Articles | Volume 14, issue 5
https://doi.org/10.5194/cp-14-665-2018
https://doi.org/10.5194/cp-14-665-2018
Research article
 | 
28 May 2018
Research article |  | 28 May 2018

Placing the Common Era in a Holocene context: millennial to centennial patterns and trends in the hydroclimate of North America over the past 2000 years

Bryan N. Shuman, Cody Routson, Nicholas McKay, Sherilyn Fritz, Darrell Kaufman, Matthew E. Kirby, Connor Nolan, Gregory T. Pederson, and Jeannine-Marie St-Jacques

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Cited articles

Andersen, K. K., Ditlevsen, P. D., Rasmussen, S. O., Clausen, H. B., Vinther, B. M., Johnsen, S. J., and Steffensen, J. P.: Retrieving a common accumulation record from Greenland ice cores for the past 1800 years, J. Geophys. Res., 111, D15106, https://doi.org/10.1029/2005JD006765, 2006.
Anderson, L.: Holocene record of precipitation seasonality from lake calcite δ18O in the central Rocky Mountains, United States, Geology, 39, 211–214, https://doi.org/10.1130/g31575.1, 2011.
Anderson, L.: Rocky Mountain hydroclimate: holocene variability and the role of insolation, ENSO, and the North American Monsoon, Global Planet. Change, 92, 198–208, https://doi.org/10.1016/j.gloplacha.2012.05.012, 2012.
Anderson, L., Abbott, M. B., Finney, B. P., and Burns, S. J.: Regional atmospheric circulation change in the North Pacific during the Holocene inferred from lacustrine carbonate oxygen isotopes, Yukon Territory, Canada, Quaternary Res., 64, 21–35, 2005.
Anderson, L., Abbott, M. B., Finney, B. P., and Burns, S. J.: Late Holocene moisture balance variability in the southwest Yukon Territory, Canada, Quaternary Sci. Rev., 26, 130–141, 2007.
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Short summary
A synthesis of 93 published records reveals that moisture availability increased over large portions of North America over the past 2000 years, the Common Era (CE). In many records, the second millennium CE tended to be wetter than the first millennium CE. The long-term changes formed the background for annual to multi-decade variations, such as "mega-droughts", and also provide a context for amplified rates of hydrologic change today.
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