L. Edwards, 2015: Trends and oscillations in the Indian summer monsoon rainfall over the last two millennia. Nat. Commun., 6, 6309, doi:10.1038/ncomms7309.Sinha A. et al. . Trends and oscillations in the Indian summer monsoon rainfall over the last two millennia . Nat. Commun. 6 , ...
Weakening of Indian summer monsoon rainfall (ISMR) is traditionally linked with large-scale perturbations and circulations. However, the impacts of local changes in land use and land cover (LULC) on ISMR have yet to be explored. Here, we analyzed this to
indiaclimate-modelcmip6climate-changecdomonsoon UpdatedApr 1, 2021 Python astvd3/Monsoon-Prediction-Model Star4 A supervised Learning approach to find the trends on which the monsoon rainfall depends and its prediction. predictiontrendsmonsoonmonsoon-prediction-model ...
Fig. 2. Sub-regions of India: Northwest (NW), Central north (CN), Northeast (NE), West Central (WC) and Peninsular (Pen). Retrieve from http://www.monsoondata.org/hist/region.html. 3. Characteristic of the sea ice extent in the Indian Ocean sector and Indian rainfall 3.1. Sea ice...
For summer monsoon rainfall purpose India is divided into 35 subdivisions. The daily rainfall series of one such subdivision (Konkan) has been analysed using the phase space approach. Fifteen years (1959–1973) of daily rainfall data have been utilised in this study. The analysis shows that the...
Meanwhile, cold SST anomalies and suppressed convection in the equatorial western Pacific lead to reduced summer monsoon rainfall over the East Asian region (B. Wang et al., 2000; R. Zhang et al., 1996). On average, this negative correlation between the ASM and ENSO is reflected in 20th-...
The rainfall delivered by the Indian summer monsoon (ISM) contributes to about 80% of the total precipitation in the region around the northern Indian Ocean (including India and Myanmar) (Subash and Sikka, 2014), and the ISM is characterized by complex climate dynamics in terms of rainfall dis...
wind and rainfall patterns, the characteristics and behavior of monsoons vary from region to region. The South Asian monsoon, for example, is particularly strong as the Himalayas and Tibetan-Iranian Plateau prevent dry air from the north flowing to the humid monsoon region in India and southern ...
During the 'break' period, the axis of the MT shifts north of our site, resulting in dry air intrusions of westerly winds into northwest and central-north India, which tend to suppress rainfall through decrease of convective instability and depletion of parcel buoyancy23,24. In summary, the ...
Rainfall over northeast (NE) and North India (EI) has been modulated by ENSO-induced SSTA and MSLA over SWIO, thus effecting the total AISMR magnitude. The ENSO-induced changes in heat capacitance (SSTA and MSLA) over SWIO during antecedent months has less impact on west coast of India,...