Please use this identifier to cite or link to this item: http://irepo.futminna.edu.ng:8080/jspui/handle/123456789/31981
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dc.contributor.authorAbdulkadir, Aishetu-
dc.contributor.authorAbdullahi, Jibrin-
dc.contributor.authorIbrahim, Ishiaku-
dc.contributor.authorUsman, M. T-
dc.contributor.authorAbubakar, Alhassan-
dc.contributor.authorAisha, Bello Hassan-
dc.contributor.authorAbdullahi, Chado Salihu-
dc.date.accessioned2026-08-18T16:27:56Z-
dc.date.available2026-08-18T16:27:56Z-
dc.date.issued2026-08-06-
dc.identifier.issn2731-9431-
dc.identifier.urihttp://irepo.futminna.edu.ng:8080/jspui/handle/123456789/31981-
dc.description.abstractThe savanna ecological zones of Nigeria are vulnerable to eco-climatic anomalies driven by climate change and land degradation. Despite previous studies on individual climate stressors, few have developed sub-national spatial Eco-Climatic Resilience Indices (ECRI) that integrate both biophysical and socio-economic dimensions across the region, thereby limiting targeted climate adaptation planning. This study applied Mann–Kendall rainfall trend analysis and the Sen slope test to rainfall data acquired from the Nigeria Meteorological Agency (NIMET) across 19 stations from 1971 to 2023. A four-stage cluster sampling design was employed to sample 2400 farming households from 48 communities in the study regions. A Principal Component Analysis (PCA) was applied to reduce the dimensionality of the data from 46 variables across climatic anomalies, ecological anomalies, exposure, sensitivity, adaptation capacity, and transformative adaptation capacity. Community PCA scores were interpolated and integrated into the composite ECRI, which was then classified into five resilience zones. The findings revealed a spatial mixed trend in rainfall as stations in the Sudan-Sahelian savanna showed both significant and insignificant upward trends, with the highest rate of change recorded in Kano (+17.89 mm/year), while stations in the Guinea Savanna indicated a significant and insignificant downward trend, with the highest rate of change recorded in Makurdi (−26.43 mm/year). Although the stations in the Sudan-Sahelian showed upward rainfall trends, the ECRI map depicted a north–south resilience gradient, with very low resilience across the Sahelian savanna to the north and very high resilience across the Guinea Savanna to the south. Overall, the climate and ecological stressors were strongly related (r = 0.82). These findings imply that increased rainfall does not necessarily translate into improved climate resilience. The varying resilience levels depicted by ECRI signal the need for state and location-specific transformation/adaptation strategies to build individual, community, and state capacity for more resilient livelihoods across the study region and similar regions with comparable socio-economic and climate characteristicsen_US
dc.description.sponsorshipThis research was funded by Tertiary Education Trust Fund (TETFUND) National Research Fund (NRF) grant (TETF/ES/ DR&D-CE/NRF2021/SETI/GEO/00023/VOL.1).en_US
dc.language.isoenen_US
dc.publisherDiscover Environmenten_US
dc.subjectEco-climatic resilienceen_US
dc.subjectClimate anomaliesen_US
dc.subjectGeospatial mappingen_US
dc.subjectAdaptive capacityen_US
dc.subjectSavanna zones of Nigeriaen_US
dc.subjectLivelihood vulnerabilityen_US
dc.titleMapping climate and ecological anomalies as a veritable tool for planning eco‑climate resilience across the savanna zones of Nigeriaen_US
dc.typeArticleen_US
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