From 0b674b9f17d42ec0de532ff9e38e203d50436cfa Mon Sep 17 00:00:00 2001
From: Max-Coppin <147694216+Max-Coppin@users.noreply.github.com>
Date: Wed, 6 Mar 2024 11:51:22 +0100
Subject: [PATCH] home

---
 _config.yml        |  3 ++-
 _layouts/home.html | 14 ++++++++++++++
 _layouts/home.md   | 29 -----------------------------
 3 files changed, 16 insertions(+), 30 deletions(-)
 delete mode 100644 _layouts/home.md

diff --git a/_config.yml b/_config.yml
index bcf2be2..0baaab5 100644
--- a/_config.yml
+++ b/_config.yml
@@ -312,7 +312,8 @@ title: "Homepage"
 author_profile: true
 author: Max Coppin
 
-      
+
+
       
 defaults:
   # _docs
diff --git a/_layouts/home.html b/_layouts/home.html
index 1a2a5a8..189c124 100644
--- a/_layouts/home.html
+++ b/_layouts/home.html
@@ -21,6 +21,20 @@ <h3 class="archive__subtitle">{{ site.data.ui-text[site.locale].recent_posts | d
 
 {% include paginator.html %}
 
+<h1>Presentation</h1>
+<p>I’m a PhD student at LEGI and IGE (Grenoble, France) under Joel Sommeria and Bruno Derumble supervision. My field of study is geophysical fluid dynamics, and my thesis focuses on the modeling of ocean convection on the Coriolis platform.</p>
+
+<h2>Current project</h2>
+<p>We explore the different regimes of convection as a function of the two major variables in geophysical fluids, namely rotation (through the Coriolis effect) and stratification. We also explore the influence of wind-induced stress.</p>
+
+<p>My study is based on a number of themes:</p>
+<ul>
+  <li><strong>Turbulence in convection:</strong> How does turbulent kinetic energy evolve in a convective plume and in the mixing layer? Refinement of turbulence parameterization and turbulent closure models.</li>
+  <li><strong>The organization of convection:</strong> In this part, I am interested in the coherent structures that can be observed in convection (plumes, cones, cells, convective vortices) and how these structures are affected by the different convection regimes.</li>
+  <li><strong>Experimental observation methods:</strong> We are exploring new methods in order to perform temperature field measurements with the T-LIF.</li>
+</ul>
+
+
 
 
 
diff --git a/_layouts/home.md b/_layouts/home.md
deleted file mode 100644
index 33a2ae3..0000000
--- a/_layouts/home.md
+++ /dev/null
@@ -1,29 +0,0 @@
----
-
-permalink: / 
-layout: single 
-author_profile: true
-author: Max Coppin
-title: "Homepage"
-toc: false
-header:
-  overlay_color: "#000"
-
----
-# Presentation
-I’m a PhD student at LEGI and IGE (Grenoble, France) under Joel Sommeria and Bruno Derumble supervisation. My field of study is geophysical fluid dynamics, and my thesis focuses on the modelisation of ocean convection on the Coriolis platform.
-
-## Current project
-We explore the different regimes of convection as a function of the two major variables in geophysical fluids, namely rotation (through the Coriolis effect) and stratification. We also explore the influence of wind-induced stress.
-
-My study is based on a number of themes :
-
-- Turbulence in convection :
-How does turbulent kinetic energy evolve in a convective plume and in the mixing layer ?
-Refinement of turbulence parameterisation and turbulent closure models
-
-- The organisation of convection :
-In this part I am interested in the coherent structures that can be observed in convection (plumes, cones, cells, convective vortices) and how these structures are affected by the different convection regimes.
-
-- Experimental observation methods :
-We are exploring new methods in order to perform temperature field measurements with the T- LIF.