4.6 Article

The new historical flood of 2021 in the Amazon River compared to major floods of the 21st century: Atmospheric features in the context of the intensification of floods

Journal

WEATHER AND CLIMATE EXTREMES
Volume 35, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.wace.2021.100406

Keywords

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Funding

  1. ANR
  2. IRD [ANR-18-MPGA-0008]
  3. Brazilian National Institute of Science and Technology for Climate Change Phase 2 under CNPq [465501/2014-1]
  4. Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) [2014/50848-9, 2017/09659-6]
  5. National Coordination for High Level Education and Training (CAPES) [88887.136402/2017-00]
  6. CNPq [301397/2019-8]
  7. Newton Fund through the Met Office Climate Science for Service Partnership Brazil (CSSP Brazil) Predicting the Evolution of the Amazon Catchment to Forecast the Level Of Water (PEACFLOW) project
  8. Max-Planck-Society
  9. INPA

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A new extreme flood occurred in the Amazon Basin in June 2021, which was associated with an intensification of atmospheric upward motion in the northern Amazonia. This was related to an intensification of the Walker circulations. Additionally, there was also an intensification of the continental Hadley circulation, resulting in dry conditions in southern and southeastern Amazonia.
In June 2021 a new extreme flood was reported in the Amazon Basin, the largest hydrological system on Earth. During this event water level was above 29 m (the emergency threshold) for 91 days at Manaus station (Brazil), surpassing even the previous historical flood of 2012. Since the late 1990s, 9 extreme floods occurred, while only 8 events were reported from 1903 to 1998. Here we report that the 2021 flood is associated with an intensification of the atmospheric upward motion in the northern Amazonia (5?degrees S-5?degrees N), which is related to an intensification of the Walker circulations. This atmospheric feature is associated with an enhanced of deep convective clouds and intense rainfall over the northern Amazonia that produce positive anomalies of terrestrial water storage over northern Amazonia in the 2021 austral summer. The intensification of Walker circulation is associated with La Nina conditions that characterize the major floods observed in Amazonia during the 21st century (2009, 2012 and 2021). However, during the 2021 an intensification of the continental Hadley circulation is also observed. This feature produces simultaneous dry conditions over southern and southeastern Amazonia, where negative rainfall anomalies, low frequency of deep convective clouds and negative anomalies of terrestrial water storage are observed.

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