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Transcript
Global weather extremes and climate change
The global average temperature at the Earth’s surface has risen by more than 1 °C since the pre-industrial era*. This measure
of warming is useful for mitigation targets but masks bigger changes on regional or shorter-term scales. Extreme weather
events have severe impacts on society and ecosystems in our current climate, and pose an increasing threat as climate
changes. Building future resilience to extremes requires continued development in attribution science and forecasting skill.
Some types of weather extremes
have increased globally
Global observations show an increase in certain types
of extreme weather since 1950.1,2 The number of warm
days and nights have increased, whilst the number of cold
days and nights have declined.1,2 Heatwaves have become
more frequent. Met Office research shows extreme summer
temperature events in Europe are now 10 times more likely
than they were in the early 2000s.3 The number of heavy
rainfall events over land has increased in more regions than
it has decreased.1 ,2
Figure 1. The number of warm nights increased globally between 1951
and 2015. This map shows the rate of increase, per decade, of days where
minimum night-time temperatures were in the warmest 10%. Areas
where data are not available are shown in white. Source: GHCNDEX.4
*Pre-industrial is defined here as the 1850-1900 average.
Understanding long-term changes in many weather-related
extremes including droughts, floods, cyclones and wildfires
can be difficult because of natural variability and limitations
in observational records. Assessing the vulnerability of
human populations and ecosystems to future weatherrelated threats depends on continued monitoring efforts
and improved, higher resolution climate models..
Is climate change responsible?
The science of determining how much of a role human influence has played in an extreme weather or climate event,
known as attribution science, has advanced rapidly in response to increasing risks from climate change. The Met Office
Hadley Centre is working with partners to pioneer the development of an event attribution system to provide regular and
reliable assessments of recent extremes.5,6
Current attribution science shows:
Temperatures: Global records reveal large increases in warm
extremes and decreases in cold extremes worldwide since 1950,
which can be confidently attributed to human influences on climate
as global mean surface temperature has risen unequivocally.2 The
likelihood of the European heatwave of 2003 was at least doubled
by human influence.7
Rainfall: As temperatures rise, the capacity of the atmosphere to hold
moisture increases, and heavier rainfall can be expected. At the same
time, higher rates of evaporation mean drought conditions can be
exacerbated in some regions. Confidence in attributing these types of
event to human influence can be more difficult in some cases as there
is high regional natural variability in rainfall extremes. As understanding
and climate modelling capabilities continue to improve, confidence in
the attribution of these events is rapidly advancing. 2
Storms: Severe storms, hurricanes and typhoons can also be difficult
to attribute as they are strongly influenced by atmospheric circulation
and the impacts of climate change are less well understood.
Further extremes are likely as emissions continue
As global average surface temperature rises, it is virtually certain hot temperature extremes over most land areas will be
more frequent on daily and seasonal timescales.1 Under a medium/high emissions scenario, temperatures endured in
Europe during the heatwave of 2003 could be considered cooler than average by the end of the century.3
Extreme rainfall over mid-latitude land masses and wet tropical regions is expected to become more intense and more
frequent.1 Predicting the frequency and intensity of extreme rainfall events will be invaluable for countries across the world as
they make plans to adapt to more flooding.
Met Office scientists have pioneered the use of very high-resolution (1.5km-scale) regional climate models which can simulate
hourly rainfall extremes far more realistically than coarser models typically used for projections.8-10 Projections of future UK
rainfall already indicate that wetter winters and more intense summer downpours are likely under a medium/high emissions
scenario, both raising the risk of future flooding.
Monthly to decadal forecasting for early warning of extreme weather events
Advance warning of an increased risk of extreme weather events associated with particular climate regimes, such as
El Niño, allows vital time to prepare, thereby reducing potential impacts on life and property. The Met Office has been at
the forefront of work in this area – applying its expertise to regions around the world.
Using the latest Met Office initialised climate predictions, Met Office scientists have demonstrated skilful prediction of
the winter North Atlantic Oscillation (NAO) more than a year ahead.11 The NAO has a profound influence on European
and North American weather patterns, and reliable forecasts on seasonal to interannual timescales are hugely valuable in
planning for winter variability and the heightened risk of hazardous weather.
Continued improvement in monthly, seasonal, and decadal forecasting will help with disaster risk reduction in the UK and
across the world. The Met Office is involved in a number of projects with this goal, funded through the European Union’s
Horizon 2020 programme:
EUPORIAS
(European Provision of Regional
Impacts Assessments on Seasonal
and Decadal Timescales) links
seasonal-decadal climate
predictions with climate impacts
and policy, and addresses key
knowledge gaps and vulnerabilities
in sectors such as water, energy,
transport, food security, and health.
SPECS
(Seasonal to Decadal climate
Prediction for the improvement
of European Climate Services)
aims to deliver a new generation
of European climate forecast
systems for reliable, local climate
information over land at seasonal
to decadal time scales.
EUCLEIA
(European Climate and Weather
Events: Interpretation and
Attribution), seeks to understand
the extent to which weather and
climate extremes in Europe have
changed due to human influences
on climate, and identify types of
events where further research is
needed to robustly attribute risk.
References: 1IPCC AR5, 2013; 2Herring et al., 2015; 3Christidis et al., 2015; 4Donat et al., 2013; 5WIRES Clim Change 2016; 6Stott et al., 2016; 7Stott et al., 2004;
8
Chan et al., 2014; 9,10Kendon et al., 2014; 2016; 11Dunstone et al., 2016
Work featured in this publication has been supported by the Joint UK BEIS/Defra Met Office Hadley Centre Climate Programme (GA01101).
Produced by the Met Office. Met Office and the Met Office logo are registered trademarks. © Crown Copyright 2016, Met Office 16/0844