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lies outside these ranges and this likelihood cannot be accurately quantified. In particular, we cannot rule out substantial additional sea level rise associated primarily with dynamic ice discharge from the West Antarctic Ice Sheet (see section 3.2.1). We recommend that decision makers make use

. This roughly coincides with the meridian 9 separating the Arabian Sea and Bay of Bengal regions in this study, which lie respectively to the east and west of the trough axis. Figure A1.4: Spatial patterns representing the effect of mass changes on the fields associated with the Earth’s Gravity (G

apply to the weather parameter ‘Runway state’: a. Dry = D b. Damp = Dp c. Wet = W d. Wet & raining = R e. Frosty = F f. Lying snow = S g. Icy = I h. Unknown = blank j) The weather parameters ‘Upper wind direction & Upper wind speed’ show data at 3000ft. Note: The weather parameters ‘Rain amount

speed, relative and specific humidity, sea level pressure, snowfall amount, lying snow amount, daily mean, maximum and minimum temperature, as well as hourly precipitation, via CEDA and the User Interface. Some variables are being processed onto the 5km OSGB grid, which we anticipate

locate storms within 200 miles of the radar station. In addition, tropical cyclones are tracked by satellites, which provide very useful information both to forecasters and numerical forecast models. "Official" responsibility for forecasting tropical cyclones in the areas affected lies with the regional

simulations that have not been initialised with observations are shown in green. In both cases, the shading represents the probable range, such that the observations are expected to lie within the shading 90% of the time. All temperatures are represented as anomalies from the 1981-2010 mean. The results

30° above the horizon, have an apparent width of more than three fingers at arm's length. When in the form of dark rolls (top photograph) the edges often merge together to form a continuous layer. Sometimes the elements lie in parallel bands (middle photograph). Due to perspective these may appear

with a hardening of the urban environment and inadequate drainage to deal with high quantities of water, will place urban areas at increased risk of flooding. Most of West Africa’s largest cities are coastal and low-lying and are therefore susceptible to inundation by sea water. Due to higher sea levels

, over the Pennines, Cumbrian Hills, and more widely in Scotland, with up to 15cm falling over the Shetlands on the 7th. A cold easterly airstream together with lying snow allowed temperatures to fall to -10°C or below over Sutherland. The UK got a brief respite from the wet and windy weather between

The differences in these curves show how the probabilities for the coming periods differ compared to past years. Where the solid curve (corresponding to this year's Outlook) lies above the dashed curve (normal likelihood), the temperature, precipitation or wind speed at that point has a greater-than