Understanding the intrinsic characteristics and nonlinear dynamics of dry-wet conditions in rain-fed agricultural regions like Guinea is crucial for agricultural planning and water resources management. Standardized Precipitation Index (SPI) for 1, 3, 6, 9 and 12- month timescales, derived from eight synoptic stations in Guinea between 1991 and 2020, were used to assess dry-wet conditions. By applying Multifractal Detrended Fluctuation Analysis (MFDFA) hybridized with the Improved Complete Ensemble Empirical Mode Decomposition with Adaptive Noise (ICEEMDAN) algorithm on multiscale SPIs (SPI-1, SPI-3, SPI-6, SPI-9 and SPI-12), the multifractality, the long-term memory and the complexity of temporal fluctuations of dry-wet conditions were investigated in Guinea. The results indicate that (1) anti-persistence, anti-persistence combined with non-stationary, persistence, and randomness is present in the SPI series. In particular, the SPI-3 and SPI-6 series are persistent at all the studied stations, while the SPI-9 and SPI-12 series are persistent or anti-persistent depending on the station; (2) all SPI series exhibit multifractal dynamics, with varying strengths influenced by timescale and geographical location. Multifractality in SPI-3 is primarily due to long-term temporal correlations, while SPI-6, SPI-9 and SPI-12 are influenced by both long-term correlations and the broadness of the probability distribution function, with long-term correlation being the dominant factor. Consequently, SPI-6, SPI-9, and SPI-12 are potentially more sensitive to climate dynamics than SPI-3; (3) predictive models based on persistence and multifractal theories are effective for SPI-3, and SPI-6, while for SPI-9 and SPI-12, models based on either persistence or averaging previous values are recommended, depending on the station.
No takes yet. Share an insight, caveat, or question.
Noukpo et al. (2025) studied this question.
Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context: