2020
DOI: 10.1007/s00703-020-00734-5
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A review on the Indian summer monsoon rainfall, variability and its association with ENSO and IOD

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Cited by 126 publications
(78 citation statements)
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“…The IOD phenomenon has been considered as an important mode of climate variability in the tropics (Behera et al ., 2006) and it is also an important modulator of the variability of ISMR (Ashok et al ., 2004). A positive (negative) IOD event is characterized by enhanced (suppressed) rainfall in the Indian region (Ashok et al ., 2001; Hrudya et al ., 2020). It can also modulate the number of rain events in central India by forming a convergence zone over the region through the anomalous moisture transport from the southeastern equatorial Indian Ocean to the Bay of Bengal (Ajayamohan and Rao, 2008).…”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation
“…The IOD phenomenon has been considered as an important mode of climate variability in the tropics (Behera et al ., 2006) and it is also an important modulator of the variability of ISMR (Ashok et al ., 2004). A positive (negative) IOD event is characterized by enhanced (suppressed) rainfall in the Indian region (Ashok et al ., 2001; Hrudya et al ., 2020). It can also modulate the number of rain events in central India by forming a convergence zone over the region through the anomalous moisture transport from the southeastern equatorial Indian Ocean to the Bay of Bengal (Ajayamohan and Rao, 2008).…”
Section: Introductionmentioning
confidence: 99%
“…Apart from the Indian region, the IOD produces impact on several other tropical regions such as Europe, North and South America, South Africa, and so on (Saji and Yamagata, 2003; Preethi et al ., 2015). After the discovery of IOD, several studies were carried out to understand its characteristics and impact on ISMR (Ashok et al ., 2001, 2004; Vinayachandran et al ., 2002; Yamagata et al ., 2004; Behera et al ., 2006; Ashok and Saji, 2007; Francis et al ., 2007; Luo et al ., 2010; Du et al ., 2013; Doi et al ., 2017; Behera and Ratnam, 2018; Lu et al ., 2018; Hrudya et al ., 2020). It was well established that the frequency and strength of positive IOD has increased in recent decades (Abram et al ., 2008), and also the IOD‐ISMR relationship has strengthened (Ashok et al ., 2001, 2004; Ummenhofer et al ., 2011; Krishnaswami et al ., 2014).…”
Section: Introductionmentioning
confidence: 99%
“…During La Niña/El Niño events, the southeast to southwest Pacific Ocean temperature difference increases/decreases, which generally strengthens/weakens the Walker circulation and the trade winds. With the higher/lower ocean temperatures, Southeast Asia (partially including the LMRB) experiences more/less evaporation and clouds, and consequently more/less precipitation (e.g., Cherchi & Navarra, 2013; Hrudya et al, 2020; Juneng & Tangang, 2005; Räsänen et al, 2016; Räsänen & Kummu, 2013). During La Niña/El Niño events, the temperatures over the Arabian Sea, Indian Ocean, and the Bay of Bengal also remain cooler/warmer than normal.…”
Section: Discussionmentioning
confidence: 99%
“…While fluctuations in the ENSO are relatively influential in the context of global climate fluctuations, the IOD is known to account for approximately 12% of Indian Ocean sea surface temperature fluctuations, which mainly affect countries adjacent to the Indian Ocean [ 20 , 21 ]. Variation in the ENSO and IOD can cause severe flooding and droughts around the world through atmospheric remote connections [ 7 , 22 ]. In particular, South and Southeast Asian regions, which are located in areas impacted by fluctuations in both the ENSO and IOD, are greatly affected by the climate.…”
Section: Discussionmentioning
confidence: 99%