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(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 Outlook Africa: April to January Current

PowerPoint Presentation

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, with respect to the 1981-2010 climatology

PowerPoint Presentation

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 blue indicate values

PowerPoint Presentation

, 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 blue indicate values below the 20th (Cool) and 10th (Cold

africa-climate-outlook---june-2025.pdf

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, with respect

africa-climate-outlook---march-2024.pdf

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, with respect to the 1981-2010

Parallel Suite 43 release notes

temperature profiles. In the tropics and sub-tropics, convection has more realistic structure and spurious light rain/drizzle is reduced. Improvements in the representation of warm rain microphysics results in a reduction in the amount of spurious light drizzle that is especially notable

mo-state-of-uk-climate-2015-v3.pdf

State of the UK Climate 2015 Mike Kendon 1 , Dr Mark McCarthy 1 , Dr Svetlana Jevrejeva 2 , Tim Legg 1 1 Met Office National Climate Information Centre 2 National Oceanography Centre Cover: Satellite image of storm Desmond on 5 December 2015. The low pressure centre is off south-east Iceland at 940

Central England Floods 20 July 2007

stayed mainly dry with some sunshine. In comparison, Scotland, Northern Ireland and northern England had a much quieter day with a good deal of sunshine, although the rain across southern areas pushed into northern England during the late afternoon and early evening. Winds were generally light, although

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Can you bank on the bank holiday weather?

earlier in the week, temperatures are now rising across much of the UK as warmer air is drawn northeast from the North Atlantic. This has brought a lot of moisture too which will help trigger showers as well as allow some low cloud to affect some coasts. With light winds, showers that do develop

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