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it was printed. Revision History Date of this revision: 27 th May 2016 Date of Next revision: 1 st June 2017 Revision date 27 May 2016 First issue Summary of Changes Distribution This document has been distributed to Name Title Date of Issue Version Page 2 Product Description Pollen Forecast produced using
: Indian monsoon Interactions between moist convection and large-scale circulation Development of model assessment software Before joining the Met Office, Alistair completed an MSc in Applied Mathematics at St Andrews University, followed by a PhD in fluid dynamics at the Department of Mathematics in the University of Bristol.
on the day it was printed. Revision History Date of this revision: 27 th May 2016 Date of Next revision: 1 st June 2017 Revision date 27 May 2016 First issue Summary of Changes Distribution This document has been distributed to Name Title Date of Issue Version Page 2 Product Description National Severe
="degC">-3.7</Extreme> <Extreme locId="99163" locationName="Porthmadog" type="HRAIN" uom="mm">1.0</Extreme> <Extreme locId="03716" locationName="St Athan" type="HSUN" uom="hours">7.5</Extreme> </Extremes> </Region> <Region id="se" name="London & South East England"> <Extremes> <Extreme locId="03874
influencing methane profiles in the free troposphere many days and 100’s of km away from the intrusion (b) orographic and other processes associated with complex flow not captured in the transport model (c) errors or biases in the background field and (d) transient emissions not captured in the estimated
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
and Gloucestershire. On 26 November properties were flooded in North Wales, including St Asaph (Denbighshire), with roads and rail services affected in Conwy and Denbighshire. Parts of Newcastle-upon-Tyne and a hospital in Northallerton were affected by flooding. Roads were closed and rail services
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
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
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
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