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/wiser The views expressed in this publication are the sole responsibility of the author(s) and do not necessarily reflect the views of FCDO or the Met Office, UK. Images: I-stock; Robert Powell, Paul Watkiss. Citation. Watkiss, P. and Cimato, F. (2022). How to Note 1: Commissioning Socioeconomic Benefit
. These changes are calculated from the population data in the 'middle of the road' socio-economic scenario (SSP2), used throughout the poster. References Dankers, R., Arnell, N. W., Clark, D. B., Falloon, P. D., Fekete, B. M., Gosling, S. N., Heinke, J., Kim, H., Masaki, Y., Satoh, Y., Stacke, T., Wada, Y
The UK comprises of England, Wales, Scotland and N Ireland. England and Wales comprises of England N, England S and Wales. England comprises of England N and England S.
41/49 SE 51/62 SE 38/47 S 41/52 SW 48/60 SW 51/65 SW 52/66 SW 900 30/40 SE 35/47 SE 24/32 S 30/40 SW 32/43 SW 37/50 SW 38/52 SW 600 31/38 SE 44/55 SE 33/41 S 35/44 SW 37/48 SW 43/55 SW 44/57 SW 300 16/26 E 29/44 SE 18/25 S 20/31 SW 19/30 SW 23/36 SW 24/38 SW Glen 8/14 E 19/37 SE 13/26 S 17/32 SW 13
May 2024’s average mean temperature of 13.1°C for the UK beat 2008’s previous record figure of 12.1°C in a series which dates back to 1884. The month’s mean temperature has been influenced particularly by above average temperatures in the northern half of the UK, with Scotland’s May mean
Weather Forecast Forecast for Wednesday 17 Sep 2025 Height (m) Wind Speed mean/gusts (mph) Wind Direction (blowing from) 06:00 09:00 12:00 15:00 18:00 21:00 00:00 1000 24/29 SE 36/43 SE 40/48 S 45/56 SW 51/63 SW 51/65 SW 53/67 SW 900 24/29 SE 32/40 SE 36/44 S 43/54 SW 47/60 SW 48/61 SW 50/64 SW 600 18
century. Science Advances,. 4, eaao5297 (2018). References England, M.H., S. McGregor, P. Spence, G. A. Meehl, A. Timmermann, W. Cai, A.S. Gupta, M. J. McPhaden, A. Purich and A. Santoso (2014). Recent intensification of wind-driven circulation in the Pacific and the ongoing warming hiatus, Nature
of the Chernobyl nuclear accident. After that he carried out post-doctoral research at Edinburgh University on stratospheric ozone depletion. Key papers include: Stott, P. A., S. F. B. Tett, G. S. Jones, M. R. Allen, J. F. B. Mitchell, G. J. Jenkins., 2000. External control of twentieth century
the solar wind in-situ The Parker spiral Image credit: I. Mueller-Wodarg There are different types of solar wind • Fast solar wind (v≈750km/s) comes from coronal holes • At solar minimum, polar coronal holes dominate flow – fast wind over the Sun’s poles • Slower (v≈400 km/s), denser (≈2x) and more
- - - Wet Bulb Freezing Level m AMSL Hourly to T+360 - - - Relative Humidity % Hourly to T+360 Three-hourly to T+360 - Local Midday / Midnight to Day 15 Mean Sea Level Pressure Pa Hourly to T+360 Three-hourly to T+360 - Local Midday / Midnight to Day 15 Wind Wind Speed m/s Hourly to T+360 Three-hourly
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