sandbox/Antoonvh/README.pubs

Pages for peer reviewed publications

This page gives an overview of my pages that were used for published articles, etc.

A fourth-order accurate adaptive solver for incompressible flow problems

By: J. Antoon van Hooft and Stéphane Popinet

Year: 2022

In: Journal of Computational Physics

DOI: https://doi.org/10.1016/j.jcp.2022.111251

• Chapter 2, solver formulation
  The implementation of the 4th-order accurate solver
• Chapter 3, tests, experiments and examples

1. Adaptive Convergence rates
   
2. Two-dimensional vortices of Taylor and Green
3. Three-dimensional vortices of Antuono
4. Viscous boundary layer
5. Shear instability
6. Rising buoyant plume
7. Dipole-wall collision
8. Head-on collision of two vortex rings

• Appendix
  Non-smooth advection

Detecting nighttime inversions in the interior of a Douglas fir canopy

By: B. Schilperoort; M. Coenders-Gerrits; C. Jiménez Rodríguez; J.A. van Hooft; B.J.H. van de Wiel; H. Savenije

Year: 2022

in: Agricultural and Forest Meteorology

DOI: https://doi.org/10.1016/j.agrformet.2022.108960

• A model for Layer formation in a forest canopy

Modeling the Atmospheric Diurnal Cycle

PhD thesis by Antoon van Hooft

Year: 2020

At: TU Delft repository

DOI: https://doi.org/10.4233/uuid:e45cea45-8915-4a11-b8fd-389cb3e19d22

In order of appearance:

• Front cover
  
• Ouverture: Root finding
• Entr’acte 1: The Mandelbrot set
  
• Chapter 2 is based on an article
  
• Entr’acte 2: A dipole collision with a wall
  
• Chapter 3 is based on an article
  
• Entr’acte 3: The collision of two vortex rings
  
• Chapter 4 is based on an article
  
• Entr’acte 4: Error estimation for a Poisson solver
• Encore: This section is based on the experience writing these pages

A Note on the Scalar-Gradient Sharpening in the Stable Atmospheric Boundary Layer

By: J. Antoon van Hooft

Year: 2020

In: Boundary-Layer Meteorology

DOI: https://doi.org/10.1007/s10546-020-00516-x

Scalar-gradient sharpening by the self advection of a dipolar vortex.

An Idealized Description for the Diurnal Cycle of the Dry Atmospheric Boundary Layer

By J. Antoon van Hooft, Peter Baas, Maurice van Tiggelen, Cedrick Ansorge and Bas J.H. van de Wiel.

Year: 2019

In: Journal of the Atmospheric Sciences

DOI: https://doi.org/10.1175/JAS-D-19-0023.1

In order of appearance,

• The effects of the pressure-gradient force, using a Single-Column Model (SCM).
• The effect of including a layered soil-heat storage model in the SCM.
• Large-eddy simulation of the diurnal cycle with a weak wind forcing.

Adaptive Cartesian Meshes for Atmospheric Single-Column Models

By J. Antoon van Hooft, Stéphane Popinet and Bas J.H. van de Wiel

Year: 2018

In: Geoscientific Model Development

DOI: https://doi.org/10.5194/gmd-11-4727-2018

In order of appearance,

• Results Sect 3.1, The Laminar Ekman-spiral test case;
  1. using a fixed and equidistant grid
     
  2. using an adaptive grid
• Results Sect. 3.2, The GABLS1 case;
  1. using an adaptive grid
  2. using a fixed and equidistant grid
     
• Results Sect 3.3, The GABLS2 case;
  1. using an adaptive grid
  2. using a fixed and equidistant grid

Towards Adaptive Grids for Atmospheric Boundary-Layer Simulations

By: J. Antoon van Hooft, Stéphane Popinet, Chiel C van Heerwaarden, Steven J.A. van der Linden, Stephan R de Roode and Bas J.H. van de wiel.

Year: 2018

In: Boundary-layer meteorology.

DOI: https://doi.org/10.1007/s10546-018-0335-9

In order of appearance,

• Section 2.1: Generate an example tree grid and output the relevant cells
• Section 2.2: Analysis of a data slice from a 3D turbulence simulation
  
• Chapter 3: DNS of the growth and decay of a convective atmospheric Boundary layer using an Adaptive grid
  
• Chapter 3: DNS of the growth and decay of a convective atmospheric Boundary layer in fixed-and-regular-grid mode
  
• Chapter 4: LES of an atmospheric boundary layer filled with a radiant smoke cloud
  
• Appendix 1: DNS of a lid driven cavity in two dimensions using an adaptive grid
  
• Appendix 1: DNS of a lid-driven cavity in two dimensions with a fixed-and-regular grid