Inundation dynamics in seasonally dry floodplain forests in southeastern Brazil

Author:

Meyer Oliveira Aline1ORCID,van Meerveld Ilja1ORCID,Gianasi Fernanda Moreira2ORCID,Maciel Silva‐Sene André2ORCID,Farrapo Camila Laís2ORCID,de Carvalho Araújo Felipe2ORCID,Oliveira Fernanda2ORCID,Aparecido Silva Ferreira Leony2ORCID,Carolina Arantes da Silva Lidiany2ORCID,Gama Reis Miguel2ORCID,Vieira Pompeu Patricia3ORCID,Manoel dos Santos Rubens2ORCID

Affiliation:

1. Department of Geography University of Zurich Zurich Switzerland

2. Department of Forest Sciences Federal University of Lavras Lavras Minas Gerais Brazil

3. Unit of Aquidauana State University of Mato Grosso do Sul Aquidauana Mato Grosso do Sul Brazil

Abstract

AbstractFloodplains are one of the most threatened ecosystems. Even though the vegetation composition in floodplain forests is expected to reflect the variation in groundwater levels and flood duration and frequency, there is little field data on the inundation dynamics (e.g., the variability in flood duration and flood frequency), especially for the understudied seasonally dry tropics. This limits our understanding of these ecosystems and the mechanisms that cause the flooding. We, therefore, investigated six floodplain forests in the state of Minas Gerais in Brazil for 1.5 years (two wet seasons): Capivari, Jacaré, and Aiuruoca in the Rio Grande basin, and Jequitaí, Verde Grande, and Carinhanha in the São Francisco basin. These locations span a range of climates (humid subtropical to seasonal tropical) and biomes (Atlantic forest to Caatinga). At each location, we continuously measured water levels in five geomorphologically distinct eco‐units: marginal levee, lower terrace, higher terrace, lower plain, and higher plain, providing a unique hydrological dataset for these understudied regions. The levees and terraces were flooded for longer periods than the plains. Inundation of the terraces lasted around 40 days per year. The levees in the Rio Grande basin were flooded for shorter durations. In the São Francisco basin, the flooding of the levees lasted longer and the water level regime of the levees was more similar to that of the terraces. In the Rio Grande basin, flooding was most likely caused by rising groundwater levels (i.e., “flow pulse”) and flood pulses that caused overbank flooding. In the São Francisco basin, inundation was most likely caused by overbank flooding (i.e., “flood pulse”). These findings highlight the large variation in inundation dynamics across floodplain forests and are relevant to predict the impacts of changes in the flood regime due to climate change and other anthropogenic changes on floodplain forest functioning.

Funder

Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung

Conselho Nacional de Desenvolvimento Científico e Tecnológico

Publisher

Wiley

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