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s−1) (red: ERA5; black CANARI LE; grey: individual LE members. The dotted lines indicate the axis of the stratospheric polar vortex. i.e. where !U peaks, while the dashed lines are the zero-wind line. The 20 m s −1 contours are thickened to highlight the stratospheric polar vortex
new risks over implementation delivery and benefits realisation would be assessed. A health and safety risk have been added to the register. • Simon Brown (Services Director) presented the annual Health and Safety (H&S) report. He discussed the external report on H&S governance and the plans
+0.7 ns England NW and Wales N -1.2 83 3.6 359 +0.6 121 Midlands -1.3 ns 3.6 206 +0.9 114 East Anglia -1.3 ns 4.0 149 +0.8 ns England SW and Wales S -1.1 ns 4.6 368 +0.8 117 England SE and Central S -1.2 ns 4.3 217 +1.0 ns In each district temperatures are significantly higher when averaged over
conventions. A-Z of storm names for 2020-21 A: Aiden B: Bella C: Christoph D: Darcy E: Evert (Eh-vert) F: Fleur G: Gavin H: Heulwen (Hail-wen) I: Iain J: Julia K: Klaas (Klaa-s) L: Lilah (Ly-la) M: Minne (Minn-eh) N: Naia (N-eye-a) O: Oscar P: Phoebe R: Ravi S: Saidhbhin (Sigh-veen) T: Tobias V
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
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
. height_AGL_at_freezing_level Height of the 0degC isotherm (freezing level) above the surface (ground.) m s-1 None None 15-minutely T+0 to T+54 3-hourly T+57 to T+120 m None None Hourly T+0 to T+54 3-hourly T+57 to T+120 m None None Hourly T+0 to T+54 3-hourly T+57 to T+120 15-minutely T+0 to T+54 3-hourly T
(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
o W, 0-60 o N) minus global SST between 60 o S and 60 o N (Trenberth and Shea 2006). The Pacific Ocean also displays longer timescale variations (Figure 5), variously referred to as the Pacific Decadal Oscillation (PDO; Mantua et al. 1997), Pacific Decadal Variability (PDV; Deser et al. 2012
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
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