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The intrusion of Mozambique Channel warm waters could result in an asynchronicity in seasonality between upwelling surface signature and upwelling favourables winds. A joint U. The broad spectral coverage and high spectral resolution of ASTER will provide scientists in numerous disciplines with critical information for surface mapping, and monitoring of dynamic conditions and temporal change. Example applications are: monitoring glacial advances and retreats; monitoring potentially active volcanoes; identifying crop stress; determining cloud morphology and physical properties; wetlands evaluation; thermal pollution monitoring; coral reef degradation; surface temperature mapping of soils.

Gully erosion in Madagascar : causes and impacts. Soil erosion has been recognized as the main cause of land degradation worldwide and gully erosion is currently considered as one of the most impressive and striking erosion type.

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This global environmental problem has numerous causes both natural and anthropogenic and inflict serious socio-economic problems all around the world. The present study aims to discuss the occurrence and environmental issues related to lavakization in Madagascar and its impact on landscape badland formation , land use management, flora and fauna, infrastructures, soil properties and human life itself. We assembled and reviewed lavaka researches since Exact location of the field surveys, cited triggering factors and results of these scientific papers have been studied in detail and compared with our data collected using satellite imagery.

Lavaka distribution was analyzed using GIS methods and the relation between their density and different factors was studied. An overview of the many contributing factors climate, topography, geology, vegetation cover, fault systems, tectonism and land use including inappropriate cultivation and irrigation systems is given in order to better understand lavaka formation, distribution and impacts. Synthesis of previous researches might help us define area susceptible to gully formation.

This can be used to determine prevention priorities for farmers, to manage their lands sustainably. Malagasy dialects and the peopling of Madagascar. The origin of Malagasy DNA is half African and half Indonesian, nevertheless the Malagasy language, spoken by the entire population, belongs to the Austronesian family. The language most closely related to Malagasy is Maanyan Greater Barito East group of the Austronesian family , but related languages are also in Sulawesi, Malaysia and Sumatra.

For this reason, and because Maanyan is spoken by a population which lives along the Barito river in Kalimantan and which does not possess the necessary skill for long maritime navigation, the ethnic composition of the Indonesian colonizers is still unclear. There is a general consensus that Indonesian sailors reached Madagascar by a maritime trek, but the time, the path and the landing area of the first colonization are all disputed. In this research, we try to answer these problems together with other ones, such as the historical configuration of Malagasy dialects, by types of analysis related to lexicostatistics and glottochronology that draw upon the automated method recently proposed by the authors.

Understanding the persistence of plague foci in Madagascar. Plague, a zoonosis caused by Yersinia pestis, is still found in Africa, Asia, and the Americas. Madagascar reports almost one third of the cases worldwide. Flea vector and wild rodent host population dynamics are tightly correlated with modulation of climatic conditions, an association that could be crucial for both the maintenance of foci and human plague epidemics. The black rat Rattus rattus, the main host of Y. Also, endemic fleas could play an essential role in maintenance of the foci.

This review discusses recent advances in the understanding of the role of these factors as well as human behavior in the persistence of plague in Madagascar. Understanding the Persistence of Plague Foci in Madagascar. Neither geologists nor biologists have a definition that is capable of classifying Madagascar unambiguously as an island or a continent; nor can they incorporate Malagasy natural history into a single model rooted in Africa or Asia.

Madagascar is a microcosm of the larger continents, with a rock record that spans more than million years Ma , during which it has been united episodically with, and divorced from, Asian and African connections. This is reflected in its Precambrian history of deep crustal tectonics and a Phanerozoic history of biodiversity that fluctuated between cosmopolitanism and parochialism. Both vicariance and dispersal events over the past 90 Ma have blended a unique endemism on Madagascar , now in decline following rapid extinctions that started about years ago.

One authority has reported that less than 1 percent of Spencer, William. Historical Dictionary of Morocco. African Historical Dictionaries Middle East and Africa, 5, No. Hodges, Tony. Historical Dictionary of Western Sahara. Uilenberg, H. Hoogstraal, J. A chronology for late prehistoric Madagascar. A database has been assembled with age determinations for Madagascar.