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4) � • Projections (2050s): Fig 5 to Fig 6 T: S�N, δT↑ for winter (~3.25̊ ) ; δT↓ for summer (~2.87 ̊ ) P: Winter, W�E δP↑ Up_GL(0.4mm)<Lw_GL (1.0mm); Summer: Lw_GL P↑ (~0.7mm), Up_GL P↑ (Q3-0.2mm), P↓ (Q0-0.3mm) Discussion, Conclusions and Future Directions � PRECIS performed well on the high

Information Bathymetry of the AMM15 model domain. The red line defines the low-resolution AMM7 model domain. The yellow dotted box is the domain covered by the AMM15 products delivered on a regular grid to UKMCAS users. (Figure from Tonani et al. 2019) Filetype Variables(s) Description Averaging

1989 with 1665.3 & NE 9.60, also 9.60 in 1990. mm. hours. England NW & Wales N Midlands East Anglia England SW & Wales S England SE & Central S 4th warmest in series with 9.50, warmest 1990 with 9.55. 4th warmest in series with 10.14, warmest 1990 with 10.22. 4th warmest in series with 10.79, warmest

findings Met Office ( https://metoffice.gov.uk/binaries/content/assets/metofficegovuk/pdf/business/international/rep ort-on-regional-sea-level-projections-for-south-asia---arrcc-report---external-1.pdf) Hinkel, J., Jaeger, C., Nicholls, R. J., Lowe, J., Renn, O., & Peijun, S. (2015). Sea-level rise

Clim Dyn (2015) 44:1901–1918 DOI 10.1007/s00382-014-2272-8 Assessing the effect of domain size over the Caribbean region using the PRECIS regional climate model Abel Centella‐Artola · Michael A. Taylor · Arnoldo Bezanilla‐Morlot · Daniel Martinez‐Castro · Jayaka D. Campbell · Tannecia S. Stephenson

to penetration onto the high polar plateau where the South Pole sits. In the British Antarctic Expedition of 1907—1909, better known as the Nimrod expedition, Shackleton and his team pioneered the Beardmore Glacier route to the South Pole and came to within 112 miles of the South Pole by reaching 88°23’S

summary report. Report SC060064/TR6. Bristol: Environment Agency Fox-Kemper, B., H.T. Hewitt, C. Xiao, G. Aðalgeirsdóttir, S.S. Drijfhout, T.L. Edwards, N.R. Golledge, M. Hemer, R.E. Kopp, G. Krinner, A. Mix, D. Notz, S. Nowicki, I.S. Nurhati, L. Ruiz, J.-B. Sallée, A.B.A. Slangen, and Y. Yu, 2021: Ocean

Basin, Kenya Please cite this paper as: Rwigi, S. K., N. J. Muthama, A. O. Opere and F. J. Opijah, 2016. Assessment of Potential Changes in Hydrologically Relevant Rainfall Statistics over the Sondu River Basin in Kenya Under a Changing Climate. J. Meteorol. Relat. Sci. vol 9 pg 2-12. http://dx.doi.org

Volcanic Ash – T+0 annotated satellite image Issued 0930 UTC on Wed 11 Dec 2013 VOLCICE1303 Exercise Katla eruption Low Confidence gh Confidence Airep report of Ash cloud considered to be unlikely given upper wind trajectories and available imagery. lcanic Ash can be seen in imagery tending northeast from Katla. This s been confirmed by ground based servation at Keflavik. © Crown copyright Met Office

(magenta circles), NMHS AWSs reporting to the GTS (white and green squares). MODE-S receivers were installed at airports in the cities of Entebbe, Kisumu, Nairobi, Dar es Salaam and Mwanza. Given the likely availability of these additional datasets, the HIGHWAY Project Steering Committee and the funding