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Climate Change Likely to Worsen Impact of Urban Runoff on Southern California Ocean

Published on: 11/09/2021
Primary Contact(s): kimberly.puglise@noaa.gov

The downtown Los Angeles skyline. Credit Wikimedia Commons.

An NCCOS-funded study found that nutrient-laden, urban runoff is fueling algal blooms in Southern California's coastal waters that are acidifying the water and depleting it of oxygen, making habitat unsuitable for marine organisms. The research team's modeling shows the trend is likely to worsen under future climate change scenarios.

The Southern California Bight, an area of ocean located between the Baja Peninsula and Point Conception in Santa Barbara County, borders a population of 23 million people, including the Greater Los Angeles area, that discharges approximately 8 million cubic meters of nutrient-enriched stormwater and wastewater into the ocean each day. Considering that the U.S. West Coast is already experiencing increased hypoxia (low oxygen) and acidification from climate change, the effect of local human nutrient inputs exacerbates this trend.

The research is the result of multiple projects funded by NCCOS (under the Ecology and Oceanography of Harmful Algal Blooms Program, and the Coastal Hypoxia Research Program) and NOAA's Ocean Acidification Program (Ocean Acidification and Hypoxia).

Effects on coastal eutrophication in the Southern California Bight (A–C) Four-year averages (January 1997 to December 2000) of surface chlorophyll concentration (mg Chl m−3) from remote sensing and in situ data (A; filled circles are CalCOFI and POTW agency observations, and color contours satellite data) and from the ANTH and CTRL simulations respectively (B and C). CalCOFI = California Cooperative Oceanic Fisheries Investigations; POTW = publicly owned treatment works; CTRL = Weather Research and Forecast Model simulations with natural ocean cycles of regional biogeochemical dynamics in the absence of terrestrial nutrient inputs; ANTH = Weather Research and Forecast Model simulations of regional biogeochemical dynamics including inputs of dissolved inorganic and organic nitrogen and phosphorus, silicate, iron, and inorganic and organic carbon from rivers, wastewater outfalls, and atmospheric deposition. Credit: Kessouri et al 2021.

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