Assessing how accumulated precipitation and long dry sequences impact the soil water storage
Precipitation or no precipitation persistent over time often became extreme weather conditions with greater regional economic impact. The temporal and spatial variability of these variables, together with the evapotranspiration, is crucial in the east-northeast of Argentina, where rain-fed agricultu...
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John Wiley and Sons Ltd
2017
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| LEADER | 14292caa a22011657a 4500 | ||
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| 003 | AR-BaUEN | ||
| 005 | 20230518204602.0 | ||
| 008 | 190410s2017 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-85018712643 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 030 | |a IJCLE | ||
| 100 | 1 | |a Pántano, V.C. | |
| 245 | 1 | 0 | |a Assessing how accumulated precipitation and long dry sequences impact the soil water storage |
| 260 | |b John Wiley and Sons Ltd |c 2017 | ||
| 270 | 1 | 0 | |m Pántano, V.C.; Departamento de Ciencias de la Atmósfera y los Océanos, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos AiresArgentina; email: vpantano@at.fcen.uba.ar |
| 506 | |2 openaire |e Política editorial | ||
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| 504 | |a Vicente-Serrano, S.M., Beguería-Portugués, S., Estimating extreme dry-spell risk in the middle Ebro valley (northeastern Spain): a comparative analysis of partial duration series with a General Pareto distribution and annual maxima series with a Gumbel distribution (2003) Int. J. Climatol., 23, pp. 1103-1118. , https://doi.org/10.1002/joc.934 | ||
| 520 | 3 | |a Precipitation or no precipitation persistent over time often became extreme weather conditions with greater regional economic impact. The temporal and spatial variability of these variables, together with the evapotranspiration, is crucial in the east-northeast of Argentina, where rain-fed agricultural production is carried out. In this work, the frequency of precipitation was studied from dry spells and complemented with an analysis of the accumulated precipitation and evapotranspiration. In particular, dry sequences longer than 15 days, return period and severity, were the focus of this study. Finally, the impact of the amount and frequency of precipitation on soil water storage was assessed through a decadal analysis. The region of study is characterized by northeast-southwest gradient in accumulated precipitation and east–west gradient in winter long dry sequences. During summer, higher and more frequent precipitations (lower probability of long dry sequences and lower return period of 15 days and severity) were presented whereas the opposite was found in winter. However, the stations located to the west presented the highest probability of long dry sequences with higher severity and lower accumulated precipitation. This result highlights the vulnerability of the agriculture activity in the western stations. Regarding the impact of long dry sequences over soil water storage, the seasonality of evapotranspiration is also involved. The impact is stronger during austral summer because of higher values of evapotranspiration and it is lower during winter, in spite of the higher probability of long sequences. Decadal analysis suggested that soil water storage responds to precipitation amount or frequency depending on the magnitude of the anomalies. In this sense, the impact of precipitation over soil water storage depends on how it is distributed. © 2017 Royal Meteorological Society |l eng | |
| 536 | |a Detalles de la financiación: Universidad de Buenos Aires | ||
| 536 | |a Detalles de la financiación: 212492 | ||
| 536 | |a Detalles de la financiación: Secretaría de Ciencia y Técnica, Universidad de Buenos Aires | ||
| 536 | |a Detalles de la financiación: National Council for Scientific Research | ||
| 536 | |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas, PIP 227 | ||
| 536 | |a Detalles de la financiación: Seventh Framework Programme | ||
| 536 | |a Detalles de la financiación: The authors thank the responsible editor and the reviewers for their valuable suggestions that improved the manuscript. This research was supported by the European Community's Seventh Framework Programme (FP7/2007-2013) under Grant Agreement N? 212492: CLARIS LPB. ?A Europe-South America Network for Climate Change Assessment and Impact Studies in La Plata Basin? and the projects UBACyT (2014?17) 20020130100263BA and PDTS UBA AG5 (2014?17) from the University of Buenos Aires and CONICET PIP 227 from the National Council of Scientific and Technical Research. | ||
| 593 | |a Departamento de Ciencias de la Atmósfera y los Océanos, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Argentina | ||
| 593 | |a Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET), Buenos Aires, Argentina | ||
| 593 | |a Cátedra de Climatología y Fenología Agrícolas, Facultad de Agronomía, Universidad de Buenos Aires, Argentina | ||
| 690 | 1 | 0 | |a DRY SPELLS |
| 690 | 1 | 0 | |a PRECIPITATION DISTRIBUTION |
| 690 | 1 | 0 | |a RETURN PERIOD |
| 690 | 1 | 0 | |a SOIL-ATMOSPHERE INTERACTION |
| 690 | 1 | 0 | |a AGRICULTURE |
| 690 | 1 | 0 | |a DROUGHT |
| 690 | 1 | 0 | |a EVAPOTRANSPIRATION |
| 690 | 1 | 0 | |a PROBABILITY |
| 690 | 1 | 0 | |a REGIONAL PLANNING |
| 690 | 1 | 0 | |a SOIL MOISTURE |
| 690 | 1 | 0 | |a SOILS |
| 690 | 1 | 0 | |a AGRICULTURAL PRODUCTIONS |
| 690 | 1 | 0 | |a DRY SPELLS |
| 690 | 1 | 0 | |a EXTREME WEATHER CONDITIONS |
| 690 | 1 | 0 | |a LOWER PROBABILITIES |
| 690 | 1 | 0 | |a PRECIPITATION DISTRIBUTION |
| 690 | 1 | 0 | |a RETURN PERIODS |
| 690 | 1 | 0 | |a SOIL ATMOSPHERE |
| 690 | 1 | 0 | |a TEMPORAL AND SPATIAL VARIABILITY |
| 690 | 1 | 0 | |a WATER SUPPLY |
| 690 | 1 | 0 | |a ATMOSPHERE-BIOSPHERE INTERACTION |
| 690 | 1 | 0 | |a EVAPOTRANSPIRATION |
| 690 | 1 | 0 | |a PRECIPITATION (CLIMATOLOGY) |
| 690 | 1 | 0 | |a PRECIPITATION ASSESSMENT |
| 690 | 1 | 0 | |a PRECIPITATION INTENSITY |
| 690 | 1 | 0 | |a RETURN PERIOD |
| 690 | 1 | 0 | |a SOIL WATER |
| 690 | 1 | 0 | |a SPATIAL VARIATION |
| 690 | 1 | 0 | |a WATER STORAGE |
| 651 | 4 | |a ARGENTINA | |
| 700 | 1 | |a Penalba, O.C. | |
| 700 | 1 | |a Spescha, L.B. | |
| 700 | 1 | |a Murphy, G.M. | |
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