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, GIC, etc. (29ea.) Aviation Power SWx Operations – observation network GIC Monitor (x3) TEC & Scintillation Monitor (x5) Singapyung Sintaebaek Daejeon Gwangju Dongjeju SWx Operations – satellite tracking facilities ‣ACE Tracking Antenna � global tracking network for RTSW � 13-meter dish antenna (S

this signal has a particularly large spatial extent and a magnitude of >1.6 hPa s �1 in the ensemble mean by the 2080s/2090s. In north central Sahel both ensembles show smaller upward anomalies (approximately 0.8 hPa s �1 ) corresponding to the wet signal in Figure 1. These changes are amplified

, Institut Pierre Simon Laplace (IPSL) S. Flavoni: Sorbonne Universités, LOCEAN Laboratory, Institut Pierre Simon Laplace (IPSL) L. Hermanson: Met Office Hadley Centre N. Keenlyside: University of Bergen and Bjerknes Centre for Climate Research, Nansen Environmental and Remote Sensing Center

Climatic Change (2013) 120:965–975 DOI 10.1007/s10584-013-0831-3 LETTER Climate change projections of the North American Regional Climate Change Assessment Program (NARCCAP) L. O. Mearns & S. Sain & L. R. Leung & M. S. Bukovsky & S. McGinnis & S. Biner & D. Caya & R. W. Arritt & W. Gutowski & E

Specific humidity (huss) 4 4 4 4 Temperature, maximum (tasmax) °C 4 4 4 4 Temperature, mean (tas) °C 4 4 4 4 hourly 4+ Temperature, minimum (tasmin) °C 4 4 4 4 Wind gust m/s 4 3-hourly Wind speed (sfcWind) m/s 4 4 4 3-hourly 4 Wind speed eastwards (uas) m/s 4 4 4 4 Wind speed northwards (vas) m/s 4 4

third of a degree at the equator, giving 360 x 216 grid points in total, and 40 unevenly spaced levels in the vertical (a resolution of 10m near the surface). References: Collins, W.J., N. Bellouin, M. Doutriaux-Boucher, N. Gedney, T. Hinton, C. D. Jones, S. Liddicoat, G. Martin, F. O'Connor, J. Rae

Response to CO2 Forcing, Journal of Climate, DOI: 10.1175/JCLI-D-17-0323.1. Gohar G, Bernie D, Good P and Lowe JA, 2018. UKCP18 Derived Projections of Future Climate over the UK, Met Office. Lowe JA, Howard TP, Pardaens A, Tinker J, Holt J, Wakelin S, Milne G, Leake J, Wolf J, Horsburgh K, Reeder T

American Multimodel Ensemble models? J. Climate, 30, 8335–8355, https://doi.org/10.1175/JCLI-D-17-0054.1. Bellprat, O., Kotlarski, S., Lüthi, D., De Elía, R., Frigon, A., Laprise, R., & Schär, C. (2016). Objective calibration of regional climate models: application over Europe and North America. Journal

forecast, EXP (with IAU) had a Ps tendency of 0.13[Pa/s] at the 1 st timestep, a 46% decrease compared to CTR (without IAU) of 0.24[Pa/s] Ensemble Mean Fields : week 3 Precipitation • (Left) Operational precipitation is overestimated compared to GPCP over the equatorial area • (Middle) WCDA

and 40°S. Here, a low-level westerly flow prevails throughout the year, leading to high precipitation at the western slopes and dry conditions east of the Andes (Garreaud et al., 2008). Wind fields Driven by the high pressure cell in the SW-Atlantic, the easterly trade winds penetrate