7.7.1 The UK is committed to an 80% reduction in greenhouse gas emissions by 2050, and a recommended cut of up to 42% by 2020. Recent research shows that although we need to reduce emissions to stay below an increase of 2oC, it is now acknowledged that there is a significant risk that global temperatures could rise by 4oC (DECC).
‘Warming to the idea: building resilience to extreme weather and climate change in the South West’ updates the summary report of a scoping study carried out in 2003, which summarised the impacts of climate change across a number of sectors in the South West. The updated publication incorporates the latest climate projections (UK Climate Projections 2009) and reflects current understanding of the key issues and adaptation opportunities for the South West (Climate South West, 2010).
7.7.2 Global average temperatures have risen by nearly 0.8oC since the late 19th century, rising at about 0.2oC/decade over the past 25 years (United Kingdom Climate Impacts Partnership).
7.7.3 Annual average daily mean temperature in the South West has increased by 1.37°C between 1961 and 2006, similar to annual trends in London, South East and East of England (Figure 1.4). However, this increase has been larger in winter (1.72°C) than in summer (1.41°C). A similar pattern exists for changes in average daily minimum and maximum temperature.
7.7.4 Over the last 250 years, there has been a slight trend for increased rainfall in winter and decreased rainfall in summer, a trend which is in line with the expected changes. All regions of the UK have experienced an increase over the past 45 years in the amount of winter rain that falls in heavy downpours.
7.7.5 Between 1961 and 2006 there has been increased seasonal and annual total precipitation in the South West, with the largest increase seen in autumn (28.6%). The only exception to this pattern is a small decrease in total precipitation during summer (8.8%). During the same time period the South West has also experienced a small increase in the number of days of rain in autumn and winter and a small decrease in the number of days of rain in spring and summer.
7.7.6 Climate change is expected to increase the risk of river and urban flooding in our region. Our long, varied coastline will be affected by rising sea levels, with an expected increase in risk of flooding for our low lying coastal communities. More information about 7.6 'Flooding' is available in this report.
7.7.7 Global sea-level rise has accelerated between the mid 19th and mid 20th century and is now at about 3mm per year. It is likely that human activities have contributed to between a quarter and a half of this rise in the last half of the 20th century. Absolute sea level (i.e. corrected for land movement) around the South West has risen by around 1 mm/yr over the 20th century (Proudman Oceanographic Laboratory), and there are indications that the increase has been at a faster rate than this in the 1990s and 2000s. The nature of land movement in the South West (where land levels are generally getting lower through time) is likely to enhance the effect of rising sea levels.
Table 7.7.1 Sea level change at Newlyn (Cornwall) since 1946
| Average annual change in mean sea level |
1.0 mm / yr |
| Average annual change in extreme high water level |
2.1 mm / yr |
| Average annual change in extreme low water level |
1.3 mm / yr |
| Source: Proudman Oceanographic Laboratory |
7.7.8 There is some evidence that annual average extremes in high water are increasing faster than annual average extremes in low water. Sea surface temperature around the UK coast has also risen by 0.7°C in the last 30 years.
7.7.9 The Government indicates that we are currently on the medium emissions path in terms of greenhouse gas emissions. Based on the data from UKCP09, the data below provides an overview of the key findings for the South West for the 2020s under the medium emissions scenarios. The 'central estimate' (i.e. The value at the 50% probability level) is reported first, followed by the wider range of uncertainty in brackets. The wider range uses the minimum value at the 10% probability level and the maximum at the 90% probability level, across all three emission scenarios, High (SRES A1FI), Medium (SRES A1B) and Low (SRES B1).
7.7.10 In the South West under medium emissions:
Table 7.7.2 Future seasonal climate (2020)
| Season |
2020s |
|
Spring |
|
|
Warmer by 1.2 deg C (0.62 - 1.9) |
|
|
Marginally wetter by 0.1% (-7.3 to + 8.7%)
|
|
|
Decrease of -2.7% (6.7 to +2.2%)
|
|
|
Decrease of -1.2% (-3.8% to +0.9%)
|
|
Summer |
|
|
Warmer by 1.6 deg C (05 to 2.7)
|
|
|
Drier by 8% (-26.6. to + 17.5%)
|
|
|
Decrease of -5.7% (-14.2 to +4.5%) |
|
|
Decrease of -3.1% (-8.2 to +2.6%)
|
|
Autumn |
|
|
Warmer by 1.5 deg C (0.77 to 2.5)
|
|
|
Wetter by 1.5% (-12.1 to + 16%)
|
|
|
Decrease of -2.0% (-6.3 to 1.8%)
|
|
|
Negligible decrease of -0.5% (-2.3 to +1%)
|
|
Winter |
|
|
Warmer by 1.3 deg C (0.46 to 2.0)
|
|
|
Wetter by 7% (-3.1 to +19.6%)
|
|
|
No change (-2.2 to +19.6%)
|
|
|
Negligible decrease of -0.1% (-0.6 to +0.5%)
|
Annual
|
|
|
Warmer by 1.4 deg C (0.74 to 2.1)
|
|
|
No change (-4.8% to 6.0%)
|
|
|
Decrease of -2.7% (-6.0 to +0.9%)
|
|
|
Decrease of -1.2% (-2.9 to +0.4%)
|
7.7.11 More information is available from Climate South West