Caatinga 2017
DOI: 10.1007/978-3-319-68339-3_10
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Water as Capital and Its Uses in the Caatinga

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Cited by 39 publications
(26 citation statements)
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“…The unplanned use of plowing and harrowing on cultivated land stimulates the oxidation of organic matter and degradation of the soil structure [7,14]. In SDTF, this process is more intense due to the ready availability of solar energy and uncertainty of rainfall-the predominant hot semi-arid climate is characterized by a poor temporal and spatial distribution of rainfall [15], with a frequent occurrence of both dry years and consecutive dry days during the rainy season.…”
Section: Introductionmentioning
confidence: 99%
“…The unplanned use of plowing and harrowing on cultivated land stimulates the oxidation of organic matter and degradation of the soil structure [7,14]. In SDTF, this process is more intense due to the ready availability of solar energy and uncertainty of rainfall-the predominant hot semi-arid climate is characterized by a poor temporal and spatial distribution of rainfall [15], with a frequent occurrence of both dry years and consecutive dry days during the rainy season.…”
Section: Introductionmentioning
confidence: 99%
“…In this region, which hosts the largest seasonally dry tropical forest in the world (Fig. 1; Pennington et al 2009), pronounced rainfall seasonality (Nimer 1972, Andrade et al 2017) strongly influences arthropod abundance (Vasconcellos et al 2010, Franc ßa et al 2020 and acts as a cue to set the timing and intensity of bird breeding and moulting (Cavalcanti et al 2016. The observed decrease in the number of records of Xenopsaris in the Caatinga between April and November is congruent with both rainfall seasonality (Fig.…”
Section: Discussionmentioning
confidence: 65%
“…2009), pronounced rainfall seasonality (Nimer 1972, Andrade et al . 2017) strongly influences arthropod abundance (Vasconcellos et al . 2010, França et al .…”
Section: Discussionmentioning
confidence: 99%
“…Soils are mostly of Pre‐Cambrian origin, nutrient‐rich, stony and shallow, while sandy soils of sedimentary origin are deep and nutrient‐poor, but they cover a relatively small fraction (~30%) of the Caatinga region (Moro et al, 2016). The Caatinga dry forest encompasses a wide variation in precipitation regimes, mostly from 400 to 1200 mm/year, with up to 70% of the annual precipitation concentrated into a single month (see Andrade et al, 2017, for further detail on precipitation regimes). Average annual temperature ranges from 19°C in the southern Caatinga to 28°C in the northern and eastern portions (Silva & Souza, 2018).…”
Section: Methodsmentioning
confidence: 99%