2017
DOI: 10.1016/j.atmosres.2016.11.006
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Evaluating satellite-derived long-term historical precipitation datasets for drought monitoring in Chile

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Cited by 121 publications
(36 citation statements)
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“…e di erences observed in the SPI1D between rain gauges and CHIRPS can be attributed mainly to the underestimations over the CS region, although all the CWA exhibit the same underestimation pattern by CHIRPS. e lack of zero values can arise from the screening procedure developed to remove "false zeros" in the CHIRPS estimations [50], a bias previously reported by Zambrano et al and Katsanos et al [12,51]. Regarding the remaining timescales and wet and dry categories, CHIRPS estimates and precipitation from rain gauges show a similar behaviour, although with larger regional dispersion considering the SPI6 ( Figure 6).…”
Section: Spi Classification For Wet and Dry Categoriesmentioning
confidence: 65%
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“…e di erences observed in the SPI1D between rain gauges and CHIRPS can be attributed mainly to the underestimations over the CS region, although all the CWA exhibit the same underestimation pattern by CHIRPS. e lack of zero values can arise from the screening procedure developed to remove "false zeros" in the CHIRPS estimations [50], a bias previously reported by Zambrano et al and Katsanos et al [12,51]. Regarding the remaining timescales and wet and dry categories, CHIRPS estimates and precipitation from rain gauges show a similar behaviour, although with larger regional dispersion considering the SPI6 ( Figure 6).…”
Section: Spi Classification For Wet and Dry Categoriesmentioning
confidence: 65%
“…As described by Funk et al [9], the CHIRPS algorithm (i) is built around a 0.05°c limatology that incorporates satellite information to represent sparsely gauged locations, (ii) incorporates monthly 1981-present 0.05°infrared cold cloud duration-based precipitation estimates, (iii) blends station data to produce a preliminary information product with a latency of about 2 days after the end of a pentad and a nal product with an average latency of about 3 weeks, and (iv) uses a novel blending procedure incorporating the spatial correlation structure of infrared cold cloud duration estimates to assign interpolation weights. is dataset was found to reproduce adequately several characteristics of precipitation over South America [12,17,43] and particularly over the CWA, showing a good agreement for the representation of the seasonal and interannual variability of precipitation and its spatial patterns [24].…”
Section: Advances In Meteorologymentioning
confidence: 72%
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