London scoping - ukcip
London scoping - ukcip
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.