2017
DOI: 10.5194/bg-14-4355-2017
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The influence of El Niño–Southern Oscillation regimes on eastern African vegetation and its future implications under the RCP8.5 warming scenario

Abstract: Abstract. The El Niño-Southern Oscillation (ENSO) is the main driver of the interannual variability in eastern African rainfall, with a significant impact on vegetation and agriculture and dire consequences for food and social security. In this study, we identify and quantify the ENSO contribution to the eastern African rainfall variability to forecast future eastern African vegetation response to rainfall variability related to a predicted intensified ENSO. To differentiate the vegetation variability due to E… Show more

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Cited by 38 publications
(31 citation statements)
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“…Likewise, CCSM4 has improved El Niño-Southern Oscillation (ENSO) variability with more reasonable frequency distribution compared to earlier versions of CCSMs [32]. ENSO is a major driver of interannual rainfall variability in eastern Africa [33].…”
Section: Environmental Modelling Datamentioning
confidence: 99%
“…Likewise, CCSM4 has improved El Niño-Southern Oscillation (ENSO) variability with more reasonable frequency distribution compared to earlier versions of CCSMs [32]. ENSO is a major driver of interannual rainfall variability in eastern Africa [33].…”
Section: Environmental Modelling Datamentioning
confidence: 99%
“…In this paper, we demonstrated the ability of TropWet to identify significant changes in the extent of green vegetation over the Southern African region. In this manner, TropWet is able to support on-going efforts to quantify the specific effects of variations in El Niño or La Niña events (e.g., [44]). In doing so, policy makers have a tool to examine the implications of these events and help mitigate against them.…”
Section: Discussionmentioning
confidence: 99%
“…TropWet was also applied to the Southern Africa region including Angola, Namibia, South Africa, Botswana, Zimbabwe, Zambia, Swaziland, Lesotho, Malawi, and Mozambique ( Figure 1). This region is vulnerable to the effects of global atmospheric circulation patterns such as the El Niño-Southern Oscillation (ENSO) and the Subtropical Indian Ocean Dipole (SIOD) [44,45]. Evidence shows that La Niña events coinciding with a positive SIOD can result in wetter than average conditions, whereas El Niño events coinciding with a negative SIOD phase can result in drier conditions [69].…”
Section: Southern African Countriesmentioning
confidence: 99%
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