Crown

Fishing pressures can be managed using spatial measures such as prohibiting or restricting certain types of fishing, target species, or vessel capacity. This dataset depicts restrictions on fishing of BASS defined by EU, UK and Scottish legislation since 1986. Polygons were simplified for web use and are for illustrative purposes only. Guidance should be sought from Fishery Offices on interpreting legislation.
 

UKCP09 is the name given to the UK Climate Projections. UKCP09 provides future climate projections for land and marine regions as well as observed (past) climate data for the UK.This layer is part of the Sea Surface and Seabed Temperature Change  sub-set of the UKCP09 marine and coastal projections up to 2090s using a medium emission scenario and, where appropriate, medium probability. It displays the change in sea surface salinity for winter up to 2085 under a medium emissions scenario.

Summarising the anticipated changes around Scotland based on central estimate projections for 2080-90 using the medium emission scenario, surface salinity is projected to decrease everywhere, and in fact around the entire north east Atlantic, by about 0.2 salinity units. This decrease is mainly due to wide scale changes in the ocean rather than the local effect of rivers. There is very little regional or seasonal variability.

UKCP09 is the name given to the UK Climate Projections. UKCP09 provides future climate projections for land and marine regions as well as observed (past) climate data for the UK.This layer is part of the Sea Surface and Seabed Temperature Change  sub-set of the UKCP09 marine and coastal projections up to 2090s using a medium emission scenario and, where appropriate, medium probability. It displays the change in sea surface temperature for Autumn up to 2085 under a medium emissions scenario.

Summarising the anticipated changes around Scotland based on central estimate projections for 2080-90 using the medium emission scenario, sea surface temperature is projected to be between 2 and 2.5ºC warmer although in summer north and west of Scotland may be only 1ºC warmer. The autumn seems to be when most warming will be evident. At the sea bed, warming is similar as at the surface, but only on the shallow continental shelf. In the deep waters surrounding Scotland, off the shelf, temperatures are projected to change very little. There is quite a lot of both regional and seasonal variation in temperature change.

UKCP09 is the name given to the UK Climate Projections. UKCP09 provides future climate projections for land and marine regions as well as observed (past) climate data for the UK.This layer is part of the  Stratification Changes sub-set of the UKCP09 marine and coastal projections up to 2090s using a medium emission scenario and, where appropriate, medium probability. It displays the Change in the Start Date of Stratification to 2085 under a medium emissions scenario.

Summarising the anticipated changes around Scotland based on central estimate projections for 2080-90 using the medium emission scenario for Stratification, it is projected that it will start earlier, possibly by as much as 5 to 10 days. However, there are exceptions to this pattern, such as in the Tay / Forth area, west of the Hebrides, and some other local inshore areas. In the offshore waters, stratification will end later in the year, by possibly as much as 10 to 15 days. In inshore waters again there is quite a complex pattern in the projected changes. The length of the stratified period in offshore waters is generally 10-15 days longer than currently, with some local, inshore variation.