998 resultados para Great Moderation


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Zangwill

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Digitalisiert in Kooperation mit dem YIVO Institute for Jewish Research am Center for Jewish History, NY

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Signatur des Originals: S 36/F10889

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Signatur des Originals: S 36/F10890

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by Henry Thatcher Fowler

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Digitalisiert in Kooperation mit dem YIVO Institute for Jewish Research am Center for Jewish History, NY

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Digitalisiert in Kooperation mit dem YIVO Institute for Jewish Research am Center for Jewish History, NY

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[by Stephen John Smith, late 5th (Wellington) Regiment, secretary Samoa administration in military occupation, 1915-1918]

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In light of dramatic changes in American family demography in recent decades, there is a growing recognition that family structure is one of a host of important social factors contributing to children’s health and well-being. The article by Augustine and Kimbro contributes to a growing body of research linking children’s family structure and health outcomes, focusing specifically on the association between family living arrangements and children’s risk of obesity. Their analyses are especially helpful in suggesting that family scholars should pay more attention to potential heterogeneity in relationships between family structure and children’s outcomes.

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Tropical south-western Pacific temperatures are of vital importance to the Great Barrier Reef (GBR), but the role of sea surface temperatures (SSTs) in the growth of the GBR since the Last Glacial Maximum remains largely unknown. Here we present records of Sr/Ca and d18O for Last Glacial Maximum and deglacial corals that show a considerably steeper meridional SST gradient than the present day in the central GBR. We find a 1-2 °C larger temperature decrease between 17° and 20°S about 20,000 to 13,000 years ago. The result is best explained by the northward expansion of cooler subtropical waters due to a weakening of the South Pacific gyre and East Australian Current. Our findings indicate that the GBR experienced substantial meridional temperature change during the last deglaciation, and serve to explain anomalous deglacial drying of northeastern Australia. Overall, the GBR developed through significant SST change and may be more resilient than previously thought.