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On the south-eastern side, we have a real interaction of the different climate modes.
On the east side, we also have a very strong influence from tropical climate modes like El Nino".
The statistical analysis suggest the potential of ANN over MR models for rainfall forecasting using large scale climate modes.
It would be particularly interesting to assess the potential effects of the main climate modes acting in the region to cover all possible climate scenarios (e.g. SAM, El Niño Southern Oscillation) during a future eruption.
After accounting for these indices the total number of stations showing statistically significant trends is reduced, suggesting that much of the observed trend in AM floods may be associated with these climate modes.
The use of dual (combined lagged ENSO IOD) input sets for calibrating and validating ANN and MR Models is proposed to investigate the simultaneous effect of past values of these two major climate modes on long-term spring rainfall prediction.
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His current research includes identifying global climate data sets (satellite proxies, gridded station data, climate mode reanalysis), assessing their qualities, combining data from different sources, and adapting these products for specific applications.
While the main mode of variability of the atmospheric circulation in the Southern Hemisphere extratropics is the SAM25, the last 50 years of seasonal and decadal climate variability of Antarctica have been described as a consequence of the interplay between the former climate mode and the El Niño Southern Oscillation (ENSO 26.
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Whereas there was lack of decadal model of climate variability in the Indian Ocean (Han et al. 2014), decadal variations of the ITF transport are mainly associated with the decadal climate mode in the Pacific, such as the Pacific Decadal Oscillation or the Interdecadal Pacific Oscillation (Zhuang et al. 2013).
In angiosperms, two consecutive slowdowns in diversification were identified for the current cool climate mode.
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