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Areas where fishing of QUEEN SCALLOPS is restricted

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 of QUEEN SCALLOPS 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.
Other area based measures contributing to the MPA network

A Marine Protected Area network is designed to conserve a scientific selection of both marine biodiversity (species and habitats) and geodiversity (the variety of landforms and natural processes that underpin the marine landscapes), offering long-term support for the services our seas provide to society. In the 2012 "Report to the Scottish Parliament on Progress to Identify a Scottish Network of Marine Protected Areas", eight fisheries restriction areas were considered to contribute to the MPA network as existing "other area based measures".  Four of these areas overlap with Special Areas of Conservation (SACs) and have now been removed from the list.
Areas where fishing of BASS is restricted

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 Projections - Percent change in winter precipitation, 2080s compared to 1970s, 50% probability level

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 Precipitation and Air temperature 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 projected change in winter precipitation (50% probability level) 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 scenarion for Precipitation (rainfall), over Scotland summers will become up to 20% drier, and winters 20% wetter. Overall, the central estimate is for the annual average rainfall to be about 10% less in the 2080s. There are some regional differences.
UKCP09 projections - Change (m) in significant wave height by 2085, compared to 1975, medium emissions scenario – winter

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 Level / Storm surges, Tides and Wave Height 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 significant wave height for winter 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, significant wave heights north of Scotland will decrease by about 30 cm in the winter.  The other seasons have different patterns of change, although changes are quite small.
UKCP09 Projections - Change in number of days of stratification (in days) by 2085, compared to 1975, medium emissions scenario. Negative days mean date moves earlier.

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 Total Number of Stratified Days 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.
UKCP09 projections - Extreme water level (cm) - 2095 projection - 50-year return extreme water level above the highest astronomical tide (due to storm surge + worst case relative sea level rise

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 Level / Storm surges, Tides and Wave Height 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 2095 projection of exceedance of the Highest Astronomical Tides by 50-year return period storm surge combined with a worst case estimate of relative sea level rise.

Summarising the anticipated changes around Scotland based on central estimate projections for 2080-90 using the medium emission scenario, Storm surges / tides current estimates do not suggest storminess will increase significantly over Scotland making the predictions of increases in storm surge heights over the next 100 years small. For example extreme storm surges with return periods of 2, 10, 20 and 50 years are between about 1 and 3 cm by 2095. There is some regional variation.  Currently, the highest storm surge that may occur in a 50-year period raises the sea surface by between 90 and 180 cm. The effect is least on the east coast and in Shetland, and greatest on the west coast. The central estimate predicts that by 2095, these extreme water levels will have changed very little.
UKCP09 Projections - Increase (°C) in summer air temperature, 2080s compared to 1970s, 50% probability level

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 Precipitation and Air temperature 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 projected change in summer air temperature (50% probability level) 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 scenarion for Air temperature,  winter air temperatures are expected to increase by between 1.1 and 2.4ºC by the 2080s. Increases are projected to be greater on the east coast than on the west coast. Very similar values are projected for summer.  There are some regional differences in the projections.2080s. There are some regional differences.
UKCP09 Projections - Increase in extreme storm surge water level (cm) by 2100, compared to 2000, for the 50-year return surge, medium emissions scenario

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 Level / Storm surges, Tides and Wave Height 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 trend in extreme storm surge water level for the 50 year return surge.

Summarising the anticipated changes around Scotland based on central estimate projections for 2080-90 using the medium emission scenario, Storm surges / tides current estimates do not suggest storminess will increase significantly over Scotland making the predictions of increases in storm surge heights over the next 100 years small. For example extreme storm surges with return periods of 2, 10, 20 and 50 years are between about 1 and 3 cm by 2095. There is some regional variation.  Currently, the highest storm surge that may occur in a 50-year period raises the sea surface by between 90 and 180 cm. The effect is least on the east coast and in Shetland, and greatest on the west coast. The central estimate predicts that by 2095, these extreme water levels will have changed very little.
UKCP09 projections - Extreme water level (cm) - Present day baseline – 50-year return extreme water level above the highest astronomical tide (due to storm surge)

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 Level / Storm surges, Tides and Wave Height 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 present day baseline of exceedance of the Highest Astronomical Tides by 50-year return period storm surge

Summarising the anticipated changes around Scotland based on central estimate projections for 2080-90 using the medium emission scenario, Storm surges / tides current estimates do not suggest storminess will increase significantly over Scotland making the predictions of increases in storm surge heights over the next 100 years small. For example extreme storm surges with return periods of 2, 10, 20 and 50 years are between about 1 and 3 cm by 2095. There is some regional variation.  Currently, the highest storm surge that may occur in a 50-year period raises the sea surface by between 90 and 180 cm. The effect is least on the east coast and in Shetland, and greatest on the west coast. The central estimate predicts that by 2095, these extreme water levels will have changed very little.

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