In the first photo, easy to understand why RI's barrier beaches are destined to be reclaimed by a rising Atlantic Ocean. You can see, in the aerial photo on the display board, how narrow that barrier beach is. In second photo, left to right are Atlantic, barrier beach, Trustom Pond. Fortunately, I'm too old to live to see these portions of our Atlantic coast reclaimed by the sea. But happen it will, and I believe as a result of climate change. Not the most devastating result of climate change, to be sure, but it will certainly affect our summer tourist industry in due course. I have read, and am not sure if true, that the disappearance of RI's barrier beaches will be among the earliest major physiographic changes to occur on the east coast of the US as a result of rising sea levels....
(Wish I knew how to make photos full size, instead of click on thumbnails?)
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You can likely also see why there are probably worse places to spend a Summer day. I took these photos during the annual Sept. Monarch butterfly migration. We used to see thousands. Now, very, very few....
So I took a quick google tour to see what data is there to quibble about. Here's a site that has a pro+ bias that does some of the reasons people quibble with their view, and systematically demolishes them, in their opinion. LOL. https://www.skepticalscience.com/sea-level-rise.htm
In geologic contexts, it is a fact that plate tectonics is ongoing, with different areas in uplift or subsidence. Here in Utah, the eastern half of the state has been in uplift for millions of years, raising former sealevel terrain that had geologically proven periodic shallow oceanic basins flooded repeatedly, lifted up, dried out to a basic salt flat, flooded again, and so forth, to make thousands of feet of salt beds, and now the region is oh 4000 feet above sea level or more. In the western half of Utah, although at a much earlier time it was shallow ocean, it was raised to significant elevation a hundred million years ago, and has been in subsidence for the past 50 million years. We go out to the trilobite beds in the West, and then go look for dinosaur bones in the East.
There is one other thing that is more important than any possible global warming trend on seashores, and that is wave erosion, storm erosion, the relentless reworking of material on the edges of the oceans. That is what has build beaches in the first place.
Even in the Pacific Atoll type of land formations, it could be uplift/subsidence that we are really looking at as the most important factor.
Of course, polar ice, or high latitude or high altitude land ice accumulations can be contributors as well, but I'm betting on the coming ice age. Go buy some seashore, but get the title of the plot to read "thence to the seachore" or you'll be left high and dry.
In the Great Basin, do not buy land in Salt Lake City unless you believe the State will build seawalls against a rising GSL shoreline. Right now the lake is as low as it has been in my lifetime, but it's been lower historically, and will rise again.
Those sand dunes around Barstow are interesting. In the legends of the natives, those lakes have come and gone a few times, and they're coming back, soon.