This file was generated with pandoc article.tex -o article.html --standalone --mathjax and placed in static/articles/. To replace this with your own article, see the instructions in the Writing section of this site.
The uniform debris cover hypothesis predicts that a sufficiently thick and laterally continuous debris mantle will drive the glacier surface toward thermal equilibrium with its surroundings. For a debris layer of thickness $h$ and thermal conductivity $k$, the melt rate $\dot{m}$ scales approximately as: $$\dot{m} \approx \frac{k \, \Delta T}{h \, L_f \, \rho_i}$$ where $\Delta T$ is the temperature difference across the layer, $L_f$ is the latent heat of fusion, and $\rho_i$ is the density of ice.
Replace this section with your actual discussion. Articles can include figures, footnotes, references, and any LaTeX content that Pandoc can convert to HTML with MathJax rendering.