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A robust feature of global warming is that the surface of the land warms more than the   surface of the oceans. We call this the land/ocean temperature contrast.\\   The reason is partly because the oceans are slow to warm up compared to land,   but that's not the whole story.\\   If we were to warm earth's oceans by $1^{\circ}$C and then stop (in our real world "experiment" we haven't stopped   yet), the land would warm by about $1.5^{\circ}$C and then stay warmer than the   oceans, even after the ocean has 'caught up' to the land. The land and ocean surface temperatures have a similar relationship in   the warming and cooling of year-to-year variability. \\  diff --git a/layout.md b/layout.md  index f0a6af8..2db22e1 100644  --- a/layout.md  +++ b/layout.md 
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Intro_GW.html Intro_gw.tex  interannual_variability.tex  Interannual_variability.html  ENSO_experiment.tex  ENSO_experiment.html  Tropics_vs_ExtraTropics.tex  Tropics_vs_extratropics.html  Impacts_on_us.tex  Impacts.html