Please use this identifier to cite or link to this item: http://repository.futminna.edu.ng:8080/jspui/handle/123456789/18217
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dc.contributor.authorJimoh, O. D.-
dc.contributor.authorOtache, M. Y.-
dc.contributor.authorAdesiji, A. R.-
dc.contributor.authorOlaleye, R. S.-
dc.contributor.authorAgajo, J-
dc.date.accessioned2023-04-07T16:43:24Z-
dc.date.available2023-04-07T16:43:24Z-
dc.date.issued2023-
dc.identifier.urihttp://repository.futminna.edu.ng:8080/jspui/handle/123456789/18217-
dc.description.abstractMeteorological droughts occur when there is deficiency in rainfall; i.e. rainfall availability is below some acclaimed normal values. Hence, the greater challenge is to be able to obtain suitable methods for assessing drought occurrence, its onset or initiation and termination. Thus, an attempt was made in this paper to evaluate the performance of Standardised Precipitation Index (SPI) and Standardised Precipitation Anomaly Index (SPAI) to characterise drought in Northern Nigeria for purposes of comparison and eventual adoption of probable candidate index for the development of an Early Warning System. The findings indicated that despite the fact that the annual timescale may be long, it can be employed to obtain information on the temporal evolution of drought especially, regional behaviour. However, monthly timescale can be more appropriate if emphasis is on evaluating the effects of drought in situations relating to water supply, agriculture and groundwater abstractions. The SPAI can be employed for periodic rainfall time series though; it accentuates drought signatures and may not necessarily dampen high fluctuations due to implications of high climatic variability considering the stochastic nature and state transition of drought phenomena. On the other hand, the temporal evolution of SPI and SPAI were not coherent at different temporal accumulations with differences in fluctuations. However, despite the differences between the SPI and SPAI, generally at some timescales, for instance, 6-month accumulation, both spatial and temporal distributions of drought characteristics were seemingly consistent. In view of the observed shortcomings of both indices, especially the SPI, the Standardised Nonstationary Precipitation Index (SnsPI) should be looked into and too, other indexes that take into consideration the implications of global warming by incorporating potential evapotranspiration may be deemed more suitable for drought studies in Northern Nigeria.en_US
dc.description.sponsorshipTertiary Education Trust Fund (TETFUND) Nigeriaen_US
dc.language.isoenen_US
dc.publisherJournal of Water Resource and Protectionen_US
dc.relation.ispartofseriesvolume 15(2);PP. 51 -70-
dc.subjectcharacterisationen_US
dc.subjecttimescaleen_US
dc.subjectmeteorologicalen_US
dc.subjectdroughten_US
dc.subjectmetricsen_US
dc.titleCharacterisation of Meteorological Drought in Northern Nigeria Using Comparative Rainfall-Based Drought Metricsen_US
dc.typeArticleen_US
Appears in Collections:Civil Engineering

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