Ocean Solstice

Animation by Hannah Whitman for Pelican of London.

Today, I’m telling a kid’s story about summer solstice below the waves to make a bigger point about how the ocean ecosystem and seasons interact.

Shoal of herring drawn using Cyberlink Power Director 365.
Sparkle and Shimmer in their shoal of herring. (Drawn using Cyberlink Power Director 365, (c) C Braungardt 2026).

Many different forms of tiny floating algae (diatoms) and tiny floating animals called copepods (a form of zooplankton) feeding on the algae.

Seals and seabirds feeding on herring feeding on copepods feeding on tiny algae – the ocean food web. (both drawn using Power Director 365 as above).

Ocean Solstice

We know the summer solstice marks the longest day and shortest night of the year – but what does it mean for the marine ecosystem? The story of Sparkle and Shimmer only tells part of the story.

The seasonal peak in daylight, solar energy and surface warming around the summer solstice contributes to the timing of high productivity, feeding and breeding behaviour in marine ecosystems, from microscopic algae (phytoplankton) and animals (zooplankton) to fish of all sizes, seabirds and marine mammals [1].

Phytoplankton at the base of the marine food web depend on the availability of sunlight, carbon dioxide and nutrients to grow. In spring, as days lengthen and the upper ocean becomes brighter, phytoplankton can multiply rapidly if enough nutrients are present. By the time of the solstice, many temperate and high-latitude waters have already experienced a major spring bloom. This bloom feeds zooplankton, which are then eaten by small fish, shellfish larvae and other animals. In this way, the extra daylight around the solstice helps fuel a chain of productivity that supports much larger species [2].

However, more sunlight does not always mean more growth. As the sun warms the sea surface, the upper layer of water becomes lighter and more stable, creating stratification. Stratification can be beneficial because it keeps phytoplankton near the well-lit surface, but it can also reduce the mixing that brings nutrients up from deeper water. Phytoplankton growth begins to slow after the spring bloom when nitrate, phosphate and silicate have been used up. In that case, ecosystems shift from intense bloom conditions to a more nutrient-limited summer state around and after the summer solstice [1].

Longer days and warmer surface waters affect breeding, feeding and migration patterns of many marine animals. For example, fish time their spawning so that their larvae hatch when plankton prey are abundant. Seabirds raise chicks during this period of high productivity, feeding on large zooplankton and fish. Marine mammals follow seasonal movements of fish and gather in feeding grounds where summer productivity is high. One dramatic example of the latter is the migration of the great whales to polar seas to feed on krill and herring in near-continuous daylight to build reserves that must sustain the animals through much of the year [3].

Such seasonal behaviour makes ecosystems vulnerable to the effect of human activities: in particular, climate change is altering some of the natural patterns associated with the solstice. Warmer seas can strengthen stratification, shift the timing of algal blooms and change which species thrive in a given location. If plankton blooms occur earlier than the hatching of fish larvae or the breeding of seabirds, food webs become mismatched. Marine heatwaves before the height of summer may also stress kelp forests, corals and cold-adapted species, which are important breeding grounds for many marine species. The location and type of food sources may shift, with potentially dire consequences for predators and their fecundity [4].

So, the summer solstice is not just a marker of the longest day, it is part of a wider seasonal rhythm that governs light, temperature, nutrients and life cycles across marine ecosystems. Its influence is powerful when the natural balance between sunlight, ocean mixing and temperature is in tact. The ability of marine species to keep pace with a changing climate is becoming a key factor shaping the future of the ocean ecosystem [5, 6].

References

[1] NASA. no date. Plankton Blooms – the good, the bad and the shiny. Nasa Earthdata CZCS Classic Scenes. [online] https://www.earthdata.nasa.gov/data/instruments/czcs/classic-scenes/plankton-blooms-good-bad-shiny

[2] NOAA. 2026. Aquatic food webs. National Oceanic and Atmospheric Administration. [online] https://www.noaa.gov/education/resource-collections/marine-life/aquatic-food-webs

[3] Hodgson BR. 2005. Global importance of supporting the krill to whale component of the pelagic food web associated with migrations following deep sea seamounts. International Marine Science Journal, 1(3), 17-33.[online] https://openaccesspub.org/article/2201/imsj-25-5590.pdf

[4] MB&S. no date. Marine heatwaves are pushing ocean life to the breaking point. Marine Biodiversity & Sustainability Learning Center. [online] https://www.marinebiodiversity.ca/marine-heatwaves-are-pushing-ocean-life-to-the-breaking-point/#google_vignette

[5] NOAA Fisheries. no date. Oceans and climate change: Tracking and predicting the impacts. National Oceanic and Atmospheric Administration. [online] https://www.fisheries.noaa.gov/topic/climate-change/understanding-the-impacts

[6] Cheng L et al. 2025. Ocean stratification in a warming climate. Nature Review – Earth and Environment 6, 637-655. [online] https://www.nature.com/articles/s43017-025-00715-5

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