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G.M. Ariful Islam

Researcher at Chinese Academy of Sciences

Publications -  6
Citations -  68

G.M. Ariful Islam is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Monsoon & Holocene. The author has an hindex of 3, co-authored 5 publications receiving 38 citations.

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Detection of changes and trends in climatic variables in Bangladesh during 1988-2017.

TL;DR: The trend patterns of Tmax, Tmin, and MTR reveal that most of the regions of the country have been colder during winter and hotter during the monsoon, while the wind speed has decreased significantly all over the country and decreased by a higher rate in the north-western (NW) region.
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Modern alluvial pollen distribution in Ganges–Brahmaputra–Meghna (GBM) floodplain and its paleoenvironmental significance

TL;DR: In this article, the main characteristics of modern alluvial pollen distributions and its relationship with corresponding vegetation and climate were determined from 47 sediment samples collected from Ganga-Brahmaputra-Meghna (GBM) riverbed, and a palynological analysis was carried out.
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The present-day atmospheric dust deposition process in the South China Sea

TL;DR: In this paper, the authors investigated the grain size distribution, depositional flux, and features revealed by scanning electron microscopy, combined with 5-day back trajectories to indicate the present-day dust deposition process for the first time.
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The Dust Deposition Process and Biogeochemical Impacts in the Northern South China Sea

TL;DR: In this article, a total of 147 aerosols samples were collected near the northern South China Sea (SCS) coast between 13 February, 2016, and 12 February, 2017, have been investigated for the grain size distribution, depositional flux, ten-day back trajectories, clusters analysis, combining with primary productivity (Chlorophyll-a concentration) to indicate the present-day dust deposition process and biogeochemical impacts in the northern SCS on the first time.
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Variable Kuroshio Current intrusion into the northern South China Sea over the last 7.3 kyr

TL;DR: In this article, the authors report high-resolution sea surface temperature (SST) and δ18Osw (as a proxy for sea surface salinity, SSS) records based on paired Mg/Ca ratios and analysis of the planktonic foraminifera Globigerinoides ruber combined the Pulleniatina obliquiloculata and G. ruber ratios from core 05E306 (22°0.06′−N, 118°59.64′−E; water depth = 1440 m) in the northern