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into the long edge of the cork at right angles to each other. Step 4: Cut out four small squares of card and label with the four main points of the compass; N, E, S, W. Attach these to the end of each matchstick with Blu-tack. Step 6: Fill the bottle with sand (or pebbles or something else to weigh

Figure 17. Map showing the 30-year (1971–2000) average number of days per year with rainfall amounts greater than or equal to 1 mm. 250 Nettlecombe (altitude 96 m) Plymouth (altitude 50 m) 200 Days 150 100 50 0 J F M A M J J A S O N D J F M A M J J A S O N D 250 Princetown (altitude 453 m) Yeovilton

meteorology and from 1989-2002 using ERA-Interim meteorology, amounting to more than 100000 maps. The model output estimates the 30-day timeintegrated air concentration (dosage) at each grid box (40 km horizontal resolution and 0-100m above ground level) from a release of 1 g/s at Mace Head

, AM mo wind S, li rain many, mo vis, PM mo wind SW, good, NIGHT li wind SE, clear - KMD LV Tue Jul 29:1.AM ,li wind E,good,.PM,mo wind NW, mo rain many, poor,NIGHT, li wind var,2, AM li wind SE, li rain few, mo vis.PM mo wind W, good,NIGHT li wind E,p/cloud - KMD Example of hazard warning message LV

as the average temperature increases cold extremes currently can and do still occur, for example the ’Beast from the East’ in 2018 resulted in the coldest March day on record with a maximum of -4.7 °C recorded at Tredegar in South Wales. However, during the 2010’s these occurrences have been outnumbered

indicates the similarities between the scenarios. Table 2 SRES scenarios that are most similar to the new RCPs, in terms of median global temperature increase by 2100 References Caesar, J., Palin, E., Liddicoat, S et al. Response of the HadGEM2 Earth System Model to Future Greenhouse Gas Emissions Pathways