Search results (2,833)

in the map indicate a ranking of temperature, with the 0th percentile being the coolest and the 100th percentile being the warmest in the 1981-2010 climatology. Orange and red shading represent values above the 80th (Warm) and 90th (Hot) percentile, respectively; regions shaded in light and dark

the coolest and the 100th percentile being the warmest in the 1981-2010 climatology. Orange and red shading represent values above the 80th (Warm) and 90th (Hot) percentile, respectively; regions shaded in light and dark blue indicate values below the 20th (Cool) and 10th (Cold) percentile

in the 1981-2010 climatology. Orange and red shading represent values above the 80th (Warm) and 90th (Hot) percentile, respectively; regions shaded in light and dark blue indicate values below the 20th (Cool) and 10th (Cold) percentile, with respect to the 1981-2010 climatology. The data used in this map

climatology. Orange and red shading represent values above the 80th (Warm) and 90th (Hot) percentile, respectively; regions shaded in light and dark blue indicate values below the 20th (Cool) and 10th (Cold) percentile, with respect to the 1981-2010 climatology. The data used in this map are from

represent values above the 80th (Warm) and 90th (Hot) percentile, respectively; regions shaded in light and dark blue indicate values below the 20th (Cool) and 10th (Cold) percentile, with respect to the 1981-2010 climatology. The data used in this map are from the NOAA Climate Prediction Center. Climate

weather conditions for that location for the time specified. For example, if our forecasts models predict sunny intervals with just a small chance of a short light shower, then the symbol which is displayed is likely to be the sunny interval symbol. This is because the predominant weather type during

in the London area, along with pollution which the winds from the east had brought from industrial areas on the continent. Early on 5 December, in the London area, the sky was clear, winds were light and the air near the ground was moist. Accordingly, conditions were ideal for the formation of radiation

have had polarizers since the days of C/P on SMM and SOLWIND on P78-1. – This capability has tended to be underused. Mainly because of low cadence. Polarization at Large Elongations. ● ● High degree of polarization of Thomson-scattered light to well past 90°. Current imagers are not noise-limited

, please contact the Customer Centre on: Tel: 0370 900 0100 Fax: 0370 900 5050 Email: [email protected] If you are outside the UK: Tel: +44 330 135 0000 Fax: +44 330 135 0050 From Sorcery to Supercomputers A brief history of key developments in meteorology as illustrated by Treasures from

miles) from the foot of the fell. The Helm Wind can be very gusty as it blows down the steep fell sides but ceases under the helm bar cloud. To the west of this point, a light westerly wind may blow over a short distance. The term ‘Helm Wind’ is applied to similar winds with associated cloud elsewhere, such as in the Lake District or along the Pennines.