2019
DOI: 10.1007/s00382-019-04889-9
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Dominant modes of winter precipitation variability over Central Southwest Asia and inter-decadal change in the ENSO teleconnection

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Cited by 30 publications
(31 citation statements)
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“…The EA‐WA sector has been previously identified as being a region where precipitation can be forecast with higher skill compared to most places of the globe on the subseasonal time scale (Tippett et al, ; Vigaud et al, ). Enhanced probabilities of above‐normal rainfall in Week 3–4 forecasts (i.e., 15–28 days in advance) for starts during El Niño and MJO Phase 7 are consistent with regional influences from ENSO (Abid et al, ; Alizadeh‐Choobari et al, ; Atif et al, ; Barlow et al, ; Hoell et al, ; Hoell, Barlow, Cannon, & Xu, ; Kang et al, ; Kijazi and Reason, ; Mutai and Ward, ; Nicholson, ; Soltani et al, ; Rana et al, , ) and the MJO (Barlow et al, , ; Hoell et al, ; Hoell, Cannon, & Barlow, ; Mutai and Ward, ; Pohl and Camberlin, , ; Pohl et al, ; Nazemosadat and Ghaedamini, ; Nazemosadat and Shahgholian, ). As noted in the recent review from Barlow et al (), regional droughts have also been related to ENSO (Al Senafi and Anis, ; Athar, ; Barlow et al, ; Donat et al, ; Hoell et al, , , ; Krichak et al, ; Mariotti et al, ; Mariotti, ; Nazemosadat and Ghasemi, ; Niranjan and Ouarda, ; Price et al, ; Syed et al, ; Yin et al, ) and the MJO (Barlow et al, ; Barlow, ; Hoell et al, ; Nazemosadat and Ghaedamini, ; Pourasghar et al, ; Tippett et al, ).…”
Section: Introductionmentioning
confidence: 54%
“…The EA‐WA sector has been previously identified as being a region where precipitation can be forecast with higher skill compared to most places of the globe on the subseasonal time scale (Tippett et al, ; Vigaud et al, ). Enhanced probabilities of above‐normal rainfall in Week 3–4 forecasts (i.e., 15–28 days in advance) for starts during El Niño and MJO Phase 7 are consistent with regional influences from ENSO (Abid et al, ; Alizadeh‐Choobari et al, ; Atif et al, ; Barlow et al, ; Hoell et al, ; Hoell, Barlow, Cannon, & Xu, ; Kang et al, ; Kijazi and Reason, ; Mutai and Ward, ; Nicholson, ; Soltani et al, ; Rana et al, , ) and the MJO (Barlow et al, , ; Hoell et al, ; Hoell, Cannon, & Barlow, ; Mutai and Ward, ; Pohl and Camberlin, , ; Pohl et al, ; Nazemosadat and Ghaedamini, ; Nazemosadat and Shahgholian, ). As noted in the recent review from Barlow et al (), regional droughts have also been related to ENSO (Al Senafi and Anis, ; Athar, ; Barlow et al, ; Donat et al, ; Hoell et al, , , ; Krichak et al, ; Mariotti et al, ; Mariotti, ; Nazemosadat and Ghasemi, ; Niranjan and Ouarda, ; Price et al, ; Syed et al, ; Yin et al, ) and the MJO (Barlow et al, ; Barlow, ; Hoell et al, ; Nazemosadat and Ghaedamini, ; Pourasghar et al, ; Tippett et al, ).…”
Section: Introductionmentioning
confidence: 54%
“…Weakening of the SH encourages disturbances in the weaker subtropical jet, allowing for WWD to propagate toward HMA, increasing precipitation in Central Himalayas (Cohen and Entekhabi, 1999;Wu and Wang, 2002;Cannon et al, 2015). Rana et al (2019) shows that ridging that extends into central Asia and Europe during SH+ blocks eastward propagating westerly storm system, and restricts westerly flow to more southerly latitudes, resulting in increased precipitation in the southern region of CSWA. Table 1 indicates that Karakoram and Pamir ARs are significantly more frequent during SH-compared to neutral.…”
Section: Climate Modulationmentioning
confidence: 99%
“…During the warm phase of ENSO, when the tropical oceans are warmer than usual, anomalous upper-level convergence over southern Asia has been shown to intensify WWDs (Yadav et al, 2009;Thapa et al, 2018). (Rana et al, 2019) explains that increased precipitation in Central Southwest Asia (CSWA) during winter season El Niño years is mainly attributed to a deepened trough over CSWA with cyclonic circulation that enhances southwesterly flow and moist air advection from the Indian Ocean basin into CSWA. Guan and Waliser (2015) found that El Niño conditions slightly increase NDJFM AR frequency in southwest and southern Asia but has no considerable impact on precipitation.…”
Section: Climate Modulationmentioning
confidence: 99%
“…The average response of precipitation to El Niño and La Niña phases of ENSO is investigated in several studies (Barlow et al ., 2002; Nazemosadat and Ghasemi, 2004; Hoell et al ., 2017a; Alizadeh‐Choobari et al ., 2018). A consistent finding between previous studies is that wet and dry conditions are accompanied respectively by El Niño and La Niña (Nazemosadat and Ghasemi, 2004; Barlow et al ., 2016; Rana et al ., 2017, 2019; Hoell et al ., 2017a, 2017b, 2018; Alizadeh‐Choobari et al ., 2018). The range of response is reported by Hoell et al .…”
Section: Introductionmentioning
confidence: 99%
“…The first leading mode of winter precipitation (EOF‐1) is significantly linked to ENSO characterized by a mono‐sign pattern according to findings by Rana et al . (2019). Simulations based on a large ensemble of atmospheric models (three models, 42 members) forced by 1901–2012 time varying boundary conditions show the association of wet years with El Niño throughout the whole period and exceptionally dry conditions with La Niña after 1970 (Hoell et al ., 2017a).…”
Section: Introductionmentioning
confidence: 99%