6533b831fe1ef96bd129847e
RESEARCH PRODUCT
Spatial coherence of monsoon onset over Western and Central Sahel (1950-2000)
Romain MarteauVincent MoronNathalie Philipponsubject
Wet seasonAtmospheric Science010504 meteorology & atmospheric sciencesonset[SDE.MCG]Environmental Sciences/Global Changes0207 environmental engineeringDry spell02 engineering and technologyMonsoon01 natural sciencesWest africaSahelpredictabilitymonsoon020701 environmental engineeringObservation dataComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereSpatial coherence[ SDE.MCG ] Environmental Sciences/Global ChangesGeographyBoreal13. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyClimatology[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologyOnset datedescription
Abstract The spatial coherence of boreal monsoon onset over the western and central Sahel (Senegal, Mali, Burkina Faso) is studied through the analysis of daily rainfall data for 103 stations from 1950 to 2000. Onset date is defined using a local agronomic definition, that is, the first wet day (>1 mm) of 1 or 2 consecutive days receiving at least 20 mm without a 7-day dry spell receiving less than 5 mm in the following 20 days. Changing either the length or the amplitude of the initial wet spell, or both, or the length of the following dry spell modifies the long-term mean of local-scale onset date but has only a weak impact either on its interannual variability or its spatial coherence. Onset date exhibits a seasonal progression from southern Burkina Faso (mid-May) to northwestern Senegal and Saharian edges (early August). Interannual variability of the local-scale onset date does not seem to be strongly spatially coherent. The amount of common or covariant signal across the stations is far weaker than the interstation noise at the interannual time scale. In particular, a systematic spatially consistent advance or delay of the onset is hardly observed across the whole western and central Sahel. In consequence, the seasonal predictability of local-scale onset over the western and central Sahel associated, for example, with large-scale sea surface temperatures, is, at best, weak.
year | journal | country | edition | language |
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2009-03-01 |