The Climate of the United States since 1895: Spatial and Temporal Changes
- 1 March 1980
- journal article
- Published by American Meteorological Society in Monthly Weather Review
- Vol. 108 (3) , 249-266
- https://doi.org/10.1175/1520-0493(1980)108<0249:tcotus>2.0.co;2
Abstract
Time series of temperature and precipitation weighted by area and grouped by season for each of the 48 contiguous United States were analyzed. Within an 83-year period of record (1895–1977) three subperiods or climatic regimes are identified and the differences in their means and standard deviations plotted and analyzed. The statistical significance of the changes in the mean was calculated by using a two-tailed t test; for changes in the standard deviation, the F-ratio test was used. The variation patterns suggest that an east-west mode for changes in both temperature and precipitation is dominant over the continental United States. Over the past 25 years the average temperature of the United States has decreased∼1°F (0.6°C) from the relatively warm interval of the 1920's to the middle 1950's. However, most of this cooling has occurred in the eastern United States. In winter, for example, the southeastern United States cooled ∼3°F (1.7°C), whereas the Far West actually recorded warmer mean tempe... Abstract Time series of temperature and precipitation weighted by area and grouped by season for each of the 48 contiguous United States were analyzed. Within an 83-year period of record (1895–1977) three subperiods or climatic regimes are identified and the differences in their means and standard deviations plotted and analyzed. The statistical significance of the changes in the mean was calculated by using a two-tailed t test; for changes in the standard deviation, the F-ratio test was used. The variation patterns suggest that an east-west mode for changes in both temperature and precipitation is dominant over the continental United States. Over the past 25 years the average temperature of the United States has decreased∼1°F (0.6°C) from the relatively warm interval of the 1920's to the middle 1950's. However, most of this cooling has occurred in the eastern United States. In winter, for example, the southeastern United States cooled ∼3°F (1.7°C), whereas the Far West actually recorded warmer mean tempe...Keywords
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