new method called Surface Temperature Initiated Closure (STIC) that reintroduces radiometric surface temperature into the Penman-Monteith equation for estimating surface sensible and latent heat fluxes. STIC derives analytical solutions for surface and atmospheric conductances, eliminating the need for external submodels. It was tested using high-temporal resolution data from four experimental sites, comparing estimates of latent and sensible heat fluxes to eddy covariance measurements. Results showed root mean square deviations between 7-16% for latent heat flux and 40-74% for sensible heat flux estimates compared to measurements.
The document is Karl Nilsson's doctoral thesis which uses numerical modeling to study wind turbine wakes and wake interactions. It summarizes the key findings of the research which included: 1) validating numerical simulations of the Lillgrund wind farm against power production data, 2) analyzing uncertainties in the rotor modeling approach, and 3) evaluating the impact of including a power controller in the simulations. The research provides insights into modeling wind farm flows and optimizing wind farm layouts.
The document describes models developed to predict soiling-caused photovoltaic (PV) power output degradation in Doha, Qatar based on environmental variables. Field data on PV performance and dust concentration, wind speed, and relative humidity were collected. A linear model and a semi-physical model were developed to correlate daily changes in PV performance (∆CI) with the daily average environmental conditions. The semi-physical model, which considers dust deposition and resuspension processes, predicted daily ∆CI slightly more accurately than the linear model based on R-squared values. However, both models performed roughly the same in predicting ∆CI over longer periods. The results suggest it is possible to use the models to estimate PV
Climate change is projected to impact drastically in southern African during the 21st century
under low mitigation futures (Niang et al., 2014). African temperatures are projected to rise
rapidly, in the subtropics at least at 1.5 times the global rate of temperature increase (James
and Washington, 2013; Engelbrecht et al., 2015). Moreover, the southern African region is
projected to become generally drier under enhanced anthropogenic forcing (Christensen et
al., 2007; Engelbrecht et al., 2009; James and Washington, 2013; Niang et al., 2014). These
changes in temperature and rainfall patterns will plausibly have a range of impacts in South
Africa, including impacts on energy demand (in terms of achieving human comfort within
buildings and factories), agriculture (e.g. reductions of yield in the maize crop under higher
temperatures and reduced soil moisture), livestock production (e.g. higher cattle mortality as
a result of oppressive temperatures) and water security (through reduced rainfall and
enhanced evapotranspiration) (Engelbrecht et al., 2015).
Natural Gas Compressibility Factor Correlation Evaluation for Niger Delta Gas...IOSR Journals
This document presents a new natural gas compressibility factor correlation developed specifically for Niger Delta gas fields in Nigeria. Laboratory PVT reports from 22 gas reservoirs in the Niger Delta were compiled into a database and used to evaluate existing compressibility factor correlations. A new correlation was then developed using the database. The performance of the new correlation was found to have the lowest standard error and absolute error compared to other evaluated correlations when calculating z-factors for different Niger Delta reservoir systems. Statistical analysis also showed the new correlation had the highest correlation coefficients and best matched experimental and other estimated z-factor values. It was concluded that the new developed correlation and that of Papay correlation are the most appropriate for calculating natural gas compressibility factors in Niger Delta gas fields
This document summarizes revisions made to the gust effect factor formulation in ASCE7-95 wind load provisions. It discusses concepts of spatial and temporal wind averaging and introduces the new gust effect factor. The factor is derived based on considerations of peak gust wind speeds, turbulence intensity, structure size, and other factors. Examples are provided to illustrate using the new provisions to evaluate gust effect factors for flexible structures.
International Journal of Computational Engineering Research(IJCER) ijceronline
International Journal of Computational Engineering Research(IJCER) is an intentional online Journal in English monthly publishing journal. This Journal publish original research work that contributes significantly to further the scientific knowledge in engineering and Technology.
On March 11, 2016, ICLR held a Friday Forum workshop entitled 'Mapping extreme rainfall statistics for Canada', led by Dr. Slobodan Simonovic of Western University.
Climate change is expected to increase the frequency and intensity of extreme rainfall events, affecting rainfall intensity-duration-frequency (IDF) curve information used in the design, maintenance and operation of water infrastructure in Canada. Presented in this lecture are analyses of precipitation data from 567 Environment Canada hydro-meteorological stations using the IDF_CC tool. Results for the year 2100 based on Canadian climate model and an ensemble of 22 GCMs have been generated. A spatial interpolation method was used to produce Canadian precipitation maps for events of various return periods. Results based on the Canadian climate model indicate a reduction in extreme precipitation in central regions of Canada and increases in other regions. Relative to the ensemble approach, the Canadian climate model results (a) suggest more spatial variability in change of IDFs, and (b) the ensemble approach generated generally lower values than the Canadian climate model.
Dr. Simonovic has extensive research, teaching and consulting experience in water resources systems engineering. He teaches courses in water resources and civil engineering systems. He actively works for national and international professional organizations. Dr. Simonovic’s primary research interest focuses on the application of systems approach to management of complex water and environmental systems. Most of his work is related to the integration of risk, reliability, and uncertainty in hydrology and water resources management. He has received a number of awards for excellence in teaching, research and outreach. He has published over 450 professional publications and three major textbooks. He was inducted to the Canadian Academy of Engineering in June of 2013.
A FINITE ELEMENT PREDICTION MODEL WITH VARIABLE ELEMENT SIZES - KELLEYRichard. Kelley
This document describes a finite element prediction model that uses variable element sizes. The model uses the shallow water equations on a periodic channel with a constant Coriolis parameter. Initial tests were run using a uniform element size as well as abruptly and smoothly varying element sizes. Uniform elements showed good wave propagation but some noise, while varying elements generated more noise. The goal was to develop a model that allows high resolution where needed without discontinuities at element size changes.
Implementation of Wilcox k − ω model to UCNS3DArpit Aggarwal
Arpit Aggarwal implemented the Wilcox k-ω turbulence model in the UCNS3D computational fluid dynamics solver. Validation cases for the RAE-2822 airfoil and flow over a backward-facing step showed good agreement with experimental data and other models. The implementation allows for improved accuracy in complex geometries handled by the UCNS3D solver.
Extinction of Millimeter wave on Two Dimensional Slices of Foam-Covered Sea-s...IJSRED
This document discusses millimeter wave (mmW) extinction due to its interaction with layers of air bubbles (sea foam) on the ocean surface. It presents the following key points:
1) A numerical model using the split-step Fourier method was used to evaluate mmW attenuation through layers of sea foam of varying thickness, frequency, polarization, and incidence angle.
2) Estimates of the effective dielectric constant of sea foam layers were calculated for different foam configurations and WindSat frequencies based on a two-dimensional model of randomly packed air bubbles coated with thin seawater layers.
3) The parabolic wave equation method, which approximates solutions to Maxwell's equations, was discussed as an efficient way to
This document discusses a method for classifying atmospheric circulation patterns (CPs) based on their links to extreme wave events. It proposes using an entropy measure to objectively evaluate the quality of CP classifications and determine the optimal number of CP classes. The method is applied to wave data from Durban, South Africa to classify CPs driving extreme wave heights over 3.5m. The results indicate that 15-20 CP classes are needed for a good quality classification but one persistent class explains a large proportion of extreme events regardless of the number of classes.
International journal of engineering issues vol 2015 - no 2 - paper3sophiabelthome
This document discusses rainfall frequency analysis using L-moments of probability distributions. It analyzes annual maximum daily rainfall data from two locations in India - Narwar and Banswara. It fits three probability distributions to the data - Gumbel, Frechet, and Generalized Extreme Value - using the method of L-moments. It evaluates the fit of the distributions using goodness-of-fit tests and a diagnostic test. The tests show that the Gumbel distribution best fits the Narwar data, while the Generalized Extreme Value distribution best fits the Banswara data.
The USEIT interns ran physics-based earthquake simulations using the RSQSim simulator on the Blue Waters supercomputer. They varied parameters like normal stress, shear stress, and rate-and-state friction coefficients across 17 short catalogs and compared the results to the UCERF3 forecast model. The catalog with increased normal stress of 200 MPa (Sigma High) produced the best match to UCERF3, with less than 2% difference in recurrence intervals for M≥7 events on the San Andreas Fault. This parameter set was used to generate an extended 530,000 year catalog for probabilistic earthquake forecasting.
This document discusses coupling land surface models (LSM) with radiative transfer models (RTM) for assimilating microwave brightness temperature observations over India. It explains that the community microwave emission model is used as the forward operator to relate LSM states like soil moisture to brightness temperatures. An ensemble Kalman filter is used to update LSM states by combining forecasts with observations. Results show assimilating brightness temperatures improves Noah LSM soil moisture simulations compared to open-loop runs. Issues regarding biases and parameter estimation for the RTM are discussed.
The document evaluates the performance of the TRMM Multi-satellite Precipitation Analysis (TMPA) product in estimating daily precipitation in the Central Andes region, compared to gauge measurements. It finds large biases in daily precipitation amounts from TMPA for the regions of Cuzco, Peru and La Paz, Bolivia, though strong precipitation events are generally detected. Correlation with gauge data increases significantly when aggregating TMPA estimates to longer time periods like weekly or monthly sums. Spatial aggregation has little effect on performance. The document proposes blending TMPA with daily gauge data to improve daily estimates.
1) The document analyzes the relationship between extreme precipitation events in the Gulf of Mexico region and climate change indicators like sea surface temperature and atmospheric CO2 levels.
2) It finds a statistically significant relationship, with extreme precipitation events becoming more likely as Gulf SSTs and CO2 levels increase. Using this relationship, it estimates that Hurricane Harvey in 2017 was a "very likely" 1,000-year rainfall event or rarer when accounting for climate change factors.
3) The analysis uses several statistical methods like generalized extreme value distributions and point process models to analyze extreme precipitation event data at different spatial scales and relate the frequency of extreme events to climate change indicators while accounting for seasonal and other factors.
This document summarizes an article from the International Journal of Mechanical Engineering and Technology (IJMET) that examines the effect of particle size and chemical reaction on convective heat and mass transfer of magnetohydrodynamic (MHD) nanofluid flowing in a cylindrical annulus filled with porous material. The article presents governing equations to model the coupled heat and mass transfer, which are solved numerically. Parameters like the Darcy number, Grashof number, Hartmann number, and Nusselt number are defined. The study aims to provide insights into how particle size and chemical reactions impact convective transport for applications like nuclear technology and space systems.
An Introduction to the Environment Agency extreme offshore wave, water level ...Stephen Flood
This document provides an overview of new extreme coastal event datasets produced by the Environment Agency (EA) for use in flood risk analysis. The datasets were generated using multivariate extreme value modeling of offshore wave, wind and water level conditions, which were then transformed to nearshore conditions using wave modeling. The datasets include over 10,000 years of simulated extreme coastal events that can be used in both robust probabilistic flood risk analyses or simplified analyses. Guidance is provided on applying the datasets for local flood studies.
Derivation Of Intensity Duration Frequency Curves Using Short Duration Rainfa...Mohammed Badiuddin Parvez
The estimation of rainfall intensity is commonly required for the design of hydraulic and water resources engineering control structures. The intensity-duration-frequency (IDF) relationship is a mathematical relationship between the rainfall intensity, the duration and the return period. The present study aimed the derivation of IDF curves of Yermarus Raingauge Station of Raichur District with 19 years of rainfall data (1998 to 2016). The Normal Distribution, Log Normal Distribution, Gumbel distribution, Pearson Type III Distribution and Log Pearsons Type III Distribution techniques are used to Find the rainfall intensity values of 2, 5, 10, 15, 30, 60, 120, 720, 1440 minutes of rainfall duration with different return period. Chi Square test was conducted to find the goodness of fit the short duration IDF using daily rainfall data are presented, which is input for water resources projects.
Extreme value distribution to predict maximum precipitationJonathan D'Cruz
The document analyzes extreme rainfall events in Mumbai, India to determine maximum probable precipitation amounts for different return periods. It describes using the Hershfield technique and Gumbel's extreme value theory to analyze 35 years of rainfall data for Mumbai's Colaba region. Calculations determine the probable maximum precipitation is 604.688036 mm based on past data, and estimate maximum one-day rainfall amounts for return periods from 2 to 100 years.
The document provides background information on the COPE field campaign and the goals and instrumentation of the COPE-MED research project. The COPE campaign studied convective storms in southwest England through aircraft and ground-based radar observations. COPE-MED aims to investigate microphysical pathways and entrainment effects on precipitation formation. Key goals are to analyze cloud liquid water content and droplet number concentration measurements from the campaign and examine droplet spectral characteristics during non-precipitating cloud penetrations.
The document provides an introduction to seismology. It discusses magnitude occurrence based on the Gutenberg-Richter law which states that the number of earthquakes decreases exponentially with magnitude. It also discusses the expected largest earthquake in a year based on this relationship. Finally, it notes that the magnitude distribution considers all earthquakes in a data set or catalog, not just aftershocks.
Climate statisticians analyze observational climate data and model simulations to detect trends, attribute causes, and quantify uncertainties. They use statistical methods like linear regression to attribute observed warming to human and natural factors. They also use extreme value theory to describe rare weather events and project how these extremes may change with continued warming. A key task is quantifying various sources of uncertainty in climate projections, like different model sensitivities and emissions scenarios.
Advanced weather forecasting for RES applications: Smart4RES developments tow...Leonardo ENERGY
Recording at: https://youtu.be/45Zpjog95QU
This is the 3rd Smart4RES webinar that will address technological and market challenges in RES prediction and will introduce the Smart4RES strategy to improve weather forecasting models with high resolution.
Through wind and solar applications, Innovative Numerical Weather Prediction and Large-Eddy Simulation approaches will be presented.
Natural Gas Compressibility Factor Correlation Evaluation for Niger Delta Gas...IOSR Journals
This document presents a new natural gas compressibility factor correlation developed specifically for Niger Delta gas fields in Nigeria. Laboratory PVT reports from 22 gas reservoirs in the Niger Delta were compiled into a database and used to evaluate existing compressibility factor correlations. A new correlation was then developed using the database. The performance of the new correlation was found to have the lowest standard error and absolute error compared to other evaluated correlations when calculating z-factors for different Niger Delta reservoir systems. Statistical analysis also showed the new correlation had the highest correlation coefficients and best matched experimental and other estimated z-factor values. It was concluded that the new developed correlation and that of Papay correlation are the most appropriate for calculating natural gas compressibility factors in Niger Delta gas fields
This document summarizes revisions made to the gust effect factor formulation in ASCE7-95 wind load provisions. It discusses concepts of spatial and temporal wind averaging and introduces the new gust effect factor. The factor is derived based on considerations of peak gust wind speeds, turbulence intensity, structure size, and other factors. Examples are provided to illustrate using the new provisions to evaluate gust effect factors for flexible structures.
International Journal of Computational Engineering Research(IJCER) ijceronline
International Journal of Computational Engineering Research(IJCER) is an intentional online Journal in English monthly publishing journal. This Journal publish original research work that contributes significantly to further the scientific knowledge in engineering and Technology.
On March 11, 2016, ICLR held a Friday Forum workshop entitled 'Mapping extreme rainfall statistics for Canada', led by Dr. Slobodan Simonovic of Western University.
Climate change is expected to increase the frequency and intensity of extreme rainfall events, affecting rainfall intensity-duration-frequency (IDF) curve information used in the design, maintenance and operation of water infrastructure in Canada. Presented in this lecture are analyses of precipitation data from 567 Environment Canada hydro-meteorological stations using the IDF_CC tool. Results for the year 2100 based on Canadian climate model and an ensemble of 22 GCMs have been generated. A spatial interpolation method was used to produce Canadian precipitation maps for events of various return periods. Results based on the Canadian climate model indicate a reduction in extreme precipitation in central regions of Canada and increases in other regions. Relative to the ensemble approach, the Canadian climate model results (a) suggest more spatial variability in change of IDFs, and (b) the ensemble approach generated generally lower values than the Canadian climate model.
Dr. Simonovic has extensive research, teaching and consulting experience in water resources systems engineering. He teaches courses in water resources and civil engineering systems. He actively works for national and international professional organizations. Dr. Simonovic’s primary research interest focuses on the application of systems approach to management of complex water and environmental systems. Most of his work is related to the integration of risk, reliability, and uncertainty in hydrology and water resources management. He has received a number of awards for excellence in teaching, research and outreach. He has published over 450 professional publications and three major textbooks. He was inducted to the Canadian Academy of Engineering in June of 2013.
A FINITE ELEMENT PREDICTION MODEL WITH VARIABLE ELEMENT SIZES - KELLEYRichard. Kelley
This document describes a finite element prediction model that uses variable element sizes. The model uses the shallow water equations on a periodic channel with a constant Coriolis parameter. Initial tests were run using a uniform element size as well as abruptly and smoothly varying element sizes. Uniform elements showed good wave propagation but some noise, while varying elements generated more noise. The goal was to develop a model that allows high resolution where needed without discontinuities at element size changes.
Implementation of Wilcox k − ω model to UCNS3DArpit Aggarwal
Arpit Aggarwal implemented the Wilcox k-ω turbulence model in the UCNS3D computational fluid dynamics solver. Validation cases for the RAE-2822 airfoil and flow over a backward-facing step showed good agreement with experimental data and other models. The implementation allows for improved accuracy in complex geometries handled by the UCNS3D solver.
Extinction of Millimeter wave on Two Dimensional Slices of Foam-Covered Sea-s...IJSRED
This document discusses millimeter wave (mmW) extinction due to its interaction with layers of air bubbles (sea foam) on the ocean surface. It presents the following key points:
1) A numerical model using the split-step Fourier method was used to evaluate mmW attenuation through layers of sea foam of varying thickness, frequency, polarization, and incidence angle.
2) Estimates of the effective dielectric constant of sea foam layers were calculated for different foam configurations and WindSat frequencies based on a two-dimensional model of randomly packed air bubbles coated with thin seawater layers.
3) The parabolic wave equation method, which approximates solutions to Maxwell's equations, was discussed as an efficient way to
This document discusses a method for classifying atmospheric circulation patterns (CPs) based on their links to extreme wave events. It proposes using an entropy measure to objectively evaluate the quality of CP classifications and determine the optimal number of CP classes. The method is applied to wave data from Durban, South Africa to classify CPs driving extreme wave heights over 3.5m. The results indicate that 15-20 CP classes are needed for a good quality classification but one persistent class explains a large proportion of extreme events regardless of the number of classes.
International journal of engineering issues vol 2015 - no 2 - paper3sophiabelthome
This document discusses rainfall frequency analysis using L-moments of probability distributions. It analyzes annual maximum daily rainfall data from two locations in India - Narwar and Banswara. It fits three probability distributions to the data - Gumbel, Frechet, and Generalized Extreme Value - using the method of L-moments. It evaluates the fit of the distributions using goodness-of-fit tests and a diagnostic test. The tests show that the Gumbel distribution best fits the Narwar data, while the Generalized Extreme Value distribution best fits the Banswara data.
The USEIT interns ran physics-based earthquake simulations using the RSQSim simulator on the Blue Waters supercomputer. They varied parameters like normal stress, shear stress, and rate-and-state friction coefficients across 17 short catalogs and compared the results to the UCERF3 forecast model. The catalog with increased normal stress of 200 MPa (Sigma High) produced the best match to UCERF3, with less than 2% difference in recurrence intervals for M≥7 events on the San Andreas Fault. This parameter set was used to generate an extended 530,000 year catalog for probabilistic earthquake forecasting.
This document discusses coupling land surface models (LSM) with radiative transfer models (RTM) for assimilating microwave brightness temperature observations over India. It explains that the community microwave emission model is used as the forward operator to relate LSM states like soil moisture to brightness temperatures. An ensemble Kalman filter is used to update LSM states by combining forecasts with observations. Results show assimilating brightness temperatures improves Noah LSM soil moisture simulations compared to open-loop runs. Issues regarding biases and parameter estimation for the RTM are discussed.
The document evaluates the performance of the TRMM Multi-satellite Precipitation Analysis (TMPA) product in estimating daily precipitation in the Central Andes region, compared to gauge measurements. It finds large biases in daily precipitation amounts from TMPA for the regions of Cuzco, Peru and La Paz, Bolivia, though strong precipitation events are generally detected. Correlation with gauge data increases significantly when aggregating TMPA estimates to longer time periods like weekly or monthly sums. Spatial aggregation has little effect on performance. The document proposes blending TMPA with daily gauge data to improve daily estimates.
1) The document analyzes the relationship between extreme precipitation events in the Gulf of Mexico region and climate change indicators like sea surface temperature and atmospheric CO2 levels.
2) It finds a statistically significant relationship, with extreme precipitation events becoming more likely as Gulf SSTs and CO2 levels increase. Using this relationship, it estimates that Hurricane Harvey in 2017 was a "very likely" 1,000-year rainfall event or rarer when accounting for climate change factors.
3) The analysis uses several statistical methods like generalized extreme value distributions and point process models to analyze extreme precipitation event data at different spatial scales and relate the frequency of extreme events to climate change indicators while accounting for seasonal and other factors.
This document summarizes an article from the International Journal of Mechanical Engineering and Technology (IJMET) that examines the effect of particle size and chemical reaction on convective heat and mass transfer of magnetohydrodynamic (MHD) nanofluid flowing in a cylindrical annulus filled with porous material. The article presents governing equations to model the coupled heat and mass transfer, which are solved numerically. Parameters like the Darcy number, Grashof number, Hartmann number, and Nusselt number are defined. The study aims to provide insights into how particle size and chemical reactions impact convective transport for applications like nuclear technology and space systems.
An Introduction to the Environment Agency extreme offshore wave, water level ...Stephen Flood
This document provides an overview of new extreme coastal event datasets produced by the Environment Agency (EA) for use in flood risk analysis. The datasets were generated using multivariate extreme value modeling of offshore wave, wind and water level conditions, which were then transformed to nearshore conditions using wave modeling. The datasets include over 10,000 years of simulated extreme coastal events that can be used in both robust probabilistic flood risk analyses or simplified analyses. Guidance is provided on applying the datasets for local flood studies.
Derivation Of Intensity Duration Frequency Curves Using Short Duration Rainfa...Mohammed Badiuddin Parvez
The estimation of rainfall intensity is commonly required for the design of hydraulic and water resources engineering control structures. The intensity-duration-frequency (IDF) relationship is a mathematical relationship between the rainfall intensity, the duration and the return period. The present study aimed the derivation of IDF curves of Yermarus Raingauge Station of Raichur District with 19 years of rainfall data (1998 to 2016). The Normal Distribution, Log Normal Distribution, Gumbel distribution, Pearson Type III Distribution and Log Pearsons Type III Distribution techniques are used to Find the rainfall intensity values of 2, 5, 10, 15, 30, 60, 120, 720, 1440 minutes of rainfall duration with different return period. Chi Square test was conducted to find the goodness of fit the short duration IDF using daily rainfall data are presented, which is input for water resources projects.
Extreme value distribution to predict maximum precipitationJonathan D'Cruz
The document analyzes extreme rainfall events in Mumbai, India to determine maximum probable precipitation amounts for different return periods. It describes using the Hershfield technique and Gumbel's extreme value theory to analyze 35 years of rainfall data for Mumbai's Colaba region. Calculations determine the probable maximum precipitation is 604.688036 mm based on past data, and estimate maximum one-day rainfall amounts for return periods from 2 to 100 years.
The document provides background information on the COPE field campaign and the goals and instrumentation of the COPE-MED research project. The COPE campaign studied convective storms in southwest England through aircraft and ground-based radar observations. COPE-MED aims to investigate microphysical pathways and entrainment effects on precipitation formation. Key goals are to analyze cloud liquid water content and droplet number concentration measurements from the campaign and examine droplet spectral characteristics during non-precipitating cloud penetrations.
The document provides an introduction to seismology. It discusses magnitude occurrence based on the Gutenberg-Richter law which states that the number of earthquakes decreases exponentially with magnitude. It also discusses the expected largest earthquake in a year based on this relationship. Finally, it notes that the magnitude distribution considers all earthquakes in a data set or catalog, not just aftershocks.
Climate statisticians analyze observational climate data and model simulations to detect trends, attribute causes, and quantify uncertainties. They use statistical methods like linear regression to attribute observed warming to human and natural factors. They also use extreme value theory to describe rare weather events and project how these extremes may change with continued warming. A key task is quantifying various sources of uncertainty in climate projections, like different model sensitivities and emissions scenarios.
Advanced weather forecasting for RES applications: Smart4RES developments tow...Leonardo ENERGY
Recording at: https://youtu.be/45Zpjog95QU
This is the 3rd Smart4RES webinar that will address technological and market challenges in RES prediction and will introduce the Smart4RES strategy to improve weather forecasting models with high resolution.
Through wind and solar applications, Innovative Numerical Weather Prediction and Large-Eddy Simulation approaches will be presented.
This document compares the results of modeling toxic gas dispersion (hydrogen sulfide) using the CFD model PANACHE and the Gaussian plume model PHAST under different atmospheric conditions. The study found that PHAST consistently predicted higher concentrations than PANACHE due to not accounting for plant geometry and turbulence. Dispersion at stable conditions gave higher concentrations than neutral conditions. While PHAST is conservative, PANACHE more accurately models the plant scenario by considering geometry and turbulence. The maximum concentrations at 700m were below safety limits.
This document discusses modeling and simulations of proton exchange membrane (PEM) fuel cells. It describes modeling PEMFCs using macroscale, mesoscale, and microscale approaches. It also discusses using commercial software like ANSYS Fluent to model PEMFC performance, temperature distribution, current density, and other factors. Several case studies are presented modeling different PEMFC geometries and conditions.
- Abiotic controls, like precipitation and evaporation, dominate soil moisture spatiotemporal variability in wet climates, while biotic controls from vegetation become more important in Mediterranean climates.
- The relationship between the coefficient of variation (Cv) and mean soil moisture (Θ) was found to be unique and well described by an exponential or linear function for locations in Switzerland, but strong hysteretic cycles were observed for Mediterranean locations.
- Heterogeneity in soil properties increases Cv and tends to obscure any hysteresis, masking climatic and biotic controls on soil moisture variability. Heterogeneity can therefore hide the influences of climate and vegetation on soil moisture spatiotemporal patterns.
Wind_resource_assessment_using_the_WAsP_software_DTU_Wind_Energy_E_0174_.pdfMohamed Salah
This document provides an introduction to wind resource assessment using the WAsP software. It describes how wind resource assessment is used to estimate the wind resource potential at a site based on meteorological measurements and numerical modelling. The WAsP software implements a wind atlas methodology using measured wind data to generate a generalised wind climate, which can then be applied to a site to produce a predicted wind climate and estimate annual energy production considering wake losses from the wind farm layout. Validation, uncertainties and site conditions are also discussed.
Contribution to the investigation of wind characteristics and assessment of w...Université de Dschang
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Diapositiva - Defensa Tesis Doctorado
1. UNCERTAINTY QUANTIFICATION IN STRUCTURAL RESPONSES OF
OFFSHORE MONOPILE WIND TURBINES
UNIVERSIDAD NACIONAL DE INGENIERÍA
FACULTAD DE INGENIERÍA MECÁNICA
ESCUELA CENTRAL DE POSGRADO
THESIS
SUBMITTED FOR THE DEGREE OF DOCTOR OF SCIENCE IN ENERGY
Presented by: David Barreto Lara
2. 2
Part I. Introduction to the Context
Part II. Stochastic vs. Deterministic
Part III. Aspects of the Research
Part IV. Results
Part V. Contributions to the Existent Knowledge
Part VI. Conclusions & Future Agenda
Content
6. Wind resource is abundant and more stable given the low roughness of the
sea.
More energy per year can be produced , and larger and more powerful
wind turbines can be installed.
6
WHY OFFSHORE?
7. 7
BUT, WHAT IS THE
MAIN LIMITATION?
WHICH ARE THE MAIN
COSTS?
13. 13
UNCERTAINTY QUANTIFICATION
“The process of quantifying uncertainties associated with model calculations of true,
physical quantities of interest (QOIs), with the goals of accounting for all relevant sources
of uncertainty and quantifying the contributions of specific sources to the overall
uncertainty”.
“…quantification of uncertainties is a critical and necessary aspect to facilitate the
reliability-based design of wind turbines. He based his conclusions on an extensive review
of the literature between the 1990s and 2017 on the subject of structural reliability
analysis of wind turbines”.
DEFINITION
IMPORTANCE
“…Uncertainty quantification become essential to advancing computational capabilities
while introducing innovations in the quest toward lower LCOE”
“…it is expected to improve the predictions of the loads/responses associated with
established return periods by controlling the level of uncertainty in the probabilistic
models.”
14. 14
UNCERTAINTY QUANTIFICATION
“…It is closely related to the achievement of a high-level objective within the offshore wind
industry, the lowering of the Levelized Cost of Energy (LCOE) . This is one of the main
issues that hinder the massive deployment of wind energy projects. The objective of
lowering the LCOE can be achieved by minimizing uncertainties in the design process that
could lead to excessive material consumption or reduced operational lifetime since large
uncertainties imply the use of high safety factors.”
18. 18
PROBLEM STATEMENT
“Sensitivity analysis of the effect of wind
characteristics and turbine properties on
wind turbine loads”
(Robertson et al.)
Wave loading Conditionality of
environmental
parameters
Effect of control
actionsLoad probability
distribution
Soil structure
interaction
Simulation
length
WSC
GAPS
GAPS
GAPS
19. 19
RESEARCH OBJECTIVES
RO: Evaluate the influence of uncertainties in input parameters on the extreme responses
of a monopile OWT.
SO1: Investigate the effects of wave parameters uncertainty on the dynamic responses of a
monopile OWT.
SO2: Study the influence of wind shear uncertainty on the dynamic responses of a
monopile OWT.
SO3: Evaluate the impact of uncertainty in the simulation length on the dynamic response
extrapolation process in a monopile OWT.
SO4: Assess the effect of soil-structure interaction uncertainty on the dynamic responses
of a monopile OWT.
MAIN RESEARCH OBJECTIVE (RO)
SPECIFIC OBJECTIVES (SO)
20. 20
CONSIDERATIONS FOR THE RESEARCH
NREL 5 MW
RESPONSE:
Forces
Moments
Displacements
Etc.
FX or FASF
MY or FABM
26. 26
MAIN CHALLENGES
5.-EXTREME VALUE ANALYSIS
Maximun=
Max1
Max2
…
Max (n)
(mG,bG)
Gumbel Coefficients
Short-term distribution
Extrapolated Long-term
distribution
30. 30
SITUATION OF PAPERS
P1 It is already published and indexed in SCOPUS.
P2 It is already accepted, in process to be indexed (between Nov and Dec 2020).
P3 Planned to be submitted on December 2020.
31. 31
PAPER 1 (P1)
The main purpose of this work is to investigate the impact in short-term
responses (variance propagation) when an uncertainty is introduced in
the wave parameters.
CONSIDERATIONS FOR THE ANALYSIS
Seabed (Mudline) is considered the point which better reflects the
combined action of wind and wave.
Only the results for the fore-aft shear force (Fx) and fore-aft bending
moment (My) at mudline are considered for the sensitivity analysis.
33. 33
SENSITIVITY INDEX (S)
Baseline Hs, Tp
Case 1 Hs*, Tp*
Case 2 …..
…
Case 11 ……
Case 12 Hs*, Tp*
𝑺(𝑪𝒂𝒔𝒆) =
𝝈 𝑿 𝒅𝒆𝒓𝒊𝒗𝒆𝒅
𝝈 𝑿 𝒃𝒂𝒔𝒆
− 𝟏 𝒙𝟏𝟎𝟎%
S: Sensitivity Index
𝝈: Standard deviation
Case: Hs, Tp, HsTp
X: Dynamic Response (e. g. Bending Moment at Mudline)
34. 34
RESULTS
Sensitivity plot of Fx for Uw=11.4 m/s
and sea state 4.
Sensitivity plot of My for Uw=25 m/s
and sea state 9.
35. 35
RESULTS
Therefore, the sensitivity indexes can be modeled as:
𝐒 𝐇𝐬 = 𝐀 ∗ 𝛅
𝑺 𝑻𝒑 = 𝑩 𝟏 ∗ 𝜺 𝟐
+ 𝑩 𝟐 ∗ 𝜺
𝑺 𝑯𝒔𝑻𝒑 = 𝑪 𝟏 ∗ 𝜹 𝟐
+ 𝑪 𝟐 ∗ 𝜹
A, B1, B2, C1, C2 : Regression coefficients (SCF) to be determined.
𝜹, 𝜺 : uncertainties in the input data.
S(Hs), S(Tp), S(HsTp): Sensitivity indexes.
37. 37
RESULTS
Environmental Contour Line (ECL) : Dashed
Selected Environmental Conditions : Black points
How about other sea states along the ECL?
In order to develop a model which could predict any sensitivity coefficient in the
corresponding ECL, it is necessary to use a polynomial regression.
38. 38
RESULTS
In our case, for the polynomial interpolation, we defined two vectors which reflect the
degree of the polynomial model.
X
Y
Z (A, B1, B2, C1, C2)
41. 41
PAPER 2 (P2)
The main purpose of this work is to find a relationship between the
variation of the wind shear exponent and the predicted long term
extreme response in a monopile wind turbine.
Wind Shear Exponent 𝜶
Long-TermExtreme
Response
42. 42
WIND SHEAR: ONSHORE VS OFFSHORE (AND TRANSITION ZONES)
SWL
~5 km
~150 m
Z01
Z02
Land Sea
H (m) H (m)
Marine atmospheric
boundary layer
(MABL)
49. 49
PAPER 3 (P3)
This paper focuses on two aspects:
The first aspect is the study of the minimum simulation length required
to obtain accurate results when performing a statistical extrapolation
procedure.
The second aspect deals with the study of the effect of considering a
flexible soil foundation, rather than the usual rigid connection, on
extreme responses.
59. 59
CONTRIBUTIONS
The contributions of the present research are directly related to
the aspects introduced in the “PROBLEM STATEMENT” section (P0).
The study P0 was applied to an onshore wind turbine and
therefore waves were neglected. This aspect has been one of the first gaps
addressed in the present research.
In the papers, joint probability distributions that consider both wind
(UW) and wave parameters (HS, TP) have been taken into account for all
the papers. In this case, conditionality among parameters means that
only certain combinations of environmental conditions are suitable to
be used in the simulations.
In particular, the results of P1 confirmed the important participation of
waves to the system’s outputs. In the same way, it was observed in P2
that the FASF (FX) is mainly governed by the waves. Also, From the
results of P3, it was seen that the presence of waves particularly affects
long-term responses.
60. 60
A second gap identified at P0 was related to the fact that the
ultimate loads were estimated by averaging the absolute maximum values.
Also, authors only addressed to short term responses.
Attending to this aspect, in papers P2 and P3, the Global Maxima
Method (GMM) was employed. Then, the data were fitted to a Gumbel
distribution to find the most probable value of extreme responses at
the mudline of the monopile. Thus, a more precise estimation of the
response was obtained to perform better comparisons.
In this thesis also long-term loads were studied. relevance of this point
is related to the fact that at a long-term level the turbine control system
has a great influence on the extreme long-term load calculation. This
problem is bypassed in this research by including the Modified
Environmental Contour Method (MECM) .
From the results obtained in P2 and P3, it was found that the critical EC
for FX is near 24 m/s and for MY is around 16mps. It was also found that
the location of the critical EC for FX is particularly affected by wind
shear whereas the location of this condition is unaffected for MY.
CONTRIBUTIONS
61. CONTRIBUTIONS
A third aspect addressed in the present research is referred to
the dynamic responses considered in P0. In that study, only the FABM was
taken into consideration, and not FASF. Since P0 did not consider wave
loading, conditionality on environmental parameters, or methods based on
extreme statistics, it was deemed necessary to examine the sensitivity of
the wind shear in more detail taking into consideration all these aspects.
61
The results from P2 supported that MY was not very sensitive to wind
shear, but it was also found that FX was not sensitive to it. It is
important to mention that in P0 the responses were addressed only in
the short term. However, in this research, the analysis was made to
obtain the estimation of the 50-yr long-term responses.
62. CONTRIBUTIONS
Another important aspect that is often ignored during the
modelling of a bottom-fixed offshore wind turbine is the soil-structure
interaction. This aspect allows guaranteeing a high fidelity of the numerical
model of the offshore wind turbine. Within the literature, it is very
common to find that the foundation is modelled as a completely rigid
connection, as it was in done in P0. In an offshore context, the effects of
foundation flexibility may be important due to the combined loading
62
To evaluate the effects that a flexible soil model can induce on the
extreme responses of an offshore wind turbine, the improved apparent
fixity (IAF) soil model was used in P3. From the results, it was observed
that the inclusion of the soil flexibility induced a particular effect on the
FABM. When a completely rigid foundation was considered, the critical
wind speed was 16.5 m/s. However, when the IAF model was employed
in simulations, this critical speed was shifted to 18 m/s. Also, the value
of the 50-yr long-term extreme response experienced a slight increase
in its value.
63. CONTRIBUTIONS
Another gap not directly related to limitations derived from P0
was also addressed. In P3, there was a literature review, and it was found
that there are on-going discussions about the suitability of adopting a
simulation length of 10-minutes for offshore wind energy applications. For
onshore, 10-min has been the standard for many years. However, since
offshore wind turbines are affected by wave loading, it is not entirely clear
whether 10-min can guarantee the stochastic independence.
63
From the results of P3, the effects of simulation length were assessed.
It was found that a 10-minute simulation length gives acceptable results
for obtaining extrapolated extreme responses for the one hour level.
However, it does not provide adequate results for the extrapolation of
long-term extreme responses. This makes it necessary to use durations
longer than 30 minutes in the simulations.
65. 65
CONCLUSIONS FROM P1
It was found that there is a relationship between the sensitivity of the
outputs that can be well represented as a function of the uncertainties
in wave parameters.
It was observed a linear behaviour when there was only uncertainty in
the wave height (HS). However, when uncertainty was introduced in the
wave period (TP), or both parameters, the effect in the response
exhibited a second-order relationship.
It was found that the coefficients of the regression functions were fitted
with adequate precision using a third-order interpolation polynomial.
66. 66
CONCLUSIONS FROM P2
It was found that 50yr long-term extreme responses are driven by
different environmental factors. In the case of FX, waves are the
environmental factor that governs its behaviour. In the case of MY, it
was observed a peak within the operational range, indicating that this
response is mainly governed by the wind.
It was observed that the WSC influenced the identification of critical
wind speed for FX but not for MY.
It was found that the long-term extreme responses associated with
monopile (FX, MY) have low sensitivity with respect to WSC.
67. 67
CONCLUSIONS FROM P3
It was identified the need to explore the effects of lengths other than
that currently employed. In this regard, it was concluded that a 10-
minute simulation can estimate the distribution of one-hour extreme
responses with adequate accuracy, but it is not sufficient for long-term
responses with a return period of 50 years.
From the results, it was found that the inclusion of soil flexibility on the
simulations does not have much impact on the one-hour extreme
response. However, when a return period of 50 years is considered, the
critical condition found with the MECM for MY is shifted, and the
extreme response increases by 2.96%. In the case of FX, the inclusion of
soil does not produce a significant variation in the long-term extreme
response.
68. 68
FUTURE RESEARCH AGENDA
Inclusion of higher-order wave kinematics e.g. Stokes 5th order waves,
Stream function wave theory, and others. Also, inclusion of higher-order
loading models to capture the effects that nonlinear wave kinematics
can induce on the structure e.g. FNV, Rainey, M&M, and others.
Evaluation of including more complete and advanced soil models e.g.
coupled springs, distributed springs, among others.
Addressing the combined effect of all types of uncertainties will be
important to understand how they are interrelated and what is their
respective influence on the dynamic responses of interest.
Evaluation of the effects that ringing and springing can produce on the
aero-hydro-servo-elastic simulations must be addressed as they can
cause extreme loads to increase considerably.
69. 69
FUTURE RESEARCH AGENDA
The inclusion of more environmental variables in the joint probability
distributions and their influence on the environmental contour method
as well as the dynamic responses should be explored. These include the
turbulence intensity, wind veer, wind shear, coherence spectrum
parameters, and many others.
It is important to study the propagation of uncertainty on the dynamic
responses under different working conditions e.g. parked, idling, in
installation, with faults, and others
Fatigue analysis is also an important aspect in the verification of the
criteria fulfilment that ensures the reliability of the structure. These
types of analysis should be studied in more detail in future research.
70. 70
FUTURE RESEARCH AGENDA
Larger turbines need to be studied. The NREL has recently released the
FAST simulation model for a 15 MW wind turbine, so further research is
expected to be carried out using this model for the near future
71. ACKNOWLEDGEMENTS
Thank you for the attention¡
71
FONDECYT - CONCYTEC
Dr Madjid Karimirad and Dr. Arturo Ortega
Dr Jaime Luyo and Mrs Laura Parillo
Dr Alberto Coronado
my family, my doctoral colleagues, and
everyone who has given me any kind of help during the development of this
thesis