Abstract
Over the last 3 million years or so “ice ages” — brief periods of colder weather allowing large sheets of ice to develop — have been the dominant long term feature of Earth’s climate.
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References
Bartlett, M..S. (1946) “On the Theoretical Specification of Sampling Properties of Autocorrelated Time Series.” Journal of the Royal Statistical Society B 8, pp. 27–41.
Box, G.E.P. and G. M. Jenkins (1976). Time Series Analysis: Forecasting and Control. Holden Day: San Francisco.
Dickey, D. and W. Fuller (1981). “Likelihood Ratio Tests for Autoregressive Time Series with a Unit Root.” Econometrica 49, pp. 1057–72.
Granger, C.W.J. and P. Newbold (1977). Forecasting Economic Time Series. Academic Press: New York.
Muller, R. A. and G. J. MacDonald (1997) “Glacial Cycles and Astronomical Forcing.” Science 277, pp. 215–218.
Raymo, M. (1997). “The Timing of Major Climate Terminations.” Paleoceanography 12(4), pp. 577–85.
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© 2000 Springer Science+Business Media New York
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Patterson, D.M., Ashley, R.A. (2000). Climatological Data. In: A Nonlinear Time Series Workshop. Dynamic Modeling and Econometrics in Economics and Finance, vol 2. Springer, Boston, MA. https://doi.org/10.1007/978-1-4419-8688-7_11
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DOI: https://doi.org/10.1007/978-1-4419-8688-7_11
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