The oceans are warming at an alarming rate. 2023 shattered records across the world’s
oceans, and was the first time that ocean temperatures exceeded 1oC
over pre-industrial levels. This led to the emergence of a series of marine
heatwave events across both hemispheres, from the waters around Japan, around
South America, and across the wider North Atlantic. Marine heatwaves are periods of extremely warm sea temperatures that
can form in quite localized hot spots but also span large parts of ocean
basins. By definition, they have to last five days to be classed as a
marine heatwave, but some major events have lasted months — even years, in an
extreme case.
Notable
events have led to catastrophic impacts on marine ecosystems, the economy and
coastal communities. For example, coral bleaching in the tropics has caused
huge losses to the tourism industry, mass mortalities or major shifts in
fisheries have impacted fishing industries worldwide, and vast losses of sea
grass meadows and kelp forests have decimated countries’ natural capital.
The
UK has largely escaped any major marine heatwaves that could have caused
notable impacts to marine ecosystems and the blue economy. However, in June
2023 a short-lived but intense event materialized around the shores of the UK
and Ireland, which was widely documented in the media. The impacts of this heatwave remain unknown, highlighting a crucial gap
in our understanding of past marine heatwaves’ characteristics around the UK
and what their potential future impacts may be.
In our new article, we characterized both
marine heatwaves and their opposites — marine cold spells — around the UK for
the first time… On
average, the southern North Sea and English Channel tend to experience longer
(around a month) and moderately intense (maximum temperatures reaching 1.5oC
higher than expected) heatwaves, whereas the eastern North Sea has a tendency
to experience shorter (two to three weeks) but more intense (maximum
temperatures >3oC) heatwaves.
Marine heatwaves are documented all around the
UK, lasting up to five months and occurring throughout the year, even in winter. When investigating individual events, it is
evident that considerable variability exists in terms of location, intensity,
duration and time of year. This high variability may also explain the
inconsistent response in chlorophyll-a, a proxy for phytoplankton abundance.
Our
research reveals that chlorophyll-a extremes do not coincide with temperature
extremes in UK waters, although there is some indication that highly productive
events, for which we have coined the term ‘greenwaves’, occur more frequently
in the southern North Sea and closer to the coast. For the wider North
Atlantic, marine heatwaves are more likely to co-occur with ‘bluewaves’ (low
chlorophyll-a extremes) in the tropics and subtropics, while cold spells are
more likely to co-occur with greenwaves at higher latitudes. The direct
relationship between these types of extremes is inconsistent and needs more
investigation around the UK. This may be due to the UK residing between mid- to
high latitudes. Seasonality may also
play a vital role.
The
timing of events will also greatly affect the impacts on the wider marine
ecosystem… But if an event were to occur in winter or spring, the unseasonably
warm temperatures may initiate phytoplankton blooms, possibly leading to either
a temporary boost in productivity, greatly benefiting fisheries, or causing
harmful algal blooms, leading to negative impacts.
Our research also shows that when marine
heatwaves occur in the relatively shallow southern North Sea and English
Channel, near-bottom oxygen concentrations tend to be extremely low, which puts
benthic ecosystems under increased stress. For other locations around the UK, this
relationship is apparent during the first half of the year, where the water
column is well-mixed and the impact of extreme surface temperatures is able to
reach the seafloor. During summer, the water column is not as well mixed,
keeping the impacts of the marine heatwave confined to the surface.
Given
the complexity of this region, it is vital that more targeted research is
undertaken to understand the future impacts of marine heatwaves on marine ecosystems,
the blue economy and society. If high-risk regions can be identified, the
resilience of species and coastal communities can be assessed and properly
managed.
The June 2023 marine heatwave should be
perceived as an alarm bell. While these events do not appear to be as long-lasting or intense as other
heatwaves around the world at the moment, they are projected to increase. This
means that the UK is presented with a unique opportunity to take advantage of
our head start and learn from other nations to increase preparedness and
response capability for future extreme events.