Use este identificador para citar ou linkar para este item: https://repositorio.inpa.gov.br/handle/1/37343
Título: Comparison of spatial interpolation methods for annual and seasonal rainfall in two hotspots of biodiversity in South America
Título(s) alternativo(s): Comparação de métodos de interpolação espacial para precipitação anual e sazonal em dois hotspots de biodiversidade na América do Sul
Autor: Cerón, Wilmar Loaiza
Andreoli, Rita Valéria
Kayano, Mary Toshie
Canchala, Teresita
Carvajal, Yesid
Souza, Rodrigo Augusto Ferreira De
Palavras-chave: Biogeographic Choco
Hotspots
La Plata Basin
Rainfall
South America and spatial interpolation
Data do documento: 2021
Revista: Anais da Academia Brasileira de Ciencias
É parte de: Volume 93, Número 1, págs. 1-22
Abstract: The Colombian Biogeographic Choco (CBC) and the La Plata Basin (LPB) are regions with high biodiversity. However, these areas are characterized by scarce climatological information, complex orography, and rain-gauge network unevenly distributed. Interpolated data from the ground station might overcome these aspects. For this reason, is necessary to identify the best technique for the spatial interpolation of rainfall. Hence, the spatial interpolation techniques were applied to annual and seasonal rainfall in the CBC and LPB. Geostatistical results and deterministic approaches were compared by cross-validation. Cokriging with spherical (gaussian) model is the best interpolator in the CBC (LPB), as indicated by the lowest root mean square error (RMSE) and a standardized RMSE close to one. The CBC shows three rainfall cores: the northern, 9,000 mm/year; the central-southern, 10,000 mm/year; and the southern, 7,000 mm/ year. The LPB shows a west-east rainfall gradient, with a minimum to the west (450 mm/ year) and a maximum in the mid-west (2,000 mm/year). To the north of the LPB, rainfall reaches 1,500 mm/year, while in the south it reaches only 900 mm/year. The results in our study may be useful for scientists and decision-makers for use in environmental and hydrological models for the CBC and the LPB. © 2021, Academia Brasileira de Ciencias. All rights reserved.
DOI: 10.1590/0001-3765202120190674
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