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London scoping - ukcip

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Sea level<br />

Source: IPCC (2001a)<br />

Final Report<br />

43<br />

Tide gauge data show that global average sea level rose between 0.1 and 0.2 metres<br />

during the 20 th century.<br />

Global sea level is projected to rise by 0.09 to 0.88 metres between 1990 and 2100,<br />

for the full range of SRES scenarios.<br />

Table 4.3 Estimates of confidence for selected observed and projected changes in extreme<br />

weather and climate events<br />

Changes in phenomenon Confidence* in observed<br />

changes (latter half of 20th<br />

century)<br />

Higher maximum temperatures<br />

and more hot days over nearly all<br />

land areas<br />

Higher minimum temperatures,<br />

fewer cold days and frost days<br />

over nearly all land areas<br />

Reduced diurnal temperature<br />

range over most land areas<br />

Increase of heat index over land<br />

areas<br />

Likely Very likely<br />

Very likely Very likely<br />

Very likely Very likely<br />

Confidence* in projected<br />

changes (during the 21st<br />

century)<br />

Likely, over many areas Very likely, over most areas<br />

More intense precipitation events Likely, over many NH land areas Very likely, over many areas<br />

Increased summer continental<br />

drying and associated risk of<br />

drought<br />

Likely, in a few areas Likely, over most mid-latitude<br />

continental interiors<br />

* IPCC qualitative classification of confidence levels: Likely (66 to 90%), Very likely (90 to 99%)<br />

Source: IPCC (2001a)<br />

4.3 Climate Change Scenarios for the UK and <strong>London</strong><br />

Since the publication of the UKCIP98 scenarios (Hulme and Jenkins, 1998), significant<br />

advances in computing power have enabled a greater number of climate model experiments to<br />

be conducted at higher spatial resolutions. The Hadley Centre global climate model (HadCM3)<br />

was used to drive a high resolution atmospheric model (HadAM3H) and, in turn, a regional<br />

climate model (HadRM3) for Europe. These experiments resulted in the development of the<br />

UKCIP02 scenarios (Hulme et al., 2002) which describe how the climate of the UK land area<br />

may change in the 21 st Century at a resolution of ~50 km (as opposed to the ~300 km resolution<br />

of UKCIP98). The new scenarios also provide more information about changes in extremes of<br />

weather and sea level, and are explicitly linked to the four SRES storylines described in<br />

Table 2.1 (B1~Low Emissions, B2~Medium-Low Emissions, A2~Medium-High Emissions,<br />

A1F1~High Emissions). In contrast, the UKCIP98 scenarios were based on much simpler<br />

descriptions of future population and fossil fuel use.

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