deploy: c244521

Author: oscarbranson

04_atmosphere/l22.html

@@ -425,7 +425,7 @@ <h2> Contents </h2>
 <p>Both processes, light absorption/scattering and could formation, are not very well understood on a global level and are one on the main uncertainties associated with studies predicting the future climate indeed these processes are our largest uncertainty on historic climate change, too.
 The uncertainty is mainly due to the large variability in the physical and chemical properties of aerosol particles, as well as their temporal and spatial distributions. Unlike gases like carbon dioxide or methane, we don’t know what the levels of aerosols were like in the past.</p>
 <figure class="margin-caption align-default" id="radiative-forcing">
-<a class="reference internal image-reference" href="04_atmosphere/figures/figure22.0.png"><img alt="04_atmosphere/figures/figure22.0.png" src="04_atmosphere/figures/figure22.0.png" style="width: 80%;" />
+<a class="reference internal image-reference" href="../_images/figure22.0.png"><img alt="../_images/figure22.0.png" src="../_images/figure22.0.png" style="width: 80%;" />
 </a>
 <figcaption>
 <p><span class="caption-text">The left hand side shows the impacts on Earth’s energy budget cased by changes in gases and aerosols and highlights that the role of aerosols is highly uncertain. The right hand side shows the impact of the changes in energy balance on surface temperature.</span><a class="headerlink" href="#radiative-forcing" title="Link to this image">#</a></p>