This week, we looked at elevation data for the New Jersey shoreline from pre and post Sandy datasets, and compared two DEMs in Florida to determine the impacts of a 1M storm surge and comparing how the elevation data effects the results.
Below, you will see the final difference in elevation on a stretch of the Jersey shore from before and after Sandy. The pre-Sandy file has a more consistent coastline in terms
of obvious areas of development. There
are many areas that now look almost like little inlets where housing has
clearly been destroyed and beaches eroded.
There are clearly some areas that were hit much harder than others and
destruction is not consistent or even. The areas of greatest erosion appear to be along the center
left of the image. This matches up with
my observations of the differences between the two las images and confirms the
areas of greatest destruction. There
appear to be some data anomalies as you move farther inland in that the
difference between the two layers is as if the post layer was subtracting a
value of zero. This is also right next
to areas that were apparently built up during the storm. The take home message is that
destruction was not equal and that more analysis should be done to gain a
greater understanding of the situation.
This exercise was very good because it helped me to think about the many variables to consider when assessing pre and post storm damage. It also helped me to see the impact of data that does not perfectly align and the general limitations in analysis such as this.
The map below is a comparison of a USGS DEM and a LiDar DEM to assess the coastal affects of a 1M storm surge. There are a number of potential issues related to how we
assumed the lack of connectedness and uniform surge could influence the areas
being impacted. In reality, it is quite
likely that areas not showing a complete connection or that are in a low lying
area, but surrounded by higher ground, are actually connected and vulnerable
enough to be impacted by the combination of high winds, rainfall, and
variability in storm surge that is not encapsulated in a study that assumes
this level of uniformity. Just because
storm surge might max out at a given height on average, it does not mean this
impact is felt equally across all regions and even limited connectivity and
semi-protected areas should be considered as points of vulnerability. We could adjust our analysis by applying a storm
surge range that gives us a level of uncertainty with which to work. We could also review the areas that show
limited connectivity and determine what might be causing that limitation. All limits to connectivity of elevation are
not created equally and having a deeper understanding of those areas would be
very beneficial in designing a study to better model real world
possibilities. Rainfall and inland
flooding should also be incorporated as variables in a realistic study.
This exercise was very beneficial for understanding the impact of DEM accuracy on flood analysis. It also helped me to understand the many assumptions we make when relying on elevation data and constant variables in complex analysis.