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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.

 

 

 
   
Figure 2.1: Schematic of the greenhouse effect.  
   
Figure 2.1: Schematic of the greenhouse effect.  
   

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