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• uk_monthly_climate_summary_201907pdf

  for much of England, especially the south-west, and also south Wales, but elsewhere cloud was more variable. The second half was generally more unsettled with frequent westerly and south-westerly winds, but with an exceptionally hot spell from the 22nd to 26th which saw record-breaking temperatures

• global-model-parameters-may-2019.pdf

  energy caused by wind shear) of turbulence which is used to show dynamic stability and the formation of turbulence. 1 [YYYYMMDD]T[hhmm]Z-PT[nnnn]H[mm]M-bulk_ richardson_number.nc 3-hourly (0-144) 6-hourly (150-168) Instantaneous cloud amount below 1000ft ASL Fraction of horizontal grid square occupied

• mogreps-g-parameters-may-2019.pdf

  energy caused by wind shear) of turbulence which is used to show dynamic stability and the formation of turbulence. 1 [YYYYMMDD]T[hhmm]Z-PT[nnnn]H[mm]M-bulk_ richardson_number.nc 3-hourly (0-144) 6-hourly (150- 168) Instantaneous cloud amount below 1000ft ASL Fraction of horizontal grid square

• mogreps-g-parameters-may-2019pdf

  energy caused by wind shear) of turbulence which is used to show dynamic stability and the formation of turbulence. 1 [YYYYMMDD]T[hhmm]Z-PT[nnnn]H[mm]M-bulk_ richardson_number.nc 3-hourly (0-144) 6-hourly (150- 168) Instantaneous cloud amount below 1000ft ASL Fraction of horizontal grid square

• global-model-parameters-may-2019pdf

  energy caused by wind shear) of turbulence which is used to show dynamic stability and the formation of turbulence. 1 [YYYYMMDD]T[hhmm]Z-PT[nnnn]H[mm]M-bulk_ richardson_number.nc 3-hourly (0-144) 6-hourly (150-168) Instantaneous cloud amount below 1000ft ASL Fraction of horizontal grid square occupied

• richard-jones---k-scale-year-long-global-um-simulations-for-dyamond-3-at-convection-permitting-resolutionpdf

  Rebecca Murray-Watson and Emilie Fons Clouds in N2560 RAL3p3 simulations are more reflective than other GSRMs and CERES. Profile plot above shows additional ice in RAL3p3 – cloud fraction is largely similar to other GSRMs and UM CoMA9 and GAL9 First looks from WCRP global km-scale hackathon UM CTC 4.4

• greyzoneproject_eurec4a_protocol_v2.pdf

  prescribed sea surface temperatures. It is recommended to base the simulations on the OSTIA sea surface temperature analysis, or a similar product. 8. Cloud droplet number concentrations Aerosol or CCN concentrations are not specified. We suggest, however, to fix the cloud droplet number

• richard-jones---k-scale-year-long-global-um-simulations-for-dyamond-3-at-convection-permitting-resolution.pdf

  Rebecca Murray-Watson and Emilie Fons Clouds in N2560 RAL3p3 simulations are more reflective than other GSRMs and CERES. Profile plot above shows additional ice in RAL3p3 – cloud fraction is largely similar to other GSRMs and UM CoMA9 and GAL9 First looks from WCRP global km-scale hackathon UM CTC 4.4

• greyzoneproject_eurec4a_protocol_v2pdf

  prescribed sea surface temperatures. It is recommended to base the simulations on the OSTIA sea surface temperature analysis, or a similar product. 8. Cloud droplet number concentrations Aerosol or CCN concentrations are not specified. We suggest, however, to fix the cloud droplet number

• uk_monthly_climate_summary_201806.pdf

  . It became less settled from the 9th onwards, and on 13th/14th there were some large rainfall totals in upland areas of western/southern Scotland and north-west England. The middle part of the month saw generally larger cloud amounts, with spells of rain mainly for Scotland, but from around the 21st onwards