Time Series Analysis of MODIS-Derived NDVI for the Hluhluwe-Imfolozi Park, South Africa: Impact of Recent Intense Drought

dc.contributor.authorMbatha, Nkanyiso
dc.contributor.authorXulu, Sifiso
dc.date.accessioned2020-01-24T12:03:17Z
dc.date.available2020-01-24T12:03:17Z
dc.date.issued2018-11-30
dc.descriptionPeer reviewed article published under Climate Journal, Volume 6 Issue 4en_US
dc.description.abstractThe variability of temperature and precipitation influenced by El Niño-Southern Oscillation (ENSO) is potentially one of key factors contributing to vegetation product in southern Africa. Thus, understanding large-scale ocean–atmospheric phenomena like the ENSO and Indian Ocean Dipole/Dipole Mode Index (DMI) is important. In this study, 16 years (2002–2017) of Moderate Resolution Imaging Spectroradiometer (MODIS) Terra/Aqua 16-day normalized difference vegetation index (NDVI), extracted and processed using JavaScript code editor in the Google Earth Engine (GEE) platform was used to analyze the vegetation response pattern of the oldest proclaimed nature reserve in Africa, the Hluhluwe-iMfolozi Park (HiP) to climatic variability. The MODIS enhanced vegetation index (EVI), burned area index (BAI), and normalized difference infrared index (NDII) were also analyzed. The study used the Modern Retrospective Analysis for the Research Application (MERRA) model monthly mean soil temperature and precipitations. The Global Land Data Assimilation System (GLDAS) evapotranspiration (ET) data were used to investigate the HiP vegetation water stress. The region in the southern part of the HiP which has land cover dominated by savanna experienced the most impact of the strong El Niño. Both the HiP NDVI inter-annual Mann–Kendal trend test and sequential Mann–Kendall (SQ-MK) test indicated a significant downward trend during the El Niño years of 2003 and 2014–2015. The SQ-MK significant trend turning point which was thought to be associated with the 2014–2015 El Niño periods begun in November 2012. The wavelet coherence and coherence phase indicated a positive teleconnection/correlation between soil temperatures, precipitation, soil moisture (NDII), and ET. This was explained by a dominant in-phase relationship between the NDVI and climatic parameters especially at a period band of 8–16 months.en_US
dc.identifier.citationMbatha, N. and Xulu, S., 2018. Time Series Analysis of MODIS-Derived NDVI for the Hluhluwe-Imfolozi Park, South Africa: Impact of Recent Intense Drought. Climate, 6(4), p.95.en_US
dc.identifier.issn2225-1154
dc.identifier.urihttps://doi.org/10.3390/cli6040095
dc.identifier.urihttps://hdl.handle.net/10530/1983
dc.language.isoenen_US
dc.publisherMDPIen_US
dc.subjectdroughten_US
dc.subjecttime series analysisen_US
dc.subjectHluhluwe-iMfolozi Parken_US
dc.subjectGoogle Earth Engineen_US
dc.subjectNDVIen_US
dc.subjectwaveleten_US
dc.titleTime Series Analysis of MODIS-Derived NDVI for the Hluhluwe-Imfolozi Park, South Africa: Impact of Recent Intense Droughten_US
dc.typeArticleen_US
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