2022
DOI: 10.1016/j.apgeochem.2022.105305
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Subannual-to-biannual-resolved travertine record of Asian Summer Monsoon dynamics in the early Holocene at the eastern margin of Tibetan Plateau

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Cited by 6 publications
(2 citation statements)
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“…The δ 18 O in the travertine exhibits a gradual negative trend toward the deeper layers (Figure 1f), indicating that the amount of local precipitation was larger (Sun & Liu, 2010; Sun et al., 2022). The increase in the rainfall amount leads to the enhancement of groundwater discharge, resulting in a faster spring water flow rate.…”
Section: Resultsmentioning
confidence: 99%
“…The δ 18 O in the travertine exhibits a gradual negative trend toward the deeper layers (Figure 1f), indicating that the amount of local precipitation was larger (Sun & Liu, 2010; Sun et al., 2022). The increase in the rainfall amount leads to the enhancement of groundwater discharge, resulting in a faster spring water flow rate.…”
Section: Resultsmentioning
confidence: 99%
“…The major factors which govern the mechanism of the southwest summer monsoon system include the differential heating of the land mass in the Indian sub-continent and the Indian Ocean, development of a high pressure system over the Indian Ocean, seasonal latitudinal shifting of ITCZ at the Tropic of Cancer, formation of Tibetan trough, Sub-Tropical Westerly Jet Streams (STWJ) and the Tropical Easterly Jet streams (TEJ), and El-Nino Southern Oscillation (ENSO) [33,34]. In South Asia, the southwest summer monsoon system generally initiates with the differential heating and the development of air pressure gradient between the Indian Ocean and the land masses in India and Pakistan.…”
Section: Investigation Of Causes and Characteristics Of Monsoon Extre...mentioning
confidence: 99%