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Thermohaline Circulation and Cold-Water Surges in San Diego's Bays

Understand how thermohaline circulation drives cold-water surges in San Diego bays and affects your outdoor activities year-round.


Thermohaline Circulation and Cold-Water Surges in San Diego’s Bays

San Diego’s consistently mild climate masks one of the most dynamic oceanographic processes happening beneath our bays: thermohaline circulation. This deep-ocean conveyor system drives periodic cold-water surges that dramatically shift water temperatures, affect marine life distribution, and reshape conditions for surfers, swimmers, paddlers, and divers throughout the year.

What Is Thermohaline Circulation?

Thermohaline circulation is the global ocean’s “conveyor belt,” driven by differences in water temperature (thermo-) and salinity (-haline). Cold, dense water sinks at the poles, travels along the ocean floor, and upwells in other regions where it displaces warmer surface water. San Diego sits at a critical intersection: we’re influenced by the California Current, which brings cold water from the north, and by localized upwelling that brings nutrient-rich, frigid water from the deep.

The California Current itself is part of this larger thermohaline system. It flows south along our coast, bringing water that originated in the North Pacific. When this system intensifies—particularly in spring and summer—San Diego’s bays experience pronounced cold-water surges that can drop temperatures 10–15°F in days.

How Upwelling Works in San Diego Bays

Upwelling is the local manifestation of thermohaline circulation that most directly affects your time on the water. When northwesterly winds blow consistently along the coast, they push warm surface water offshore. Cold, deep water rises to replace it—a process called Ekman transport. This is most pronounced at headlands and near submarine canyons where bathymetry funnels deep water toward shore.

Mission Bay and San Diego Bay experience milder upwelling than the open coast, but both can see significant temperature drops. Mission Bay typically stays 2–5°F warmer than the Pacific because its enclosed geography limits exposure to offshore wind stress. However, strong spring wind events can still drive noticeable cold surges into Mission Bay within 48 hours.

Point Loma and the kelp beds off La Jolla are ground zero for upwelling. The Point Loma submarine canyon acts as a natural conduit for deep water. Divers and surfers who know this spot report temperature swings of 10°F or more between spring and early summer as upwelling intensifies.

Seasonal Patterns in San Diego

Spring (March–May): This is prime upwelling season. Northwesterly winds strengthen, and the thermohaline system’s influence peaks. Water temperatures in Mission Bay can drop from 60°F to 52°F by May. The open coast becomes significantly colder, often dipping into the high 40s. This is when booties and thicker wetsuits become non-negotiable for water sports enthusiasts.

Early Summer (June–July): Upwelling remains strong through June, often creating the coldest water of the year. July can bring brief warming as upwelling temporarily weakens, but the trend reverses by late July. Water temperatures in Mission Bay typically range from 55–62°F.

Late Summer and Fall (August–October): Upwelling gradually weakens as the season turns. Thermohaline circulation slows, and warmer surface water begins to dominate. By September, Mission Bay warms to 65–70°F. This is the warmest water of the year and the most comfortable window for swimming and paddling without thermal protection.

Winter (November–February): Thermohaline circulation weakens further, but winter storms can trigger localized upwelling events. Water temperatures stabilize around 58–62°F in Mission Bay. While not as cold as spring, it’s still cool enough to require a wetsuit for extended water time.

Practical Implications for Athletes

Surfers: Cold-water surges in spring and early summer improve wave quality by intensifying atmospheric pressure gradients. Expect better swell windows during May and June when upwelling peaks. The tradeoff: you’ll need at least a 4/3mm wetsuit, and 5/3mm is safer for extended sessions at spots like Sunset Cliffs or Swami’s.

Swimmers and Paddlers: Late summer and early fall (August–September) offer the most comfortable open-water conditions. If you’re training in Mission Bay during spring, expect core temperatures to drop faster than the air temperature suggests. Plan shorter sessions and monitor your body’s response.

Divers: Cold-water surges bring nutrient-rich conditions that attract fish and kelp growth. Visibility can actually improve as upwelled water is cleaner than warm, stagnant surface water. However, deeper dives in spring require 7mm wetsuits or drysuits, especially if you’re working below 40 feet where temperatures drop another 5–10°F.

Monitoring Conditions with Element

Thermohaline circulation and upwelling don’t announce themselves. Water temperature can shift dramatically in 24 hours based on wind patterns and larger oceanographic cycles. Checking real-time conditions before heading out—wind direction, water temperature trends, and swell forecasts—helps you prepare appropriately and predict when cold surges are likely.

The Element app tracks San Diego’s water temperatures, wind patterns, and local conditions across Mission Bay, San Diego Bay, and the open coast. Use it to anticipate cold-water surges and plan your sessions around the thermohaline rhythm that defines our year.