2021
DOI: 10.1016/j.jastp.2021.105705
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Indian summer monsoon variability over North-East India: Impact of ENSO and IOD

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Cited by 10 publications
(4 citation statements)
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“…It has been observed [54] that another important oceanic atmospheric parameter affecting drought is the Indian Ocean Dipole (IOD), which is a climate mode that describes the fluctuations in sea surface temperatures in the Indian Ocean. During positive IOD events, the western Indian Ocean becomes warmer than the eastern Indian Ocean, resulting in changes in atmospheric circulation that can impact rainfall patterns in regions such as East Africa, Southeast Asia [55,56], and Australia [57].…”
Section: Climatological Parametersmentioning
confidence: 99%
“…It has been observed [54] that another important oceanic atmospheric parameter affecting drought is the Indian Ocean Dipole (IOD), which is a climate mode that describes the fluctuations in sea surface temperatures in the Indian Ocean. During positive IOD events, the western Indian Ocean becomes warmer than the eastern Indian Ocean, resulting in changes in atmospheric circulation that can impact rainfall patterns in regions such as East Africa, Southeast Asia [55,56], and Australia [57].…”
Section: Climatological Parametersmentioning
confidence: 99%
“…Notably, the order of influence of the deeply uncertain factors on strategy failure is found to be the same across all strategies: amplitude of inflows to the donor and recipient basins, mean inflows to the donor and recipient basins, standard deviation of inflows to the donor and recipient basins and demands in the donor basin. Climate models struggle to reproduce the complex spatio‐temporal patterns of the Indian Summer Monsoon (Kodra et al., 2012; Konduru & Takahashi, 2020; Saha et al., 2021), but understanding potential future river flows is crucial to understanding potential strategy failure. Our analysis suggests an urgent need to focus on understanding the potential temporal dynamics of future hydro‐climatology of this region given its significantly important role in influencing strategy failure.…”
Section: Resultsmentioning
confidence: 99%
“…These indicators include (1) internal dynamics such as atmospheric circulations that exhibit interannual variability, combined effects of dynamic instabilities (synoptic scale disturbances), a nonlinear interaction among various scales of motion, thermal, and orographic forcing tropical and extratropical interactions, and (2) the influence of global surface boundary conditions such as soil moisture, sea ice, snow cover, and sea surface temperature (SST), which can be assessed using various indices [6,44], i.e., El Nino Southern Oscillation (ENSO), the Indian Ocean Dipole (IOD), the North Atlantic Oscillation (NAO), and the Pacific Decadal Oscillation (PDO). These indicators are the primary factors influencing the interannual variation of the southwest monsoon [54][55][56]. Figure 6a…”
Section: Inter Annual Variability Of Monsoon Rainfallmentioning
confidence: 99%