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Climate change impacts and vulnerability in Europe 2016

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Introduction<br />

collaboration between <strong>in</strong>tegrated assessment<br />

modellers, climate modellers, terrestrial ecosystem<br />

modellers <strong>and</strong> emissions <strong>in</strong>ventory experts — are<br />

called representative concentration pathways (RCPs).<br />

The RCPs provide a consistent set of trajectories for<br />

future atmospheric composition <strong>and</strong> l<strong>and</strong>-use <strong>change</strong><br />

up to the year 2100.<br />

The four RCPs are named from RCP2.6 to RCP8.5<br />

accord<strong>in</strong>g to their approximate radiative forc<strong>in</strong>g level<br />

<strong>in</strong> the year 2100. Extended concentration pathways<br />

(ECPs) extend the RCPs up to 2300 based on simple<br />

extension rules. All ECPs, <strong>in</strong>clud<strong>in</strong>g the highest, ECP8.5,<br />

assume that very low (or even negative) emission levels<br />

are reached by 2250 at the latest (Moss et al., 2010;<br />

van Vuuren et al., 2011). M<strong>in</strong>or differences <strong>in</strong> radiative<br />

forc<strong>in</strong>g between the 'name' of an RCP <strong>and</strong> the values<br />

shown <strong>in</strong> Figure 1.1 (left) are due to different def<strong>in</strong>itions<br />

of forc<strong>in</strong>g (e.g. <strong>in</strong>stantaneous, stratospherically<br />

adjusted, fixed sea surface, or effective radiative<br />

forc<strong>in</strong>g) (Sherwood et al., 2015), how models implement<br />

the various radiatively active species (e.g. prescribed<br />

aerosol optical depth vs. prescribed aerosol<br />

precursor emissions), <strong>and</strong> uncerta<strong>in</strong>ties <strong>in</strong> convert<strong>in</strong>g<br />

concentrations to radiative forc<strong>in</strong>g (Coll<strong>in</strong>s et al., 2013,<br />

Section 12.3).<br />

There are two key 'technical' differences between the<br />

SRES scenarios <strong>and</strong> the RCP scenarios. One relates<br />

to the unit applied for specify<strong>in</strong>g greenhouse gas<br />

'emissions' <strong>and</strong> the other to the l<strong>in</strong>k between <strong>and</strong><br />

socio-economic development. In the case of SRES,<br />

each scenario provides a trajectory of anthropogenic<br />

greenhouse gas emissions coupled with an underly<strong>in</strong>g<br />

storyl<strong>in</strong>e of socio-economic development. In contrast,<br />

the RCPs are scenarios of radiative forc<strong>in</strong>g, which<br />

is determ<strong>in</strong>ed not only by direct anthropogenic<br />

greenhouse gas emissions but also by the future<br />

development of the global carbon cycle <strong>and</strong> other<br />

processes. Moreover, the process of RCP development<br />

has been separated from the socio-economic storyl<strong>in</strong>e<br />

development, which means that the different RCPs are<br />

not directly associated with a particular socio‐economic<br />

scenario (see Section 1.2.2 for details on the<br />

development of socio-economic scenarios alongside<br />

the RCPs).<br />

The key 'political' difference between the RCP <strong>and</strong><br />

SRES scenarios is that the RCPs cover the full range<br />

of stabilisation, mitigation <strong>and</strong> basel<strong>in</strong>e emissions<br />

scenarios available <strong>in</strong> the scientific literature, whereas<br />

all SRES scenarios are no-climate-policy scenarios.<br />

Therefore, the range of temperature projections<br />

between the highest <strong>and</strong> lowest RCP is larger than that<br />

between the highest <strong>and</strong> lowest SRES scenario (see<br />

Figure 1.1, right). Note that the highest RCP (RCP8.5) is<br />

less extreme than the highest SRES emissions scenario<br />

(A1FI), whereas the lowest RCP (RCP2.6), which requires<br />

ambitious mitigation policies, lies far below the range of<br />

the SRES scenarios (see Figure 1.1, left). As a result, the<br />

range of projected <strong>in</strong>creases <strong>in</strong> global temperature for<br />

RCPs is smaller than the range of projections for SRES<br />

scenarios. Ow<strong>in</strong>g to the differences between RCP <strong>and</strong><br />

SRES scenarios, the projections for global temperature<br />

<strong>in</strong>crease dur<strong>in</strong>g the 21st century <strong>in</strong> the IPCC AR5 (0.3 to<br />

4.8 °C, based on the RCPs) (IPCC, 2013) <strong>and</strong> <strong>in</strong> the<br />

IPCC AR4 (1.1 to 6.4 °C, based on the SRES scenarios)<br />

(IPCC, 2007b) are not directly comparable. Further<br />

<strong>in</strong>formation on global temperature <strong>change</strong> projected<br />

for different RCPs is available <strong>in</strong> Section 3.2.2.<br />

Figure 1.1<br />

Relationship between SRES scenarios <strong>and</strong> RCPs<br />

Rediative forc<strong>in</strong>g relative to pre-<strong>in</strong>dustrial (W m -2 )<br />

10<br />

8<br />

6<br />

4<br />

2<br />

SRES (TAR)<br />

A1B<br />

A1T<br />

A1FI<br />

A2<br />

B1<br />

B2<br />

RCP (AR5)<br />

RCP8.5<br />

RCP6.0<br />

RCP4.5<br />

RCP2.6<br />

Mean surface temperature <strong>change</strong> (°C)<br />

SRES CMIP3<br />

AR4 AR5<br />

A1B<br />

A1T<br />

A1FI<br />

A2<br />

B1<br />

B2<br />

RCP CMIP5<br />

RCP8.5<br />

RCP6.0<br />

RCP4.5<br />

RCP2.6<br />

0<br />

0<br />

2000 2010 2040 2060 2080 2100 2000s 2010s 2040s 2060s 2080s 2100s<br />

4<br />

3<br />

2<br />

1<br />

Note:<br />

Source:<br />

Projected radiative forc<strong>in</strong>g (left) <strong>and</strong> global mean surface temperature <strong>change</strong> (right) over the 21st century us<strong>in</strong>g the Special Report on<br />

Emissions Scenarios (SRES) <strong>and</strong> representative concentration pathway (RCP) scenarios.<br />

IPCC, 2014a (Figure 1.4). © 2014 Intergovernmental Panel on <strong>Climate</strong> Change. Reproduced with permission.<br />

38 <strong>Climate</strong> <strong>change</strong>, <strong>impacts</strong> <strong>and</strong> <strong>vulnerability</strong> <strong>in</strong> <strong>Europe</strong> <strong>2016</strong> | An <strong>in</strong>dicator-based report

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