May 22, 2026

State of the Bay 2026: Examining Extreme Weather Events

Every three years, the Estuary Program gathers available monitoring and research data to track changes in our bay and watershed. The 2026 State of the Bay report contains a section focused on extreme weather events, which is an increasingly urgent topic of discussion as deviations from established weather patterns become more common. As part of the report, we take a closer look at extreme weather events within our watershed, predictions from the latest research and modeling, and discuss efforts underway to help us adapt to a changing climate.  

Record-Setting Rainfall

Local readers will likely remember the series of storms spanning December 2022 through March 2023, which caused significant flooding across the county. The peak of storm intensity was on January 9 when a  weather station at Cal Poly recorded 5.35 inches of rainfall within 24 hours. This was the second highest 24-hour total recorded at this station since 1990, just below the record storm in March 1995.  

Stage height is the depth of water in a creek. The graph shows maximum monthly stage height (ft) recorded by the gage at Canet Road, located at a bridge that crosses Chorro Creek. During the series of storms from December 2022 to March 2023 (orange bars), stage height reached its highest point of the decade. The dashed red line represents the height of the bridge along Canet Road. Frequent heavy rainfall coupled with groundwater saturation kept Chorro Creek significantly fuller than average for four consecutive months, contributing to persistent flood conditions.

 

Typically, we welcome rainfall in California as a relief from persistent droughts. However, the amount of rainfall that falls over a short period of time has important impacts. Intense, flashy storms can rapidly saturate the ground and contribute to significant runoff and flooding, as seen in winter 2023. Researchers believe that these events are becoming more common due to a warming atmosphere that can hold increasingly more water. This means that it takes longer for the atmosphere to become saturated with water, leading to wider gaps between storms and longer periods of dry weather that can extend droughts. When storms finally occur, there is a lot more water to release all at one time, increasing the flood risk.  

Rising Seas and Coastal Flooding

Flooding is not exclusive to  freshwater creeks. Projected increases in sea level range between 0.8 feet and 3.1 feet by 2100, depending on different global emissions scenarios. Coastal infrastructure is particularly vulnerable to sea level rise, and these vulnerabilities can be amplified during storm events. The flooding observed during the 2023 storms prompted the San Luis Obispo Council of Governments (SLOCOG) to develop plans for infrastructure improvements and habitat protection that address these changing conditions. 

SLOCOG partnered with Virtual Planet to construct models that display flood impacts on the lower-lying areas of Morro Bay along South Bay Blvd and State Park Rd. The models also demonstrate how infrastructure improvements, such as creating causeways to elevate the roads, can mitigate the impacts of coastal flooding.

 

In addition to the SLOCOG project, the Coastal San Luis Resource Conservation District (CSLRCD) is exploring nature-based solutions to increase the floodplain capacity of the Chorro Flats area to reduce the risk of future flooding. The US Geological Survey (USGS)  is also conducting sediment and water-level monitoring within the salt marsh to model impacts to sensitive habitats and identify strategies for protecting them from the encroaching tides.  

USGS developed the Coastal Storm Monitoring System (CoSMoS) to make predictions of coastal flooding so communities can be better prepared. The map above uses CoSMoS data to display the depth of water along the salt marsh during a rare, 100-year storm event. A flood like this would overtop the bridge spanning Chorro Creek along South Bay Blvd, known locally as Twin Bridges.

 

Learning from the Past

While modelling and making projections are helpful for understanding what the future might hold, looking into the past is valuable for understanding how ecosystems have historically adapted to change. The Estuary Program has partnered with the San Francisco Estuary Institute (SFEI) to examine past landscape conditions throughout the watershed as part of a historical ecology study. SFEI creates historical habitat maps using early written accounts from the 18th century, surveys and maps from the 19th to 20th centuries, and more recent aerial imagery. 

This map was drawn by hand for the United States Coast Survey in 1884. At this time, the estuary mouth was situated on the north side of Morro Rock, which was connected to the sandspit. Map “T-1662” courtesy of NOAA.

 

The goal of historical ecology is not to recreate the conditions of the past, but rather to learn from them so we can inform sustainable land management practices and guide future restoration projects. Against the backdrop of shifting weather patterns, rising sea levels, and infrastructure projects to keep coastal communities safe, we’re in for a great deal of change in a relatively short period of time. By contextualizing the past, we can make informed decisions that prioritize habitat preservation and protection.  

To learn more about these efforts, visit the State of the Bay webpage. 

References

California Ocean Protection Council. State Agency Sea Level Rise Action Plan for California. https://opc.ca.gov/wp-content/uploads/2024/02/SLR-Action-Plan-2024-Update-508.pdf  

CIMIS Weather Station 52 – San Luis Obispo: https://cimis.water.ca.gov/Stations.aspx  

SLO County Public Works Stage Height Gage at Canet Road: https://wr.slocountywater.org/sensor/?site_id=41&site=093f8e0b-dfde-4a45-b291-174ce07ead12&device_id=3&device=8e787d49-7f71-41b1-ae12-2559889f3431    

Morro Bay Estuary Climate Resiliency Transportation Plan: https://sbbclimateplan.org/  

Swain, D. L., Prein, A. F., Abatzoglou, J. T., Albano, C. M., Brunner, M., Diffenbaugh, N. S., Singh, D., Skinner, C. B., Touma, D. 2025. Hydroclimate volatility on a warming Earth. Nature Reviews: Earth & Environment. https://doi.org/10.1038/s43017-024-00624-z   


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