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Sea ice in the climate system

Figure 3: Changes to the seasonal cycle of Arctic sea ice cover shown using decadal averages of daily extent. Data are from Met Office Hadley Centre HadISST dataset The decline in summer sea ice extent of course means the amount of ice that survives through to the following winter to become multi-year

How we measure sea ice

containing sea ice with concentration of at least 15% - over the period 1981-2010. Data from Met Office Hadley Centre HadISST dataset which combined numerous satellite observations from multiple platforms. Arctic sea ice extent   Figure 1:Average summer minimum (grey) and winter maximum (white

uk_monthly_climate_summary_201803.pdf

on the 2nd, with light snow showers in the north-east, and very wet with rain, sleet and snow in the Midlands and East Anglia from mid-a ernoon. It remained very cold with an overnight minimum temperature of -10.0 °C at Alston Springhouse Park (Cumbria), and windy too with gusts of 84 mph reported

factsheet_18-weather-satellites_2023.pdf

-Imagery Cloud Water Vapour Image Precipitation Simulated-Imagery Dust Fire Visible-Imagery Low-Light-Imagery Severe-Convection Aircraft-Icing Fog Volcanic-Ash Snow Figure 6. The variety of satellite imagery products produced at the Met Office to support the forecasters and Met Office hazard centre

PowerPoint Presentation

-December period), NOAA Climate Prediction Centre gives a 50- 60 % chance of a short-lived La Niña event while the likelihood of ENSO remaining neutral is around 40 %. In contrast, output from the Australian Bureau of Meteorology strongly favours (> 90% chance) ENSO-neutral for the remainder of 2025

PowerPoint Presentation

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: October to July Current Status 8 Current Status – Precipitation percentiles

PowerPoint Presentation

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

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

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

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 the NOAA Climate Prediction Center

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