Modelling the spatial dependence of the rainfall erosivity index in the Brazilian semiarid region

Authors

  • André Quintão de Almeida Universidade Federal de Sergipe (UFS), Departamento de Engenharia Agrícola, Campus São Cristovão, Cidade Universitária Prof. José Aloísio de Campos, Avenida Marechal Rondon, s/no, Jardim Rosa Elze, CEP 49100-000 São Cristóvão, SE.
  • Rodolfo Marcondes Silva Souza Universidade Federal de Pernambuco, Departamento de Energia Nuclear, Avenida Prof. Luiz Freire, no 1.000, Cidade Universitária, CEP 50740-545 Recife, PE
  • Diego Campana Loureiro Universidade Federal de Sergipe (UFS), Departamento de Engenharia Agrícola, Campus São Cristovão, Cidade Universitária Prof. José Aloísio de Campos, Avenida Marechal Rondon, s/no, Jardim Rosa Elze, CEP 49100-000 São Cristóvão, SE.
  • Donizete dos Reis Pereira Universidade Federal de Viçosa, Campus Florestal, Rodovia LMG 818, Km 6, CEP 35690-000 Florestal, MG.
  • Marcus Aurélio Soares Cruz Embrapa Tabuleiros Costeiros, Núcleo de Apoio à Programação, Avenida Beira Mar, no 3.250, Jardins, CEP 49025-040 Aracaju, SE.
  • Jodnes Sobreira Vieira Universidade Federal de Sergipe, Departamento de Zootecnia, Campus São Cristovão, Cidade Universitária Prof. José Aloísio de Campos, Avenida Marechal Rondon, s/no, Jardim Rosa Elze, CEP 49100-000 São Cristóvão, SE.

DOI:

https://doi.org/10.1590/S1678-3921.pab2017.v52.24043

Keywords:

EI30, geostatistics, Northeastern Brazil, semivariogram

Abstract

The objective of this work was to model the spatial dependence and to map the rainfall erosivity index (EI30) in the semiarid region of Brazil. Registers of monthly erosivity from 210 rainfall stations were used, with daily time series equal to or greater than 15 years. Based on the values of the EI30, a spatial dependence model was made by adjusting the semivariogram. From the semivariogram models, erosivity isoline maps were generated with a kriging interpolator. According to the historical data series, the maximum monthly average value of the EI30 was observed in March, and the annual value ranged from 1,439 to 5,864 MJ mm ha-1 per year, classified as low and moderate, respectively. The highest EI30 values were obtained in the northern and southern extremes of the semiarid region. Average spatial dependence was observed for rainfall erosivity, in most months, especially with the spherical semivariogram model. The range of erosivity varied from 62 to 1,508 km for the monthly EI30 and was of approximately 1,046 km for the annual one. The applied model, with the validation of the semivariograms using the jackknife test, allows the spatialization of the EI30 for the semiarid region of Brazil.

Published

2017-07-07

How to Cite

Almeida, A. Q. de, Souza, R. M. S., Loureiro, D. C., Pereira, D. dos R., Cruz, M. A. S., & Vieira, J. S. (2017). Modelling the spatial dependence of the rainfall erosivity index in the Brazilian semiarid region. Pesquisa Agropecuaria Brasileira, 52(6), 371–379. https://doi.org/10.1590/S1678-3921.pab2017.v52.24043

Issue

Section

AGROMETEOROLOGY