Dukhovskoy, D. S. (2004). Arctic decadal variability: An auto-oscillatory system of heat and fresh water exchange.
Geophys. Res. Lett., 31(3).
Goto-Maeda, Y., Shin, D. W., & O'Brien, J. J. (2008). Freeze probability of Florida in a regional climate model and climate indices.
Geophys. Res. Lett., 35(11).
Hu, A., Meehl, G. A., Han, W., Lu, J., & Strand, W. G. (2013). Energy balance in a warm world without the ocean conveyor belt and sea ice.
Geophys. Res. Lett., 40(23), 6242–6246.
Hu, A., Meehl, G. A., Han, W., & Yin, J. (2009). Transient response of the MOC and climate to potential melting of the Greenland Ice Sheet in the 21st century.
Geophys. Res. Lett., 36(10).
Kara, A. B., Metzger, E. J., & Bourassa, M. A. (2007). Ocean current and wave effects on wind stress drag coefficient over the global ocean.
Geophys. Res. Lett., 34(1).
Kim, D., Lee, S. - K., Lopez, H., Foltz, G. R., Misra, V., & Kumar, A. (2020). On the Role of Pacific-Atlantic SST Contrast and Associated Caribbean Sea Convection in August-October U.S. Regional Rainfall Variability.
Geophys. Res. Lett., 47(11).
Abstract: This study investigates the large‐scale atmospheric processes that lead to U.S. precipitation variability in late summer to midfall (August–October; ASO) and shows that the well‐recognized relationship between North Atlantic Subtropical High and U.S. precipitation in peak summer (June–August) significantly weakens in ASO. The working hypothesis derived from our analysis is that in ASO convective activity in the Caribbean Sea, modulated by the tropical Pacific‐Atlantic sea surface temperature (SST) anomaly contrast, directly influences the North American Low‐Level Jet and thus U.S. precipitation east of the Rockies, through a Gill‐type response. This hypothesis derived from observations is strongly supported by a long‐term climate model simulation and by a linear baroclinic atmospheric model with prescribed diabatic forcings in the Caribbean Sea. This study integrates key findings from previous studies and advances a consistent physical rationale that links the Pacific‐Atlantic SST anomaly contrast, Caribbean Sea convective activity, and U.S. rainfall in ASO.
Koster, R. D., Mahanama, S. P. P., Yamada, T. J., Balsamo, G., Berg, A. A., Boisserie, M., et al. (2010). Contribution of land surface initialization to subseasonal forecast skill: First results from a multi-model experiment.
Geophys. Res. Lett., 37(2), n/a-n/a.
Lagerloef, G. S. E., Lukas, R., Bonjean, F., Gunn, J. T., Mitchum, G. T., Bourassa, M., et al. (2003). El Niño Tropical Pacific Ocean surface current and temperature evolution in 2002 and outlook for early 2003.
Geophys. Res. Lett., 30(10).
LaRow, T. E., Stefanova, L., Shin, D. - W., & Cocke, S. (2010). Seasonal Atlantic tropical cyclone hindcasting/forecasting using two sea surface temperature datasets.
Geophys. Res. Lett., 37(2).
Lu, J., Hu, A., & Zeng, Z. (2014). On the possible interaction between internal climate variability and forced climate change.
Geophys. Res. Lett., 41(8), 2962–2970.