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- W2565978098 abstract "We use paleoflood deposits to reconstruct a record of past floods for the Alaknanda-Mandakini Rivers (Garhwal Himalaya), the Indus River (Ladakh, NW Himalaya) and the Brahmaputra River (NE Himalaya). The deposits are characterized by sand-silt couplets, massive sand beds, and from debris flow sediment. The chronology of paleoflood deposits, established by Optically Stimulated Luminescence (OSL) and 14C AMS dating techniques, indicates the following: (i) The Alaknanda-Mandakini Rivers experienced large floods during the wet and warm Medieval Climate Anomaly (MCA); (ii) the Indus River experienced at least 14 large floods during the Holocene climatic optimum, when flood discharges were likely an order of magnitude higher than those of modern floods; and (iii) the Brahmaputra River experienced a megaflood between 8 and 6 ka. Magnetic susceptibility of flood sediments indicates that 10 out of 14 floods on the Indus River originated in the catchments draining the Ladakh Batholith, indicating the potential role of glacial lake outbursts (GLOFs) and/or landslide lake outbursts (LLOFs) in compounding flood magnitudes. Pollen recovered from debris flow deposits located in the headwaters of the Mandakini River showed the presence of warmth-loving trees and marshy taxa, thereby corroborating the finding that floods occurred during relatively warm periods. Collectively, our new data indicate that floods in the Himalaya largely occur during warm and wet climatic phases. Further, the evidence supports the notion that the Indian Summer Monsoon front may have penetrated into the Ladakh area during the Holocene climatic optimum." @default.
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- W2565978098 date "2017-05-01" @default.
- W2565978098 modified "2023-10-10" @default.
- W2565978098 title "Paleofloods records in Himalaya" @default.
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- W2565978098 cites W1972233922 @default.
- W2565978098 cites W1976259730 @default.
- W2565978098 cites W1976382232 @default.
- W2565978098 cites W1978223950 @default.
- W2565978098 cites W1983099128 @default.
- W2565978098 cites W1985036125 @default.
- W2565978098 cites W1989265022 @default.
- W2565978098 cites W1989524258 @default.
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- W2565978098 cites W1992784965 @default.
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- W2565978098 cites W1996862175 @default.
- W2565978098 cites W1998509694 @default.
- W2565978098 cites W2005811687 @default.
- W2565978098 cites W2008726876 @default.
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- W2565978098 cites W2028628075 @default.
- W2565978098 cites W2031599091 @default.
- W2565978098 cites W2037432545 @default.
- W2565978098 cites W2037511507 @default.
- W2565978098 cites W2039196622 @default.
- W2565978098 cites W2040269558 @default.
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- W2565978098 cites W2082784698 @default.
- W2565978098 cites W2085683568 @default.
- W2565978098 cites W2089756799 @default.
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- W2565978098 cites W2092861533 @default.
- W2565978098 cites W2093652715 @default.
- W2565978098 cites W2094089451 @default.
- W2565978098 cites W2094408279 @default.
- W2565978098 cites W2100696460 @default.
- W2565978098 cites W2113888435 @default.
- W2565978098 cites W2117077337 @default.
- W2565978098 cites W2117287198 @default.
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- W2565978098 cites W2150450312 @default.
- W2565978098 cites W2152559568 @default.
- W2565978098 cites W2153043474 @default.
- W2565978098 cites W2162964997 @default.
- W2565978098 cites W2166472004 @default.
- W2565978098 cites W2261600918 @default.
- W2565978098 cites W2399745203 @default.
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- W2565978098 doi "https://doi.org/10.1016/j.geomorph.2016.12.011" @default.
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