GC117-0009
Investigating Decadal Variability in the North Atlantic Using a New Time-evolving Self-organizing Maps Method

Wednesday, 16 December 2020
Poster
Qinxue Gu, Pennsylvania State University Main Campus, Meteorology and Atmospheric Science, University Park, PA, United States, Melissa Gervais, Pennsylvania State University, Department of Meteorology and Atmospheric Science, University Park, PA, United States and Elizabeth Maroon, University of Wisconsin Madison, Madison, WI, United States
Abstract:
The evolution of internal variability in the North Atlantic on decadal time scales has a critical impact on global and regional climate. Traditional methods of identifying variability are limited by their inability to represent the full spatio-temporal variability of the system, which is important for understanding the coupled dynamics in the North Atlantic. This study develops a novel method of representing the spatio-temporal evolution of internal variability using a time-evolving self-organizing maps (SOMs), a machine learning method that classifies high dimensional datasets into a specified number of clusters but in this case through providing a time series of input data. In this study, we use a long Community Earth System Model 1850 pre-industrial simulation to identify the evolution of sea surface temperature (SST) variability. The SOM is repeatedly trained using 10-year time series of winter SST in the North Atlantic sampled from 1500 years of the model simulation. The resulting SOM nodes identify the dominant patterns of 10-year continuous spatio-temporal evolutions of winter SST. These results show spatial shifts between North Atlantic Oscillation-like tripole and Atlantic Multidecadal Variability-like monopolar SST anomalies. In addition to these anomalies in the extra-tropical and tropical North Atlantic, this study also highlights the role of Greenland-Iceland-Norwegian Seas in the internal variability in the North Atlantic. The coupled atmosphere-ocean-sea ice mechanisms involved in producing these SST evolutions are then investigated through compositing multiple variables associated with deep water formation, air-sea heat flux, sea ice melt/growth, and ocean heat transport. The identification of underlying time-evolving coupled dynamics contributes to the understanding of SST evolution, bringing new insights that can benefit future studies on decadal predictability and actual decadal predictions.