2019
DOI: 10.1016/j.jhydrol.2019.124102
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Propagation dynamics from meteorological to groundwater drought and their possible influence factors

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Cited by 146 publications
(73 citation statements)
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“…During 2007–2013, the phase arrows are less than 30°, indicating that the change of SPI3 leaded SRI1 for less than 1 month. That may be due to other factors interfering with the DPT (Han et al., 2019; S. Z. Huang et al., 2015). Although hydrological drought in subregion Ⅱ had no significant periodic characteristics, there was still a close relationship between meteorological drought and hydrologic drought at the time scale of 6–14 months (1981–1983), 10–16 months (1985–1987), 6–14 months (1988–1990), 6–16 months (1991–1994), 28–32 months (1994–1998), 20–28 months (2007–2012), and 16–20 months (2014–2017) (Figure 9b).…”
Section: Resultsmentioning
confidence: 99%
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“…During 2007–2013, the phase arrows are less than 30°, indicating that the change of SPI3 leaded SRI1 for less than 1 month. That may be due to other factors interfering with the DPT (Han et al., 2019; S. Z. Huang et al., 2015). Although hydrological drought in subregion Ⅱ had no significant periodic characteristics, there was still a close relationship between meteorological drought and hydrologic drought at the time scale of 6–14 months (1981–1983), 10–16 months (1985–1987), 6–14 months (1988–1990), 6–16 months (1991–1994), 28–32 months (1994–1998), 20–28 months (2007–2012), and 16–20 months (2014–2017) (Figure 9b).…”
Section: Resultsmentioning
confidence: 99%
“…During 2007-2013, the phase arrows are less than 30°, indicating that the change of SPI3 leaded SRI1 for less than 1 month. That may be due to other factors interfering with the DPT (Han et al, 2019;S. Z. Huang et al, 2015).…”
Section: Xwt Analysis Of Spim and Sri1mentioning
confidence: 99%
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“…In addition, atmospheric circulation patterns such as the Arctic Oscillation (AO), the El Niño-Southern Oscillation (ENSO), and the Pacific Decadal Oscillation (PDO), and sunspots, are highly related to regional and local climates. They have been shown to affect global water vapor transport and redistribution (Huang et al 2017), and temperature fluctuations (Horton et al 2015), which thus affect local climate and vegetation growth (Cho et al 2014;Li et al 2015;Han et al 2019a). Dillon and Rundel (1990) studied the response of vegetation in the African desert in the 1982-1983 ENSO and found that vegetation dynamics was closely related to the event.…”
Section: Introductionmentioning
confidence: 99%