Emmanuel Olutayo Akinlabi
Rahway, New Jersey, United States
699 followers
500+ connections
About
As a Senior Data Scientist at Merck & Co., I specialize in harnessing advanced data…
Articles by Emmanuel Olutayo
Activity
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PASSION I recently was asking a friend who happen to be a member of my Church why she didn’t attend my research talk. She quipped “I didn’t bother…
PASSION I recently was asking a friend who happen to be a member of my Church why she didn’t attend my research talk. She quipped “I didn’t bother…
Liked by Emmanuel Olutayo Akinlabi
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I’m happy to share that I’ve started my Master's degree at University of the West of England!
I’m happy to share that I’ve started my Master's degree at University of the West of England!
Liked by Emmanuel Olutayo Akinlabi
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They say the hardest part of leaving a job is saying goodbyes to friends and colleagues and I totally agree with that statement. My last day with…
They say the hardest part of leaving a job is saying goodbyes to friends and colleagues and I totally agree with that statement. My last day with…
Liked by Emmanuel Olutayo Akinlabi
Experience
Education
Licenses & Certifications
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Data Analysis with Python
Coursera
IssuedCredential ID https://coursera.org/share/50bb3a691c81c37a3a899939fb3cc155
Volunteer Experience
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Member
City Mission Kaiserlautern Germany
Distribution of food and rendering help to the refugees and impoverished in Kaiserlautern, Germany
Publications
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Budgets of Second-Order Turbulence Moments over a Real Urban Canopy
Boundary Layer Meteorology
This study analyses budgets of second-order turbulence moments over a real urban canopy using large-eddy simulation. The urban canopy is representative of the City of Boston, MA, United States and is characterized by a significant height variability relative to the mean build- ing height.
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Dispersive Fluxes Within and Over a Real Urban Canopy: A Large-Eddy Simulation Study
Boundary Layer Meteorology
Large-eddy simulations (LES) are conducted to study the transport of momentum and passive scalar within and over a real urban canopy in the City of Boston, USA. This urban canopy is characterized by complex building layouts, densities and orientations with high-rise buildings. Special attention is given to the magnitude, variability and structure of dispersive momentum and scalar fluxes and their relative importance to turbulent momentum and scalar fluxes. We first evaluate the LES model by…
Large-eddy simulations (LES) are conducted to study the transport of momentum and passive scalar within and over a real urban canopy in the City of Boston, USA. This urban canopy is characterized by complex building layouts, densities and orientations with high-rise buildings. Special attention is given to the magnitude, variability and structure of dispersive momentum and scalar fluxes and their relative importance to turbulent momentum and scalar fluxes. We first evaluate the LES model by comparing the simulated flow statistics over an urban-like canopy to data reported in previous studies. In simulations over the considered real urban canopy, we observe that the dispersive momentum and scalar fluxes can be important beyond 2–5 times the mean building height, which is a commonly used definition for the urban roughness sublayer height. Above the mean building height where the dispersive fluxes become weakly dependent on the grid spacing, the dispersive momentum flux contributes about 10–15% to the sum of turbulent and dispersive momentum fluxes and does not decrease monotonically with increasing height. The dispersive momentum and scalar fluxes are sensitive to the time and spatial averaging. We further find that the constituents of dispersive fluxes are spatially heterogeneous and enhanced by the presence of high-rise buildings. This work suggests the need to parameterize both turbulent and dispersive fluxes over real urban canopies in mesoscale and large-scale models.
Other authors -
Fractal Reconstruction of Sub-Grid Scales for Large Eddy Simulation
Flow, Turbulence and Combustion
In this work, the reconstruction of sub-grid scales in large eddy simulation (LES) of turbulent flows in stratocumulus clouds is addressed. The approach is based on the fractality assumption of turbulent velocity field. The fractal model reconstructs sub-grid velocity field from known filtered values on LES grid, by means of fractal interpolation, proposed by Scotti and Meneveau (Physica D 127, 198–232 1999). The characteristics of the reconstructed signal depend on the stretching parameter d…
In this work, the reconstruction of sub-grid scales in large eddy simulation (LES) of turbulent flows in stratocumulus clouds is addressed. The approach is based on the fractality assumption of turbulent velocity field. The fractal model reconstructs sub-grid velocity field from known filtered values on LES grid, by means of fractal interpolation, proposed by Scotti and Meneveau (Physica D 127, 198–232 1999). The characteristics of the reconstructed signal depend on the stretching parameter d, which is related to the fractal dimension of the signal. In many previous studies, the stretching parameter values were assumed to be constant in space and time. To improve the fractal interpolation approach, we account for the stretching parameter variability. The local stretching parameter is calculated from direct numerical simulation (DNS) data with an algorithm proposed by Mazel and Hayes (IEEE Trans. Signal Process 40(7), 1724–1734, 1992), and its probability density function (PDF) is determined. It is found that the PDFs of d have a universal form when the velocity field is filtered to wave-numbers within the inertial range. In order to investigate Reynolds number (Re) dependence, we compare the inertial-range PDFs of d in DNS and large eddy simulation (LES) of stratocumulus cloud-top and experimental airborne data from Physics of Stratocumulus Top (POST) research campaign. Next, fractal reconstruction of the subgrid velocity is performed and energy spectra and statistics of velocity increments are compared with DNS data. It is assumed that the stretching parameter d is a random variable with the prescribed PDF. We show that the agreement with the DNS is in such case better and the error in mass conservation is smaller compared to the use of constant values of d. The motivation of this study is to reproduce effect of sub-grid scales on a motion of Lagrangian particles (e.g. droplets) in clouds.
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Estimating Turbulence Kinetic Energy Dissipation Rates in the Numerically Simulated Stratocumulus Cloud-Top Mixing Layer: Evaluation of Different Methods
Journal of the Atmospheric Sciences
In this work, direct numerical simulation (DNS) of the stratocumulus cloud-top mixing layer is used to test various approaches to estimate the turbulence kinetic energy (TKE) dissipation rate ε from one-dimensional (1D) intersections that resemble experimental series. Results of these estimates are compared with “true” (DNS) values of ε in buoyant and inhomogeneous atmospheric flows. We focus on recently proposed methods of the TKE dissipation-rate retrievals based on zero crossings and…
In this work, direct numerical simulation (DNS) of the stratocumulus cloud-top mixing layer is used to test various approaches to estimate the turbulence kinetic energy (TKE) dissipation rate ε from one-dimensional (1D) intersections that resemble experimental series. Results of these estimates are compared with “true” (DNS) values of ε in buoyant and inhomogeneous atmospheric flows. We focus on recently proposed methods of the TKE dissipation-rate retrievals based on zero crossings and recovering the missing part of the spectrum. These methods are tested on fully resolved turbulence fields and compared to standard retrievals from power spectra and structure functions. Anisotropy of turbulence due to buoyancy is shown to influence retrievals based on the vertical velocity component. TKE dissipation-rate estimates from the number of crossings correspond well to spectral estimates. The method based on the recovery of the missing part of the spectrum works best for Pope’s model of the dissipation spectrum and is sensitive to external intermittency. This allows for the characterization of external intermittency by the Taylor-to-Liepmann scale ratio. Further improvements of this method are possible when the variance of the velocity derivative is used instead of the number of zero crossings per unit length. In conclusion, the new methods of TKE dissipation-rate retrieval from 1D series provide a valuable complement to standard approaches.
Other authors -
Fractal reconstruction of sub-grid scales for large eddy simulation of atmospheric turbulence
Journal of Physics: Conference Series
We present a fractal sub-grid scale model for large eddy simulation (LES) of atmospheric flows. The fractal model is based on the fractality assumption of turbulent velocity field with a dynamical hypothesis based on energy dissipation. The fractal model reconstruct sub-grid velocity field from the knowledge of its filtered values on LES grid, by means of fractal interpolation, proposed by Scotti and Meneveau (1999). The characteristics of the reconstructed signal depends on the (free)…
We present a fractal sub-grid scale model for large eddy simulation (LES) of atmospheric flows. The fractal model is based on the fractality assumption of turbulent velocity field with a dynamical hypothesis based on energy dissipation. The fractal model reconstruct sub-grid velocity field from the knowledge of its filtered values on LES grid, by means of fractal interpolation, proposed by Scotti and Meneveau (1999). The characteristics of the reconstructed signal depends on the (free) stretching parameters, which is related to the fractal dimension of the signal. In previous studies, the stretching parameters was assumed to be constant in space and time and are obtained from experimental velocity signals of homogeneous and isotropic turbulence. To improve this method and account for the stretching parameter variability, we calculate the probability distribution function of the stretching parameter from direct numerical simulation (DNS) data of stratocumulus-top boundary layer (STBL) (courtesy of Prof. J.-P. Mellado from the Max Planck Institute of Meteorology) using the geometric method proposed by Mazel and Hayes. We perform 1D a priori test and compare statistics of the constructed velocity increment with DNS velocity increments.
Other authors
Honors & Awards
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Early Stage Researcher - Marie-Skłodowska-Curie Grant
European Union
Clouds are the largest source of uncertainty in weather prediction, climate science, and remain a weak link in modeling atmospheric circulation. This is rooted in the fact that clouds depend on the physical and chemical processes over a huge range of scales, from the collisions of micron-sized droplets and particles to the airflow dynamics on the scales of thousands of meters. Since ambiguities related to representation of clouds in climate models prevail, explorative observations are still…
Clouds are the largest source of uncertainty in weather prediction, climate science, and remain a weak link in modeling atmospheric circulation. This is rooted in the fact that clouds depend on the physical and chemical processes over a huge range of scales, from the collisions of micron-sized droplets and particles to the airflow dynamics on the scales of thousands of meters. Since ambiguities related to representation of clouds in climate models prevail, explorative observations are still needed. The challenge is on the one hand to establish connections across this range of scales, from aerosol and particle microphysics to macro-scale turbulent dynamics in clouds, and on the other to combine knowledge and training across vastly different scientific and engineering disciplines. The aim of COMPLETE is to develop an inter/multidisciplinary training network that will prepare high-potential early stage researchers (ESRs) with both scientific and industrially-oriented skills that will advance our understanding in these multi-scale complex natural phenomena. COMPLETE will vastly improve Europe’s position as a global leader in technology, science and innovation to address climate change challenges. The training programme will combine the scientific investigation of specific aspects of cloud physics and related turbulent dynamics with training in key professional skills. This comprises an exceptional experimental programme that includes field experiments, laboratory and numerical simulations, the design and development of advanced fast temperature probes, velocity MEMS and innovative atmospheric mini radio-sondes; all aimed at the production of new, Lagrangian based, cloud fluctuation datasets, required to reduce the fragmentation of results and knowledge in this field.
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Next Einstein Initiative Scholarship
Next Einstein Initiative
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Gold Medalist - National Mathematics Competition for University Students (NAMCUS 2014)
National Mathematical Center, Abuja, Nigeria
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Faculty Prize for the Best Graduating Student in the Department of Pure and Applied Mathematics
Governing Council
Languages
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Yoruba
Native or bilingual proficiency
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English
Full professional proficiency
Organizations
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American Geoscience Union (AGU)
Member
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EuroScience
Associate member
- PresentEuroScience is the non-profit grassroots association of researchers in Europe. Open to European researchers across disciplines and countries, EuroScience undertakes to advance science and innovation in Europe, thereby promoting the interests of its thousands of members.
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Marie Curie Alumi Association
Member
- PresentThe Marie Curie Alumni Association (MCAA) is promoting an active community of researchers brought together by past or present mobility experience under the European Commission's Marie Curie programme. An Association providing high-quality services to enhance research and professional collaboration.
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Nigerian Institute of Managemant (Chartered)
Graduate Member
- Present
More activity by Emmanuel Olutayo
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🎓 PhD officially earned! 🎓 I am excited and honored to share that I have successfully completed my PhD in applied mathematics at the University of…
🎓 PhD officially earned! 🎓 I am excited and honored to share that I have successfully completed my PhD in applied mathematics at the University of…
Liked by Emmanuel Olutayo Akinlabi
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I am excited to share that I have completed a rewarding summer internship at Merck , where I had the incredible opportunity to learn from some of the…
I am excited to share that I have completed a rewarding summer internship at Merck , where I had the incredible opportunity to learn from some of the…
Liked by Emmanuel Olutayo Akinlabi
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Reflecting on 10 Incredible Years in the Tech Industry! Happy New Month It feels like just yesterday I was stepping into the tech world, filled…
Reflecting on 10 Incredible Years in the Tech Industry! Happy New Month It feels like just yesterday I was stepping into the tech world, filled…
Liked by Emmanuel Olutayo Akinlabi
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I moved on to the next phase of my PhD program after passing my candidacy exam.
I moved on to the next phase of my PhD program after passing my candidacy exam.
Liked by Emmanuel Olutayo Akinlabi
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If you need help with improving your academic writing, this seminar is for you!
If you need help with improving your academic writing, this seminar is for you!
Shared by Emmanuel Olutayo Akinlabi
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Join the Knowledge and Skills Forum on June 1, 2024 at 18:00 (WAT) for a live seminar on Writing Academic Report. Our hosts are Dr. Oderinu Razaq…
Join the Knowledge and Skills Forum on June 1, 2024 at 18:00 (WAT) for a live seminar on Writing Academic Report. Our hosts are Dr. Oderinu Razaq…
Liked by Emmanuel Olutayo Akinlabi
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Lately, things have been a bit slow on my Ph.D. research, but this news just ignited my spark again, and I wanted to share it here and save it as a…
Lately, things have been a bit slow on my Ph.D. research, but this news just ignited my spark again, and I wanted to share it here and save it as a…
Liked by Emmanuel Olutayo Akinlabi
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Hello LinkedIn, As our monthly meetup steadily approaches, we want to send out a reminder. Today, we're thrilled to offer more details about our…
Hello LinkedIn, As our monthly meetup steadily approaches, we want to send out a reminder. Today, we're thrilled to offer more details about our…
Liked by Emmanuel Olutayo Akinlabi
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