1000 resultados para 145-884C
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The cold upwelling 'tongue' of the eastern equatorial Pacific is a central energetic feature of the ocean, dominating both the mean state and temporal variability of climate in the tropics and beyond. Recent evidence for the development of the modern cold tongue during the Pliocene-Pleistocene transition has been explained as the result of extratropical cooling that drove a shoaling of the thermocline. We have found that the sub-Antarctic and sub-Arctic regions underwent substantial cooling nearly synchronous to the cold tongue development, thereby providing support for this hypothesis. In addition, we show that sub-Antarctic climate changed in its response to Earth's orbital variations, from a subtropical to a subpolar pattern, as expected if cooling shrank the warm-water sphere of the ocean and thus contracted the subtropical gyres.
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Mode of access: Internet.
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Reglamento general de reforma para el régimen escolático y económico de las reales escuelas de medicina, cirugía, farmacia, o Arte de curar y para el gobierno de esta facultad en todo el reyno, 194 p.
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"The Interim commission [on food and agriculture]": p. 12-13.
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"5 March 1985."
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"January 1980."
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"August 1984."
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"13 August 1984."
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"June 1952."
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Includes index.
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Includes index.
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Includes index.
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"17 September 1984."
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"17 September 1984."