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Developing the least damaged/more natural data
layer
Least damaged/more natural workshop
Pete Chaniotis
Joint Nature Conservation Committee
What is ‘least damaged/more natural’?
• A policy approach from Sustainable Seas for All
• Scottish MPA Selection Guidelines will be applied to least damaged/more natural areas first before being applied more widely
– Identification of areas containing features which are potentially in better condition
– Identifying opportunities in areas of least activity
How was the least damaged/more natural layer developed?
• Features are sensitive to pressures that may be associated with activities
• Need to know: – The degree to which MPA search features are
sensitive to pressures– Which activities may be associated with those
pressures
• Collation of marine activities data to provide information on the extent of pressures occurring in Scotland’s seas:
• Range of sources:
– Defra-led contract ‘MB106’– JNCC data verification work– State of Scotland’s Seas
How was the least damaged/more natural layer developed?
• Assigning physical extent/pressure footprints to marine activities data
– Effects of activities may extend beyond the area over which they are undertaken
• Not possible in all cases:– Marinas, ports and harbours, coastal quarrying sites,
beach replenishment sites, munitions dumping ground points, power stations
• Represents activities currently taking place in Scotland’s seas
• Interpreted within the context of future interest areas
How was the least damaged/more natural layer developed?
Methodology
Principles
• Areas of approximately one grid cell or less were generally removed
• Areas which overlapped with known existing activity not incorporated into the production of the layer were generally removed
• Intertidal areas/thin coastal strips removed due to scale/data resolution issues
• Removal of areas which were heavily divided, e.g. subdivisions of some sea lochs by fishing activity/parts of the North Sea by oil and gas activity
• Larger, offshore areas subdivided using large scale units or common bathymetry
Mersehead Sands and Outer Solway Firth
Wigtown Bay
East Orkney
Norwegian boundary sediment plain
Montrose Field
East of Gannet Field
Greater & Lesser East of Marr & Montrose Bank
St Andrews Bay & Eden Estuary
Faroe-Shetland Channel
North Orkney to Fair Isle
North-east of Fair Isle
Waters around Roussay
Inshore South Isles - Orkney
Loch Sween
Loch Nevis & Loch Hourn
Loch Long & Loch Duich
Loch Carron
Loch Torridon
Loch Tarbert
Lochs a Chairn Bhairn, Glencoul & Glendhu
West MPA Region (islands and offshore)
Stanton Banks to South West St Kilda
Between Monach Islands and St Kilda
West of Outer Hebrides
North West Islay & Laggan Bay
East of Benbecula & North Uist
North West Tiree inc. Skerrymore
Darwin Mounds
Rockall Basin
Anton Dohrn Seamount
North West Rockall Bank
Sediment plain North of George Bligh BankHatton-Rockall
Basin
Hatton Bank
Far West Approaches
Limitations and caveats
• The data– Recognised gaps – Represents a snapshot of where and how Scotland’s seas
are being used– High-level assessment as opposed to something more
detailed
• The method– Intensity at which activities occur not considered – Cumulative effects not considered
[email protected] - Scottish [email protected] - Territorial [email protected] - Offshore waters