Anthony pointed out how the article is misleading, primarily relying on projections of computer models for sea level rise.
Kanik writes:
The U.S. States Geological Survey used two decades worth of satellite imagery of Ocean Beach in San Francisco — combined with models of sea levels rising from 1.6 to 10 feet due to global temperature increases — to estimate how the entire state’s coastline will shift in the next century.
That range is expected to vary based on the rate and reduction of carbon emissions over time.
While it may seem like that reality is in the distant future, the West Coast could see its sea levels rise up to eight inches in the next 25 years, according to the National Oceanic and Atmospheric Administration.
This claim is based on computer climate models predicting sea level rise (SLR), rather than looking at the trend of actual sea level observations. As Climate Realism has discussed repeatedly, climate models are seriously flawed. The most extreme projections of computer models simulations, RCP 8.5, those most likely used generate the highest SLR warned of, 10 feet by 2100, are not just exceedingly unlikely, they are likely impossible.
The article cites several locations along the California coast that are at greatest risk, including Humboldt Bay, Point Arena, Ocean Beach in San Francisco, Santa Cruz, Morro Bay, Pismo Beach, Newport Beach, and San Clemente.
Fortunately, real-world data exists in the form of tide-gauges on the U.S. West Coast. The sea level rise data is publicly available from the National Oceanic and Atmospheric Administration (NOAA) website known as Tides and Currents. Below in Figure 1, is a screen capture of that website showing tide gauges on the U.S. West Coast:
Figure 1: NOAA website map illustrates relative sea level trends at west coast stations, with arrows representing the direction and color the magnitude of SLR change.
Coastal Cliff Erosion and Geographical Factors: Coastal cliff erosion is a longstanding problem in California and is primarily driven by natural factors such as tides, weather, and land compaction and subsidence.
Understanding Coastal Cliff Erosion: Coastal cliff erosion refers to the gradual wearing away of cliffs and bluffs along the coastline due to various natural processes and human caused processes. While erosion can occur in different ways, coastal cliffs are particularly vulnerable due to the combined effects of weathering, wave action, and tidal forces.
Tidal Forces: Tides play a crucial role in coastal cliff erosion. The rise and fall of the tides expose the base of the cliffs to constant cycles of wetting and drying. This cyclical action weakens the stability of the cliffs and accelerates their erosion.
Storm Events and Coastal Damage: The article itself acknowledges that the damaged sections of coastlines mentioned were attributed to individual storm events rather than long-term climate change. The International Panel on Climate Change (IPCC) concludes that there is no evidence of increasing trends in severe weather events due to climate change. This further supports the argument that coastal damages in California are primarily caused by natural erosion, periodic extreme weather events, and unstable ground, rather than climate change.
Attributing any erosion solely to climate change oversimplifies the complex dynamics involved.
It is essential to critically evaluate the claims made in alarmist articles. The recent article from the Bay Area News Group (BANG) exaggerates the potential impact of climate change on California’s coastline, disregarding the long-established problem of coastal cliff erosion. By considering real-world data, including tide gauge observations and historical records, skeptics of climate change alarmism provide a more comprehensive perspective on the issue. It is crucial to differentiate between natural erosion processes and the influence of climate change to develop effective strategies for coastal management and protection.
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