Using sUAS-Acquired Imagery to Map Landslide Susceptibility along the Lake Michigan Shoreline of Wisconsin
DOI :
https://doi.org/10.17307/wsc.v1i1.340Mots-clés :
Erosion, Lake Michigan, UAV, DronesRésumé
Bluffs along the Wisconsin shoreline of Lake Michigan frequently collapse, and this collapse often occurs due to saturation and weakness in a sand layer present in the bluffs. We used an sUAS to collect visible and thermal imagery of bluffs along Lake Michigan in Kewaunee County, WI. We then proceeded to classify this imagery in ArcGIS Pro to determine whether the program’s classification tools could locate the sand layer. Furthermore, we examined imagery before and after a major storm to determine the storm’s effect on water content in the sand layer. Our results indicate that we can use automated computer programs to classify the sand layer based on a combination of visible and thermal imagery. Additionally, we found that large summer storms do not significantly alter the saturation of the sand layer and infer that their effect on bluff collapse is minimal.Références
Bay-Lake Regional Planning Commission. (1996). Lak Michigan Shoreline Recession and Bluff
Stability in Northeastern Wisconsin: 1996.
Brown, E. A., Wu, C. H., Mickelson, D. M., & Edil, T. B. (2005). Factors Controlling Rates of
Bluff Recession at Two Sites on Lake Michigan. Journal of Great Lakes Research, 31(3), 306-
doi: 10.1016/S0380-1330(05)70262-8
Hart, D. J., Swanson, K., & Rawling III, J. E. (2020). Final Report: Aerial thermal imaging applied
to Wisconsin’s groundwater, springs, thin soils, and slopes. Retrieved from the University of
Wisconsin Water Resources Institute website: https://www.wri.wisc.edu/wpcontent/uploads/DATCP2020-3.pdf
Lee, G. B., & Horn, M. E. (1972). Pedology of the Two Creeks Section, Manitowoc County,
Wisconsin. Wisconsin Academy of Sciences, Arts, and Letters. 60, 183-199.
National Cooperative Soil Survey. (2011, January). Kewaunee Series. Retrieved from
https://soilseries.sc.egov.usda.gov/OSD_Docs/K/KEWAUNEE.html
National Park Service. (2005). Fig. 7: Idealized Two Creeks Section. After Prouty (1960, Fig. 12).
Geology of Ice Age National Scenic Reserve of Wisconsin. Retrieved from
https://www.nps.gov/parkhistory/online_books/science/2/chap2.htm
USDA Natural Resources Conservation Science. (2007, May). Chapter 7: Hydrologic Soil Groups.
In Part 630 Hydrology National Engineering Handbook. Retrieved from
https://directives.sc.egov.usda.gov/OpenNonWebContent.aspx?content=17757.wba
Volpano, C. A., Zoet, L. H., Rawling III, J. E., Theuerkauf, E. J., & Krueger, R. (2020). Threedimensional bluff evolution in response to seasonal fluctuations in Great Lakes water
levels. Journal of Great Lakes Research, 46(6), 1533-1543. Doi: 10.1016/j.jglr.2020.08.017
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