2014
DOI: 10.5194/isprsarchives-xl-8-89-2014
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Integrating effective drought index (EDI) and remote sensing derived parameters for agricultural drought assessment and prediction in Bundelkhand region of India

Abstract: ABSTRACT:Drought is an extreme condition due to moisture deficiency and has adverse effect on society. Agricultural drought occurs when restraining soil moisture produces serious crop stress and affects the crop productivity. The soil moisture regime of rain-fed agriculture and irrigated agriculture behaves differently on both temporal and spatial scale, which means the impact of meteorologically and/or hydrological induced agriculture drought will be different in rain-fed and irrigated areas. However, there i… Show more

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Cited by 5 publications
(3 citation statements)
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“…The SPI measures moisture to quantify the precipitation deficit for multiple time scales at any one location and reflects the impact of drought on a range of meteorological, agricultural and hydrological applications (Marimon 2016;Degefu and Bewket 2015;Loukas and Vasiliades 2004). The SPI can be calculated at various timescales for any set of successive months of 1-month up to 72-months that one wishes to detect and to illustrate the effect of drought (Viste et al 2013;Stagge et al 2015;Padhee et al 2014;Beth and Brown 2003;AghaKouchak and Nakhjiri 2012). But statistically, 1-24 months is the best practice range of application (Guttman 1999).…”
Section: Drought Quantification: the Standardized Precipitation Indexmentioning
confidence: 99%
“…The SPI measures moisture to quantify the precipitation deficit for multiple time scales at any one location and reflects the impact of drought on a range of meteorological, agricultural and hydrological applications (Marimon 2016;Degefu and Bewket 2015;Loukas and Vasiliades 2004). The SPI can be calculated at various timescales for any set of successive months of 1-month up to 72-months that one wishes to detect and to illustrate the effect of drought (Viste et al 2013;Stagge et al 2015;Padhee et al 2014;Beth and Brown 2003;AghaKouchak and Nakhjiri 2012). But statistically, 1-24 months is the best practice range of application (Guttman 1999).…”
Section: Drought Quantification: the Standardized Precipitation Indexmentioning
confidence: 99%
“…Where geospatial approach is beneficial because it offers an analytical tool for analysing drought in a better way. Several studies have been done earlier for identification and characterisation of drought for the Indian region and other parts of the world (Aswathi et al 2018;Barker et al 2016;Chouhan et al 2017;Das et al 2020;Edossa et al 2010;Hisdal and Tallaksen 2003;Padhee et al 2014Padhee et al , 2017Khatiwada and Pandey 2019;Mishra 2020;Nikam et al 2020;Thomas et al 2015;Tigkas et al 2012) using standardised indices such as Standardised Precipitation Index (SPI) and Standardised Streamflow Index (SSI).…”
Section: Introductionmentioning
confidence: 99%
“…Various traits of drought propagation have indicated a lag between meteorological, soil moisture (Van Loon and Van Lanen 2012;Padhee et al 2014Padhee et al , 2017 and hydrological deficits. Many times hydrological droughts last for longer time periods than meteorological drought and agricultural (or soil moisture) droughts (Hisdal and Tallaksen 2003) and that the meteorological droughts are attenuated when storage is high at the time of its onset (Van Loon and Van Lanen 2012;Wang et al 2021).…”
Section: Introductionmentioning
confidence: 99%