@Article{SantosAvViChAcPoCu:2022:PrRaEr,
author = "Santos, Wharley Pereira dos and Avanzi, Junior Cesar and Viola,
Marcelo Ribeiro and Chou, Sin Chan and Acuña-Guzman, Salvador
Francisco and Pontes, Lucas Machado and Curi, Nilton",
affiliation = "{Universidade Federal de Lavras (UFLA)} and {Universidade Federal
de Lavras (UFLA)} and {Universidade Federal de Lavras (UFLA)} and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and
{Universidade Federal de Lavras (UFLA)} and {Universidade de
S{\~a}o Paulo (USP)} and {Universidade Federal de Lavras
(UFLA)}",
title = "Projections of rainfall erosivity in climate change scenarios for
the largest watershed within Brazilian territory",
journal = "Catena",
year = "2022",
volume = "213",
pages = "e106225",
month = "Jun",
keywords = "Amazon and Cerrado biomes, Climate change, Downscaling, Soil and
water conservation, Water erosion.",
abstract = "Global climate change can potentially threaten agricultural
production due to endangered natural resources, such as rainfall
patterns. Thus, extreme rainfall events can cause greater rainfall
erosivity, consequently, greater soil erosion. Conversely, a
reduction in rainfall amount can lead to water scarcity for the
agriculture production process. This way, it is a foremost need to
model climatic conditions under global climate change scenarios,
particularly in places where rainfall data tends to increase. This
work aimed to project rainfall erosivity in the major Brazilian
watershed, the Tocantins-Araguaia river basin, throughout the 21st
century under two Intergovernmental Panel for Climate Change Fifth
Assessment Report (IPCC AR5) Scenarios, the Representative
Concentration Pathways, RCP4.5 and RCP8.5 scenarios. This study
uses the downscaling of four global climate models of the Coupled
Model Intercomparison Project (CMIP5) by the Eta regional climate
model, used by the Brazilian National Institute for Space
Research. The average rainfall erosivity was calculated based on
the Modified Fournier Index in three periods of 30-year length
throughout the 21st century. Time series of R-factor were analyzed
at rain gauge station points overlapping regional model grid cells
over the basin for the 19612099 period. Projections indicated
lower annual average rainfall erosivity values in comparison with
historical data. Estimated mean rainfall erosivity values were
10,977.69 ± 526 MJ mm ha\−1 h\−1 yr\−1 for
the RCP4.5 scenario, and 10,379.71 ± 723 MJ mm ha\−1
h\−1 yr\−1 for the most pessimistic climate change
scenario, RCP8.5. The largest reductions of the mean R-factor
reached 5,5% for the multi-model ensemble projections for near
future, and 15.4% for the ensemble projections models for
long-term, with the greatest decreasing trends under RCP8.5.
Reductions greater than 2,000 MJ mm ha\−1 h\−1 are
expected throughout the 21st century according to multi-model
ensemble projections models under RCP8.5 scenario in most of the
watershed. Decreasing rainfall erosivity factor in both RCP
scenarios was due to a lower rainfall depth. However, the value of
rainfall erosivity is still considered high and should be taken
into account in soil conservation practices. Furthermore, the
smaller rainfall amount indicates a possible reduction in water
availability for crops of longer cycle, and increase in spatial
variability of less intense rainfall.",
doi = "10.1016/j.catena.2022.106225",
url = "http://dx.doi.org/10.1016/j.catena.2022.106225",
issn = "0341-8162",
language = "en",
targetfile = "santos_2022_projection.pdf",
urlaccessdate = "23 maio 2024"
}