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[1]
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Catastrophic beach sand losses due to erosion from predicted future sea level rise (0.5–1.0 m), based on increasing submarine accommodation spaces in the high-wave-energy coast of the Pacific Northwest, Washington, Oregon, and Northern California, USA
Marine Geology,
2021
DOI:10.1016/j.margeo.2021.106555
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[2]
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Catastrophic beach sand losses due to erosion from predicted future sea level rise (0.5–1.0 m), based on increasing submarine accommodation spaces in the high-wave-energy coast of the Pacific Northwest, Washington, Oregon, and Northern California, USA
Marine Geology,
2021
DOI:10.1016/j.margeo.2021.106555
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|
|
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[3]
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Catastrophic beach sand losses due to erosion from predicted future sea level rise (0.5–1.0 m), based on increasing submarine accommodation spaces in the high-wave-energy coast of the Pacific Northwest, Washington, Oregon, and Northern California, USA
Marine Geology,
2021
DOI:10.1016/j.margeo.2021.106555
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|
|
|
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[4]
|
Catastrophic beach sand losses due to erosion from predicted future sea level rise (0.5–1.0 m), based on increasing submarine accommodation spaces in the high-wave-energy coast of the Pacific Northwest, Washington, Oregon, and Northern California, USA
Marine Geology,
2021
DOI:10.1016/j.margeo.2021.106555
|
|
|
|
|
[5]
|
Catastrophic beach sand losses due to erosion from predicted future sea level rise (0.5–1.0 m), based on increasing submarine accommodation spaces in the high-wave-energy coast of the Pacific Northwest, Washington, Oregon, and Northern California, USA
Marine Geology,
2021
DOI:10.1016/j.margeo.2021.106555
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|
|
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[6]
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Late-Holocene shoreline responses to competing shelf, bay, and beach accommodation spaces under conditions of relative sea level change, and the potential for future catastrophic beach retreat in the Columbia River Littoral Cell, Washington and Oregon, USA
Marine Geology,
2020
DOI:10.1016/j.margeo.2020.106272
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