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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

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

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

. 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

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

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

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

) depth of the snow lying on the surface (ground). Typically, water is 10 times as dense as snow so multiplying by 10 gives an approximate depth of the snow, although wet snow can be significantly denser and powder snow much less dense. A scaling factor of 1000 is used to convert m to kg m-2 (GRIB2

) Instantaneous snow depth water equivalent Liquid water equivalent (LWE) depth of the snow lying on the surface (ground). Typically water is 10 times as dense as snow so multiplying by 10 gives an approximate depth of the snow although wet snow can be significantly denser and powder snow much less