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2 The climate models
A set of global and regional climate models have been set up by the Met Office Hadley Centre. An experimental design has been chosen that allows an estimate to be made of uncertainty of future climate projections.
Here we have combined the spread from the Met Office Hadley Centre models with that from alternative climate models produced by other international climate research institutes.
The Met Office Hadley Centre model ensemble is referred to as the Perturbed physics ensemble (PPE), whilst the international model ensemble is termed the Multi-model ensemble (MME). An understanding of the choice and experimental set up of climate modelling is important because these supply driving information for shelf sea and wave models reported in subsequent chapters. A particularly important aspect of the climate model output with regards to marine projections around the UK is changes in storminess and these are discussed here.
Key Findings
- The available climate models provide suitable driving data with which to force models of extreme sea level (Chapter 3 and Chapter 4), waves (Chapter 5) and shelf hydrography (Chapter 6). However, since the driving models for the marine scenarios may not sample the full range of known uncertainties, each uncertainty range quoted should be regarded as a minimum range.
- The ensemble of Met Office Hadley Centre models (PPE) typically shows a slight weakening and southward movement of the storm track over the UK.
- The ensemble containing models from other climate research centres (MME), typically shows a greater increase in storm intensity, but less latitudinal movement in track position. In contrast to the PPE, a MME latitudinal shift can be either northward or southward.
Introduction
The marine scenarios describe projected climate changes in the shelf seas around the UK. However, since the enhanced greenhouse effect (Figure 2.1), which drives these changes, involves the accumulation of radiatively absorbing gases in the atmosphere and takes place at a global scale the maritime models must be connected to climate models.
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| Figure 2.1: Schematic of the greenhouse
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This chapter gives a brief overview of these climate models and
presents results on one key aspect of their behaviour, the projected
changes in the intensity and track of atmospheric storms over Europe.
This feature is highlighted because in the present day climate it is
known to have a major impact on UK shelf waters. The downscaling
approaches used in the marine report are well-validated — as discussed
in detail in the following chapters. However, the validity of the
marine projections is predicated on the validity of the driving global
climate models. The MME members provide a good estimate of possible
climate outcomes to 2100. They provide both mean and variance of
surface climate variables (temperature, precipitation, sea level
pressure) at low spatial resolution (typically a few hundred km) but high temporal resolution over the globe. Some
models take the Earth’s climate system into regimes which cannot be
validated directly because the long-term changes are greater than those
which have occurred during the period of recorded observations. However
some validation against proxy data from different climatic regimes in
Earth’s history has been performed (e.g. Hewitt et al. 2006). Validation of
the driving global climate models is discussed in more depth in UK
Climate Projections science report: Climate change projections.
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Last Updated Friday, 18 June 2010 |