Etude de la mortalité des chamelons au Sud du Maroc : enquête rétrospective

Une enquête rétrospective a été réalisée entre janvier et août 1999 dans les provinces d'Oued Eddahab, Laâyoune, Guelmim, Tata, Essaouira, Zagora, Ouarzazate, Errachidia et Figuig. Elle a concerné 252 troupeaux camelins, soit 15 p. 100 des effectifs recensés dans ces régions. La mortalité périnatale du chamelon reste une contrainte majeure au développement de l'élevage camelin avec en moyenne 20,2 p. 100 de la mortalité (16,4 p. 100 en 1996 et 22,9 p. 100 en 1997). L'âge de la mort se situait entre 0 et 6 mois dans plus de 80 p. 100 des cas. Les premières causes de mortalité citées par les éleveurs étaient la diarrhée (72 p. 100), puis, très loin derrière, l'insuffisance alimentaire (9 p. 100), la mortinatalité (6 p. 100) et les abcès (5 p. 100), avec de fortes variations selon les provinces. La typologie des élevages a permis de distinguer quatre classes selon le profil sanitaire et cinq classes selon les pratiques d'élevage. Il existait de fortes corrélations entre la mortalité des chamelons et certaines pathologies des dromadaires adultes, notamment le syndrome respiratoire, la variole, la gale-teigne et d'autres pathologies. La forte homogénéité des modes de conduite n'a pas permis de mettre en évidence des corrélations entre la mortalité et les pratiques d'élevage qui jouaient probablement un rôle important. (Résumé d'auteur

Study on camel calf mortality in South Morocco : Retrospective survey

Between January and August 1999 a retrospective survey was conducted in the provinces of Oued Eddahab, Laayoune, Guelmim, Tata, Essaouira, Zagora, Ouarzazate, Errachidia and Figuig on 252 camel herds, i.e. 15% of the counted populations in these areas. Calf perinatal mortality remains a major constraint to development of camel husbandry with on average 20.2% deaths (16.4% in 1996 and 22.9% in 1997). In more than 80% cases death occurred between 0 and 6 months of age. Main mortality causes reported by breeders were diarrhea (72%), then far behind feed insufficiency (9%), stillbirth (6%) and abscesses (5%), with wide variations among provinces. Herd typology helped identify four classes based on health status and five based on livestock practices. Strong correlations between camel calf mortality and some adult camel diseases, notably the respiratory syndrome, camel pox, mange-moth and other diseases, were observed. Because management modes were very similar, correlations between mortality and breeding practices, which probably played a major role, could not be highlighted

Meteorological and dust aerosol conditions over the western Saharan region observed at Fennec Supersite-2 during the intensive observation period in June 2011

The climate of the Sahara is relatively poorly observed and understood, leading to errors in forecast model simulations. We describe observations from the Fennec Supersite-2 (SS2) at Zouerate, Mauritania during the June 2011 Fennec Intensive Observation Period. These provide an improved basis for understanding and evaluating processes, models, and remote sensing. Conditions during June 2011 show a marked distinction between: (i) a "Maritime phase" during the early part of the month when the western sector of the Sahara experienced cool northwesterly maritime flow throughout the lower troposphere with shallow daytime boundary layers, very little dust uplift/transport or cloud cover. (ii) A subsequent "heat low" phase which coincided with a marked and rapid westward shift in the Saharan heat low towards its mid-summer climatological position and advection of a deep hot, dusty air layer from the central Sahara (the "Saharan residual layer"). This transition affected the entire western-central Sahara. Dust advected over SS2 was primarily from episodic low-level jet (LLJ)-generated emission in the northeasterly flow around surface troughs. Unlike Fennec SS1, SS2 does not often experience cold pools from moist convection and associated dust emissions. The diurnal evolution at SS2 is strongly influenced by the Atlantic inflow (AI), a northwesterly flow of shallow, cool and moist air propagating overnight from coastal West Africa to reach SS2 in the early hours. The AI cools and moistens the western Saharan and weakens the nocturnal LLJ, limiting its dust-raising potential. We quantify the ventilation and moistening of the western flank of the Sahara by (i) the large-scale flow and (ii) the regular nocturnal AI and LLJ mesoscale processes. Key Points First detailed observations from western Sahara sector Intraseasonal shift in Saharan heat low drives meteorological/aerosol conditions Atlantic Inflow interaction with low level jet