Abstract

AbstractAnomalous conditions in the oceans and atmosphere have the potential to be used to enhance the predictability of flood events, enabling earlier warnings to reduce risk. In the Amazon basin, extreme flooding is consistently attributed to warmer or cooler conditions in the tropical Pacific and Atlantic oceans, with some evidence linking floods to other hydroclimatic drivers such as the Madden–Julian Oscillation (MJO). This review evaluates the impact of several hydroclimatic drivers on rainfall and river discharge regimes independently, aggregating all the information of previous studies to provide an up‐to‐date depiction of what we currently know and do not know about how variations in climate impact flooding in the Amazon. Additionally, 34 major flood events that have occurred since 1950 in the Amazon and their attribution to climate anomalies are documented and evaluated. This review finds that despite common agreement within the literature describing the relationship between phases of climate indices and hydrometeorological variables, results linking climate anomalies and flood hazard are often limited to correlation rather than to causation, while the understanding of their usefulness for flood forecasting is weak. There is a need to understand better the ocean–atmosphere response mechanisms that led to previous flood events. In particular, examining the oceanic and atmospheric conditions preceding individual hydrological extremes, as opposed to composite analysis, could provide insightful information into the magnitude and spatial distribution of anomalous sea surface temperatures required to produce extreme floods. Importantly, such an analysis could provide meaningful thresholds on which to base seasonal flood forecasts.

Highlights

  • River records highlight that, on average, the Amazon typically experiences an extreme hydrological event once per decade (Marengo et al, 2011)

  • This review discusses out what is currently known about how climate variability influences rainfall, river discharge and flooding in the Amazon basin

  • This information is a key component in aiding flood prediction, providing potential sources of predictability at interannual to decadal timescales to enable the possible implementation of early warning systems (EWS)

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Summary

| INTRODUCTION

On average, the Amazon typically experiences an extreme hydrological event (i.e. flood or drought) once per decade (Marengo et al, 2011). For the Amazon, increased rainfall and river discharge are consistently attributed to lower and upper atmospheric circulation anomalies as a consequence of anomalous SST conditions in the tropical Atlantic and Pacific oceans (Richey et al, 1989; Yoon and Zeng, 2010; Davidson et al, 2012; Marengo and Espinoza, 2016). When the TNA is abnormally warmer (cooler) than usual, the ITCZ is found to migrate anomalously north (south), bringing changes to low-level atmospheric circulation and spatial rainfall patterns These patterns are associated with a weakening (intensification) of the northeastern trade winds and moisture flux from the Atlantic basin (Enfield, 1996; Nobre and Shukla, 1996; Panisset et al, 2018). Central and tropical North Atlantic SSTs to explain variability in terrestrial water storage anomalies (De Linage, Famiglietti, & Randerson, 2014) and a statistical model that showed that northern (southern) sub-basins in the Amazon basin are better forecasted when using Pacific (Atlantic) SSTs (Uvo and Graham, 1998)

| Objective and framework
| METHODS AND DATA
Method of analysis
April 2014g
Findings
| CONCLUSIONS
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