NAO and PNA influences on winter temperature and precipitation over the eastern United States in CMIP5 GCMs

Author:

Ning Liang,Bradley Raymond S.

Funder

U.S. Department of the Interior's Northeast Climate Science Center

Chinese Academy of Sciences

The Priority Academic Development Program of Jiangsu Higher Education Institutions

Publisher

Springer Science and Business Media LLC

Subject

Atmospheric Science

Reference70 articles.

1. Allan AM (2013) Analyzing the present and future Pacific-North American teleconnection using global and regional climate models. Doctoral dissertation, Oregon State University, p 190

2. Allan AM, Hostetler SW, Alder JR (2014) Analysis of the present and future winter Pacific-North American teleconnection in the ECHAM5 global and RegCM3 regional climate models. Clim Dyn 42:1671–1682. doi: 10.1007/s00382-013-1910-x

3. Bai X, Wang J, Sellinger C, Clites A, Assel R (2012) Interannual variability of Great Lakes ice cover and its relationship to NAO and ENSO. J Geophys Res 117:C03002. doi: 10.1029/2010JC006932

4. Barnston AG, Livezey RE (1987) Classification, seasonality, and persistence of low-frequency atmospheric circulation patterns. Mon Weather Rev 115:1083–1126

5. Bellouin N, Boucher O, Haywood J, Johnson C, Jones A, Rae J, Woodward S (2007) Improved representation of aerosols for HadGEM2. Meteorological Office Hadley Centre, Technical Note 73, March 2007

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