Climate Fluctuations of Tropical Coupled Systems—The Role of Ocean Dynamics
By Ping Chang, Toshio Yamagata, P. Schopf, Swadhin K. Behera, J. Carton, W. Kessler, G. Meyers, T. Qu, F. Schott, S. Shetye and 1 more. 2006
253 citations recorded by the source corpus.
Subfields: Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/89c79b2cf38c145a8184737e2fd28a993758ea1d
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In Global and Planetary Change
In Oceanography
Citations in the corpus
- On the origin of equatorial Atlantic biases in coupled general circulation models (2008, background): “Since modes of tropical Atlantic variability involve ocean–atmospheric feedbacks that are dependent on the mean state (Xie and Carton 2004; Chang et al. 2006; Keenlyside and Latif 2007), the failure of coupled GCMs to simulate a realistic mean state bodes ill for their ability to predict…”
- Tropical Atlantic biases and their relation to surface wind stress and terrestrial precipitation (2012, background): “However, since they prescribe wind stress year round, the particular importance of MAM surface winds needs further confirmation.”
- Pantropical climate interactions (2019, background): “Interactions with higher latitudes can also influence the character of seasonal to decadal time-scale variability in the tropics, and there is extensive literature on this topic (23, 24).”
- Sea surface temperature variability: patterns and mechanisms. (2010, background): “Recent reviews of these modes are provided in Xie and Carton (2004) and Chang et al. (2006).”
- THE PIRATA PROGRAM History, Accomplishments, and Future Directions * (2008, background): “…achieves its maximum development during boreal spring (March-April) when the ITCZ is at its southernmost position, whereas the equatorial mode is at its maximum during boreal summer (June-August), when the ITCZ is at its northernmost position (e.g., Xie and Carton 2004; Chang et al. 2006).”
- Tropical Atmosphere-Ocean Interactions in a Conceptual Framework (2009, background): “This relation may result from local feedbacks, such as the wind–evaporation–SST and coastal upwelling feedbacks that are active during boreal summer and autumn (Chang et al. 2006b).”