Previously published results suggest that the strength of the SW Indian Monsoon can vary significantly on century- to millenium time scales, an observation
On the eastern side, theBay of Bengalis the largest bay in the world and plays a critical role in the Indian monsoon system, while theAndaman Sea, enclosed by the Andaman and Nicobar Islands, Thailand, and Myanmar, is famous for its stunning islands and vibrant marine ecosystems. ...
The autoconversion and accretion processes are found to be vital for Indian Summer Monsoon (ISM). The map-to-map correlations are examined between observed precipitation and MERRA reanalysis. The pattern correlations connote the fidelity of the MERRA datasets used here. Results of other ...
The variability of the Indian summer monsoon occurs on a wide range of timescales from hourly to orbital. The instrumental record exists, however, over the last 150 years. Thus, the variability of monsoon on the centennial scale has been explored mainly with monsoon proxies and time-slice experi...
Here we show that the Kunlun barrier on the northern Tibetan Plateau [~36°N] delimits Indian Summer Monsoon precipitation during the Holocene. The presence of the barrier relocates the insulation effect 1,000 km further north, allowing a continental low intensity branch of the Indian Summer ...
Using the Regional Atmospheric Modeling System (RAMS) we show that agricultural intensification and irrigation can modify the surface moisture and energy distribution, which alters the boundary layer and regional convergence, mesoscale convection, and precipitation patterns over the Indian monsoon region. Fo...
Millennial-scale variability of Indian summer monsoon constrained by the western Bay of Bengal sediments: Implication from geochemical proxies of sea surfa... YO A,HKBC D,JKCD E,... 被引量: 0发表: 2021年 Millennial-scale variability of Indian summer monsoon constrained by the western Bay of...
The evidence of a southern extension of the East African Rift System and its link with the Southwest Indian Ridge in the mantle gravity map is absent. Similarly, the ongoing breakup of the composite Indo-Australian plate is not manifested. A missing thermal signature in the mantle gravity map ...
D. Indian summer monsoon variability 140–70 thousand years ago based on multi-proxy records from the Bay of Bengal. Quat. Sci. Rev. 279, 107403 (2022). Article Google Scholar Ishikawa, S. & Oda, M. Reconstruction of Indian monsoon variability over the past 230,000 years: planktic ...
40–44, 1 map, 6 ills.] Google Scholar BHAN, Suraj: — Changes in the Course of Yamuna and Their Bearing on the Proto-Historic Cultures of Haryana. Arch. Congr. and Sem. Pap., 1972, pp. 125–128,1 fig. Google Scholar BHAN, Suraj: —Excavations at Mitathal (Hissar) 1968. J....