In the UK Initial Assessment 2012 (HM Government, 2012), long-term positive salinity trends were observed at the bottom waters of the northern North Sea. From 2011 a sharp decrease in salinity of the adjacent Atlantic waters was measured, which may reduce (or reverse) the long-term increases salinity reported in the previous assessment.
Salinity affects marine ecosystems in many ways. Together salinity and temperature control water density affecting circulation patterns and the distribution and timing of stratification.
Changes in salinity in UK waters are largely influenced by changes in the global circulation and currents driving variability in flows between the North Atlantic and European shelf seas. Salinity is also influenced by changes in the balance between precipitation and evaporation. Salinity in coastal regions can be strongly influenced by seasonal and inter-annual variability in the freshwater input by rivers.
In the UK Initial Assessment (HM Government, 2012) an increase in the salinity of the north-western UK waters was related to a stronger inflow of subtropical waters in the area. Similarly, the deep waters of the northern North Sea were shown to be increasing salinity related to the inflow of these Atlantic waters. The coastal areas in the southern North Sea are more influenced by river inputs and they presented more variability and few clear trends except in the German Bight (beyond UK waters but included for context in the last assessment) where winter conditions were freshening in the presence of large year to year fluctuations. No clear trend in salinity was observed in the Western Channel or in the Irish Seas.
Here we make the assessment using long-term salinity time series records at the West Channel Observatory, Rockall Trough, Faroe Shetland Channel, Fair Isle, Felixstowe and Helgoland Roads (included for broader context in the southern North Sea) which are published in the ICES Report on Ocean Climate.
The winter bottom salinities are measured in the North Sea by the ICES International Trawl Survey Quarter 1 and shown for the period 1971-2012.
The UK Climate Projections (2009) suggested that the salinity will slightly decrease in the future in the shelf seas and adjacent ocean (a decrease of approximately 0.2 by 2070-2098). Change is thought to be weaker in the Celtic and Irish Sea (approximately 0.1). The uncertainty of salinity in these projections is very high and will likely change as models develop.
The salinity of the upper ocean (0-800m water depth) to the West and North of the UK has generally increased over the last 4 decades but decreased sharply from 2011 on, reaching values below the long-term mean (1981-2010) in 2014 in Rockall Trough and in 2013 and 2015 in the Faroe-Shetland Channel (Figure 1 and 2). This decrease in salinity is consistent with the short-term decrease in temperature reflecting a changing balance of the inflow of subtropical (salty) versus subpolar (fresh) water into the area.
In the northern North Sea (Fair Isle station), salinity is influenced by the inflow of Atlantic water with significant year-to-year variations. No clear long-term trend is observed in the Fair Isle current, but in 2013-2015 salinity was below the long-term mean.
For the Southern North Sea, salinity is controlled by a balance of freshwater supply from the surrounding catchments in the UK and Northern Europe and by changes in the transport of Atlantic origin water through the Dover Strait and from the north. Two stations are available in the Southern North Sea, one near Felixstowe (UK) and Helgoland (Germany), which both demonstrate high interannual variability, experienced a notably fresh period in the 1980s, and show no clear trend since they recovered to a more typical salinity in the 1990s. Figure 1 illustrates the salinity anomalies at the stations described above with respect to the standard deviation of the period 1981-2010.
To the west of the UK in the Rockall Trough the water at depths greater than 1500m have been freshening over the last 40 years. This is thought to be a lagged effect of the freshening of the Labrador Sea (where this deep water is formed).
Linear trends in winter bottom-water salinity of the North Sea have been analysed for the period 1971-2012 (Figure 3) and show increasing salinity in the north of the area. The trend is weaker further south where the spatial variability is also relatively high. This positive trend in the northern North Sea is likely to be related to the increasing salinity observed in North Atlantic waters up to 2011.
Salinity in UK seas is the result of a combination of adjacent oceanic water and freshwater inputs from rivers and net rainfall minus evaporation. Deep ocean stations around the UK (Rockall Trough and Faroe Shetland Channel) show that the adjacent Atlantic waters have been freshening since 2011. This is likely to alter the long-term trend in salinity observed at the bottom waters of the northern North Sea, however the current analysis is too short to make this a confident finding. For the northern North Sea and southern North Sea observations of salinity find very high year-to-year variability. While no clear long-term trend is evident, conditions in the northern North Sea station were notably fresher than the long-term average in 2013 to 2015.
Salinity data are generally sparse in comparison to temperature data and so confidence in the assessments of long-term trends and spatial variability is lower. Data is particularly scarce in deeper waters both on and off the European shelf. Further under-sampling of seasonal variability adds difficulty for interpreting long-term change. The Argo float programme and installation of thermo-salinographs on ferries and voluntary observing ships will help to reduce this gap for the deep ocean and shelf seas waters, respectively. Emerging technologies, such as autonomous gliders and integrating observations with models will help fill the gaps for future assessments. Uncertainties in shelf sea salinity associated with the supply of freshwater from rivers, rainfall and climate change are areas where our understanding can be improved.
HM Government (2012) ‘Marine Strategy Part One: UK Initial Assessment and Good Environmental Status’ (viewed on 5 July 2018)
The information, figures and all the results presented in this assessment has been extracted from the following reports:
ICES Report on Ocean Climate 2015:
Larsen KMH, Gonzalez-Pola C, Fratantoni P, Beszczynska-Möller A, and Hughes SL (Editors) (2016) ‘ICES Report on Ocean Climate 2015’ ICES Cooperative Research Report Number 331, 79 pages (viewed on 14 January 2019)
Charting Progress 2 report for temperature and salinity:
UKMMAS (2010) ‘Temperature and Salinity’ Charting Progress 2 Feeder Report: Ocean Processes, Huthnance J (editor). Department for Environment Food and Rural Affairs on behalf of the UK Marine Science Co-ordination Committee (viewed on 14 January 2019)
UK Marine Climate Change Impacts Partnership Science Review 2013 for salinity:
Dye SR, Holliday NP, Hughes SL, Inall M, Kennington K, Smyth T, Tinker J, Andres O, Beszczynska-Möller A (2013) ‘Climate change impacts on the waters around the UK and Ireland: Salinity’ MCCIP Science Review 2013, 60-66. doi:10.14465/2013.arc07.060-066 (viewed on 14 January 2019)
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