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hctn_sept2023rapidhadgemstudy_v1.0.pdf

, D, McCarthy, MP, Kendon, M, Legg, T, Simpson, I. HadUK-Grid—A new UK dataset of gridded climate observations. Geosci Data J. 2019; 6: 151– 159. https://doi.org/10.1002/gdj3.78 Kendon, M., McCarthy, M., Jevrejeva, S., Matthews, A., Williams, J., Sparks, T., & West, F. (2023). State of the UK Climate

hctn_sept2023rapidhadgemstudy_v1.1.pdf

://doi.org/10.1007/s00382-022- 06403-0 Hollis, D, McCarthy, MP, Kendon, M, Legg, T, Simpson, I. HadUK-Grid—A new UK dataset of gridded climate observations. Geosci Data J. 2019; 6: 151– 159. https://doi.org/10.1002/gdj3.78 Kendon, M., McCarthy, M., Jevrejeva, S., Matthews, A., Williams, J., Sparks, T

News

Mild autumn keeps 2022 on track to be warmest UK year

The news comes as provisional figures from the Met Office show Autumn 2022 (September, October, November) was the third warmest on record for the UK, with an average mean temperature of 11.1C, topped only by 2011 and 2006’s Autumn figures, in a series which goes back to 1884.   In addition

observed_changes_in_extremes_final_v1.0.pdf

saw extremely high levels of tropical cyclone activity in the Western North Pacific. This was found to be mainly caused by sea surface warming in the eastern and central Pacific, with human influence largely increasing the odds of this event. Zhang et al 2016 Funk, C., Shukla, S., Hoell, A. and Livneh

wiser-newsletter-0722.pdf

the WISER brand, please email us. Current WISER Opportunities The Met Office is currently seeking consultancy support for the scoping phase of the WISER programme. WISER MEL Consultant The Met Office is seeking to appoint a Consultant(s) with necessary international development and MEL experience

Weather Radar Data Quality Monitoring using Operational Observations

– Fit Functions • Fit function for correlation coefficient ρ HV takes the form: with x = 1 - ρ HV . • Fit function of differential phase Φ DP takes the form: f x = a ⋅ s ⋅ x μ ⋅ e −λ with x = Φ DP - max Φ DP + 10° , where max Φ DP denotes distribution’s maximum, a is an amplitude factor, s a stretch

Multigrid solver makes global forecasts quicker

for the global latitude-longitude grid used in Numerical Weather Prediction [Buckeridge & Scheichl, 2010]. The key idea is to use conditional coarsening in the N-S direction while increasing the mesh spacing uniformly in the E-W direction.  The Figure below shows an example of a semi-coarsened mesh. Using

srocc_sea_level_rise.pdf

in the projected loss of ice from the Antarctic ice sheet (Figure 2a). These revised projections show good agreement with independent work carried out at the Met Office for UKCP18 5 . 1 Daangendorf, S. et al (2019), Nature Climate Change: Persistent acceleration in global sea-level rise since

News

Mixed picture for the week ahead

of year, particularly for southern areas of the country, where some places may reach the mid 20's. You can check the latest forecast on our website, by following us on Twitter and Facebook, as well as on our mobile app which is available for iPhone from the App store and for Android from the Google Play store.   

Slide 1

1.1yrs • Science data on transit thru’ LGA & MGA? © Crown copyright Met Office Ground Segment • Need 4 ground stations (15m dedicated dish) • 2/3 data centres for resilience • UK, US, S Korea ?? © Crown copyright Met Office Priority needs for L5 instruments / parameters • EUV imager • Magnetometer

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