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Surging Sargassum Overwhelms Half of Tourist Beaches in Quintana Roo, Leaving Just Five Unscathed by Microalgae

Climate change, elevated nutrient levels in the water, and altered ocean currents contribute to the proliferation of Sargassum.

Marine blooms of Sargassum seaweed are a consequence of rising temperatures, heightened nutrient...
Marine blooms of Sargassum seaweed are a consequence of rising temperatures, heightened nutrient levels in the water, and altered ocean currents.

Surging Sargassum Overwhelms Half of Tourist Beaches in Quintana Roo, Leaving Just Five Unscathed by Microalgae

Sargassum Invasion Overrunning Tourist Beaches in Northern Quintana Roo

In the recent week, a stunning 50 out of 100 tourist beaches in northern Quintana Roo have been invaded by excessive sargassum levels, according to the Sargassum Monitoring Network Kinich Ka'an Ojo del Cielo. Let's dive into the reasons behind this unwelcome guest and its impact.

The ever-growing problem of sargassum isn't a solitary matter, but a complex interplay of environmental, climatic, and regional factors. These factors mainly fall under three categories: oceanic and atmospheric conditions, regional events and climatic anomalies, and nutrient inputs.

Oceanic and Atmospheric Conditions

Rising Sea Temperatures: Climate change has led to warmer oceanic waters, providing an ideal environment for the rapid growth and increased biomass of sargassum.

Trade Winds and Ocean Currents: Easterly trade winds and the Atlantic Ocean's currents transport vast mats of sargassum from its breeding grounds to the Caribbean coasts, including those of Quintana Roo.

Seasonal Timing: The sargassum season, lasting from March to September (with peak months in May–August), is when the perfect conditions for proliferation, transport, and accumulation converge.

Regional Events and Climatic Anomalies

North Atlantic Oscillation (NAO): Back in 2009–2010, an extreme negative phase of the NAO possibly contributed to sargassum's seeding into new territories by altering ocean circulation patterns. This could have set the stage for recurring surges.

Regime Shifts: The past decade has seen a marked shift in sargassum proliferation patterns, with blooms now appearing more often and at larger scales.

Nutrient Inputs

Historically, rivers like the Amazon and Orinoco were suspected to be major contributors to sargassum levels. However, recent research suggests nutrients from these rivers make up only about 10% of total sargassum biomass. Other sources like coastal upwelling or localized pollution might play secondary roles.

The mass influx of sargassum greatly affects both the natural environment and local economies, particularly tourism. It also poses threats to marine life and coastal infrastructure. To counteract this issue, efforts like barriers and cleanup operations are being carried out in Quintana Roo.

In conclusion, the grand increase in sargassum levels in Quintana Roo's tourist beaches is primarily due to a combination of warmer ocean temperatures, altered ocean currents, a notable oceanographic event in 2009-2010, and favorable seasonal wind and current patterns. Riverine nutrient contributions, though significant in the past, now seem to play a smaller role than previously thought [1][4][5].

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For more in-depth understanding, check out:

  • Salmerón-Zárate, A., Edwards, R., 2022. Impacts of the sargassum (Sargassum spp.) invasion on Caribbean coasts. Marine Pollution Bulletin 165(105011), 105011.
  • Bell School, The Australian National University, 2022. The Drivers of Sargassum in the Caribbean: Climate Change and Human Activities [online]. Available at: https://researchtopolicy.anu.edu.au/sargassum-invasion-in-the-caribbean. [Accessed 22 August 2022].

The ongoing sargassum invasion in northern Quintana Roo's tourist beaches is closely linked to climate change, as warmer ocean temperatures contribute to the rapid growth and increased biomass of sargassum. Additionally, the sargassum issue is interconnected with the science of weather and environmental science, as Easterly trade winds and ocean currents transport the seaweed from its breeding grounds, influenced by seasonal timing and climatic anomalies like the North Atlantic Oscillation.

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