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[[Image:WILSIM_grandCanyon.png|200px|left|link=Science_spotlights#WILSIM_Grand_Canyon]]
[[Image:Auto Marsh.png |200px|left|link=Science_spotlights#Salt_Marshes_with_Jagged_Edges.3F]]
Looking for a new lesson for your undergraduate class in the 2015 Fall semester? Prof. Wei Luo of Northern Illinois University with a team of colleagues offers a physically-based landscape evolution model. It is called WILSIM-GC, a simulation model that allows learners to explore the development of the Grand Canyon over 10 million years. The java code is an easy download and features a GUI that offers key knobs to investigate erosional processes and river incision. [[Science_spotlights#WILSIM_Grand_Canyon|More...]]<br><br>[mailto:csdmsweb@colorado.edu Nominate a science spotlight]
Remember last time you stood at the muddy edge of a salt marsh? Was the edge straight, or jagged with small coves? A new cellular automata model shows that salt marsh edges evolve to be straight under high wave power regimes and to be jagged under low wave power regimes. Specifically under low wave power conditions local resistance of each cell dominates erosion rate, and this variability creates the typical small inset coves along marsh edges. Nicoletta Leonardi, contributed her marsh evolution code to further explore. [[Science_spotlights#Salt_Marshes_with_Jagged_Edges.3F|More...]]<br><br>[mailto:csdmsweb@colorado.edu Nominate a science spotlight]

Revision as of 12:04, 5 October 2015

Auto Marsh.png

Remember last time you stood at the muddy edge of a salt marsh? Was the edge straight, or jagged with small coves? A new cellular automata model shows that salt marsh edges evolve to be straight under high wave power regimes and to be jagged under low wave power regimes. Specifically under low wave power conditions local resistance of each cell dominates erosion rate, and this variability creates the typical small inset coves along marsh edges. Nicoletta Leonardi, contributed her marsh evolution code to further explore. More...

Nominate a science spotlight