report.md 2.1 KB
title: My Great Report subtitle: First finding of something extraordinary author: Pierre-Yves Barriat #date: "15 avril 2022" lang: "en" fontsize: 11pt
bibliography: "assets/MyLib.bib"
Abstract
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1. Introduction
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2. Tables
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: Table 1.1: Demonstration of simple table syntax.
| Default | Center | Right |
|---|---|---|
| Tires | Pc | 12.50 |
| Petrol | Br | 456.10 |
3. Figures
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4. Equations
The 0-dimension Energy Balance Model (EBM) or global EBM:
$$(1 - \alpha)\frac{S_0}{4} = \sigma T^4 \qquad (1)$$
The one-dimension EBM or zonal EBM:
$$T{i} = \frac{{\ S}{i}\left( 1 - \alpha(T_{i}) \right) + K\overline{T} - A}{B + K} \qquad (2)$$
- $T_i =$ the surface temperature at latitude band $i$
- $S_i =$ the mean annual solar radiation at latitude $i$
- $K =$ the transport coefficient (here set to 3.81 $Wm^{-2 \ \circ}C^{-1}$)
- $A$ and $B$ are constants governing the longwave radiation loss (here taking values $A = 204.0 \ Wm^{-2}$ and $B = 2.17 Wm^{-2 \ \circ} C^{-1}$)
- $\overline{T} =$ the global mean surface temperature
- $\alpha(T_{i}) =$ the albedo at latitude i, and it can be formulated by:
$$ \alpha (T_i)= \begin{cases} 0.5 & \quad \text{if \ $T{i} \leq 270K$}\ 0.5 - 0.25 * \frac{T-270}{20} & \quad \text{if \ $270K \leq T{i} \leq 290K$}\ 0.25 & \quad \text{if \ $T{i} \geq 290K$}\ \end{cases} $$