Polygon

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 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 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 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 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 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.