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Ocean glider reveals a deeper North Sea heatwave response

A Bangor co-authored study measured a sustained rise in subsurface chlorophyll during the June 2023 heatwave, beyond the brief surface signal seen by satellites.

Christine Jones ·

Bangor University’s main building, 29 May 2024. Archive institutional context, not the North Sea, the glider or the 2023 fieldwork. Tilman2007 / Wikimedia Commons, CC BY-SA 4.0; cropped.

Bangor University’s main building, 29 May 2024. Archive institutional context, not the North Sea, the glider or the 2023 fieldwork. Tilman2007 / Wikimedia Commons, CC BY-SA 4.0; cropped.

Original photographCC BY-SA 4.0

An ocean glider detected a sustained increase in chlorophyll below the North Sea’s surface during the June 2023 marine heatwave, in research co-authored by Bangor University’s Professor Tom Rippeth. The university highlighted the findings on 15 October.

Why depth mattered

Satellite observations showed a short-lived rise near the surface. The glider’s measurements captured a stronger, longer-lasting subsurface response, showing why observations through the water column add information that surface monitoring misses.

The measured signal

The paper reports typical post-bloom subsurface chlorophyll concentrations of 1 to 2 milligrams per cubic metre, compared with concentrations above 3 and short peaks above 9 during the heatwave. Chlorophyll is the measured pigment signal; these figures do not establish a matching increase in fish numbers or carbon stored.

Dates and scientific limits

The National Oceanography Centre-led paper appeared in Communications Earth & Environment on 8 October. The publisher identifies it as accepted, peer-reviewed research released early, with further edits possible before the final version. The observations concern one North Sea heatwave, rather than conditions in Welsh waters today. The abstract describes possible transport and light influences, not one proven cause for every marine heatwave.

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