Energy Balance, CO2 Balance, and Meteorological Aspects of Desertification Hotspots in Northeast Brazil

被引:15
作者
Silva, Any Caroline [1 ]
Rego Mendes, Keila [1 ]
Silva, Claudio Moises Santos e [1 ]
Torres Rodrigues, Daniele [2 ]
Brito Costa, Gabriel [1 ,3 ]
Thainara Correa da Silva, Duany [4 ]
Rodrigues Mutti, Pedro [1 ]
Rodrigues Ferreira, Rosaria [1 ]
Guedes Bezerra, Bergson [1 ]
机构
[1] Univ Fed Rio Grande do Norte, Dept Atmospher & Climate Sci, BR-59078970 Natal, RN, Brazil
[2] Univ Fed Piaui, Dept Stat, BR-64049550 Teresina, PI, Brazil
[3] Fed Univ Western Para, Inst Biodivers & Forests, BR-68035110 Santarem, PA, Brazil
[4] Fed Univ Western Para, Inst Engn & Geosci, BR-68035110 Santarem, PA, Brazil
关键词
microclimate; land degradation; atmosphere-biosphere interaction; modeling; DRY TROPICAL FOREST; CARBON-DIOXIDE; INTERANNUAL VARIABILITY; SEMIARID ECOSYSTEMS; CLIMATE-CHANGE; FLUXES; WATER; PATTERNS; CAATINGA; AREAS;
D O I
10.3390/w13212962
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The main objective of this study was to evaluate meteorological variables and the simulated components of energy and CO2 balances in desertification hotspots in Northeast Brazil. Meteorological data were obtained from the National Institute of Meteorology measurement network for the Cabrobo and Ibimirim sites. Initially, hourly linear trends were calculated for the meteorological variables using the non-parametric Mann-Kendall test. Then, the seasonal variability in the components of energy and CO2 balances was assessed through simulations of the simple tropical ecosystem (SITE) model. Results showed evidence of increasing air temperature trends in the Cabrobo site in the first months of the year, which was not observed in the Ibimirim site. Regarding relative humidity, increasing trends were observed in a few months over the Cabrobo site, while decreasing trends were observed in the Ibimirim site. Opposite behaviors were also identified for the trends in wind speed in both sites. Gross primary production (GPP) and net ecosystem exchange (NEE) simulated values were higher in the first half of the year in both sites. GPP varied from 0.8 to 1.2 g C m(-)(2) h(-)(1), and NEE fluctuated around approximately -5 g C m(-)(2) h(-)(1). These results indicate that rainfall seasonality is a crucial factor for the modulation of CO2 and energy balance fluxes in the Caatinga biome.
引用
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页数:17
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