LA Surf Lines Up at El Porto (finally)

El Porto gets all-day offshore winds, and we surf back-to-back sessions. In this vlog, I break down the difference between long-period swells and short-period swells (surf education), explain onshore vs. offshore wind, and why conditions like this are so rare in Los Angeles (plus I show you my favorite post surf breakfast burrito spot near El Porto). Matt Pagan steals my surfboard, and things nearly go sideways when we catch a gnarly surfing accident on film during a crowded LA lineup. If you surf LA, or just want to understand why some days work and most don’t, this one’s worth a watch.

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follow on IG: @hunterjoness

Surfers in this video:
• Hunter Jones
• Tim Laney
• Matt Pagan
• Dylan Morrisroe
• Ben Cohen
• Juliano Uzuelli
• Dane Acosta
• Tim Laney

Filmed by:
Cameron Nelligan

Additional footage:
Brad Jacobson

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los angeles surf, la winter surf, first swell of the year, january surf, california surf vlog, surf barrels la

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Barrier Builders: Tidal Sediment and Erosion Sculpting Coastal Sandbar Formations and Shoals

Understanding Sandbar Formations

Sandbar formations are fascinating natural structures that play a crucial role in shaping our coastal landscapes. These underwater ridges, composed primarily of sediment, are formed by the continuous action of tides and currents. As tidal waters move in and out, they transport and deposit sediment, gradually building up these barriers and shoals that define the coastal regions.

The Role of Tidal Forces

Tidal forces are the primary drivers behind the formation of sandbars. The ebb and flow of tides create dynamic water movements that redistribute sediment along the coastline. During high tide, water levels rise, allowing sediment to spread out, while low tide exposes these sediments, leading to their accumulation in specific areas. This cyclic process is essential in shaping the barriers and shoals that protect inland areas from the direct impact of ocean waves.

Sediment Distribution and Coastal Protection

Sediment plays a pivotal role in the development of sandbar formations. The size, type, and availability of sediment materials determine the stability and growth of these structures. Fine sands tend to form extensive, gentle sandbars, while coarser materials can lead to the creation of more resilient and pronounced barriers. These sandbars act as natural buffers, absorbing wave energy and reducing coastal erosion, thereby safeguarding coastal ecosystems and human settlements.

Erosion and its Impact on Sandbar Stability

Erosion is a natural process that influences the longevity and shape of sandbar formations. Strong wave action and storm events can erode these barriers, altering their structure and position. However, erosion also contributes to the continuous reshaping and dynamic nature of coastal environments. Understanding the balance between sediment deposition and erosion is key to managing and conserving these valuable coastal features.

Barriers and Shoals: Distinguishing Features

While often used interchangeably, barriers and shoals have distinct characteristics. Barriers are elongated landforms that run parallel to the coastline, providing significant protection from oceanic forces. Shoals, on the other hand, are elevated areas of shallow water that can extend offshore, posing navigation challenges but also contributing to coastal protection. Both barriers and shoals are integral components of the complex interplay between tidal movements, sediment supply, and coastal dynamics.

The Future of Sandbar Formations

As coastal areas face increasing pressures from human activities and climate change, understanding the formation and maintenance of sandbars becomes more critical. Sustainable coastal management practices are essential to preserve these natural barriers, ensuring they continue to provide protection and maintain the ecological balance. Future research and innovative conservation strategies will play a vital role in safeguarding sandbar formations for generations to come.