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https://www.youtube.com/watch?v=5dWcDlsC4cA
8/26/2021
Sea level rise over the next century will inundate portions of coastal states, requiring some kind of adaptation from local populations. In this talk, John Callahan of the Delaware Geological Survey shares the sea level rise projections he has developed for the state, and Phil Barnes, of the Institute for Public Administration in the Biden School of Public Policy, addresses options communities have to deal with rising waters.
Dr. Callahan's Areas of Expertise
Expertise in climatology, meteorology and storms, sea-level rise and climate change, tides and coastal flooding, remote sensing, GIS, geospatial and time series statistics.
Research projects include storm surge from tropical and extra-tropical cyclones in the Delaware and Chesapeake Bays; dendrochronology of Atlantic White Cedar trees; habitat identification of Delmarva Fox Squirrel; atmospheric water vapor over the Amazon Rainforest from satellites; and development of coastal flood early warning system.
Serves on the Delaware River Basin Commission Advisory Committee on Climate Change.
Lead author of Recommendations of Sea-Level Rise Planning Scenarios for Delaware: Technical Report.
What is causing the seas to rise?
The projection of sea-level rise in the future
The impact in Delaware
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Biden School of Public Policy & Administration
Institute for Public Administration
Assistant Professor
Faculty Director, Stavros Niarchos Foundation Ithaca Initiative
Policy Scientist, IPA
pbarnes@udel.edu
298P Graham Hall
302-831-7010
Philip’s research focuses on local climate change adaptation planning and implementation, with an emphasis on flooding and sea level rise mitigation. He also conducts research on non-traditional transportation policy such as bikeshare networks, electric vehicles, and autonomous vehicles. Philip works closely with state agencies on applied research to enhance local community resiliency.
RASCAL Coffee Presentation on 7/14/2021 by Elizabeth Sawin
It started in Colombia - turning off vehicles one day
Lack of physical activities - Health Benefits of walking, less traffic congestion, savings of transportation
After the energy crisis post-Fukushima event
Case Study - planting around churches and schools as well as orchards
Maggie Pletta - Wetland Outreach
"Delaware is the lowest in the nation"
Allison Rogerson - Environmental Scientist
DNREC began investigating Salt marsh restoration in 2012
Andy Howard - Environmental Scientist
Dagsboro - applying dredged material 3-9" on the surface
Matt Jennetta - Environmental Scientist
Living Shoreline
Aug. 6, 2020 - Christian Hauser
(Dr. Siders https://www.drc.udel.edu/Documents%20Bios%20CVs/SIDERS%2001.2020%20CV.pdf)
In case of problems watching the above video, the URL is at https://www.youtube.com/watch?v=tZ4axqOrkDY
$500M homes built on vulnerable land in Sussex County since 2010.
Homes built in DE are 2.6 times faster in flood zones than non-flood zones.
DE SLR Advisory Committee Vulnerability Assessment
Western Carolina University Beach Nourishment Viewer (http://beachnourishment.wcu.edu/oneState?state=DE)
Joey Flechas jflechas@miamiherald.com - November 16, 2016
https://www.miamiherald.com/news/local/community/miami-dade/miami-beach/article115264938.html
Does the beach replenishment artificially change the shoreline in the long run and also delay the effects of the sea level rise? Why should the taxpayers keep funding the lifestyle of people who choose to live in the flood-prone areas?
If FEMA is providing all fund to buy out homes, what incentives are there for local governments to not encourage expensive homes in the water-front areas to increase their tax base?
Isn't it predictable that the local governments would offer only the less expensive towns for buyouts so that they still collect higher property taxes from expensive areas while they survive?
Lecture by Dr. Andreas Muenchow - 8/20/2020
Andreas Muenchow describes his experience sailing the coastal waters of northern Greenland for over 20 years. In Muenchow's words, "While oceans, sea ice, and glaciers have much changed over time as have sensing technologies and global climate modeling, ships and sailors still extract truths not accessible by satellites and computer codes. Field work in a cold and hostile place of stunning beauty humbles the observer when nature’s plan differs from that of the sailor as it often does.
High salinity brings the freezing point down to 29 degrees F from 32 of fresh water. As going down the ocean depth, salinity gets higher and the temperature stays stable, often warmer than the surface where the ice melts.
About an hour into the lecture, Dr. Muenchow explains the speed of glacier melting and the sea level rise. When the ice melts, it immediately forms a shielding blanket around the bottom of the iceberg preventing it from melting further. However, the ocean currents and forces stir up the blanket and remove it, then the ice melts again.
Sean T. O'Neill, AICP
Policy Scientist
Institute for Public Administration
Biden School of Public Policy & Administration
University of Delaware
180 Graham Hall, Newark, DE 19716-7201
c: 301-785-2849 | oneill@udel.edu
www.ipa.udel.edu | www.bidenschool.udel.edu
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