2012
DOI: 10.1016/j.quaint.2010.12.009
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Drought area monitoring during the past three decades in Fars province, Iran

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Cited by 44 publications
(16 citation statements)
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“…Then, the aggregated precipitation data for each calendar‐end month follows an individual probability distribution function, which is subsequently transformed to a standard normal distribution. This transformation makes the SPI comparable over temporal and spatial scales and has been widely applied to capture different aspects of droughts (Liu et al, ; McKee et al, ; Nafarzadegan et al, ). Because of the ability to investigate drought severity at different time scales, the SPI is indispensable for quantifying variations in the hydrological response to meteorological droughts (Vicente‐Serrano & Lopez‐Moreno, ).…”
Section: Methodsmentioning
confidence: 99%
“…Then, the aggregated precipitation data for each calendar‐end month follows an individual probability distribution function, which is subsequently transformed to a standard normal distribution. This transformation makes the SPI comparable over temporal and spatial scales and has been widely applied to capture different aspects of droughts (Liu et al, ; McKee et al, ; Nafarzadegan et al, ). Because of the ability to investigate drought severity at different time scales, the SPI is indispensable for quantifying variations in the hydrological response to meteorological droughts (Vicente‐Serrano & Lopez‐Moreno, ).…”
Section: Methodsmentioning
confidence: 99%
“…The study area is in the Fars Province (SE Iran) between 27° 2′ to 31° 42′ N latitudes and 50° 42′ to 55° 36′ E longitudes, with an area of approximately 133,400 km 2 of mainly arid and semi-arid land 27 . It covers 8.1% of Iran and includes 26 cities (Fig.…”
Section: Study Areamentioning
confidence: 99%
“…The SPI and NPI calculation is based only on precipitation deficiency and does not consider other critical variables that may affect drought condition. Due to its robustness and convenience in application, SPI has already been widely used to characterize dry/wet conditions all over the world [17][18][19]. Moreover, it was recommended for meteorological dryness estimation in a recent meeting of the World Meteorological Organization (WMO) [20].…”
Section: Advances In Meteorologymentioning
confidence: 99%