HIGHLIGHTS
SUMMARY
Global precipitation is primarily dominated by summer monsoon characteristics, which have been found to be highly correlated with the annual cycle of solar insolation, as well as associated with changes in radiative forcing due to increased greenhouse gases (Geen et_al, 2020; Li and Ting, 2017; Trenberth et_al, 2000). Studies have demonstrated that global hydrological cycle becomes stronger in a warmer climate (Held and Soden, 2006), but additional scrutiny is needed to verify hydroclimatic changes under precessional inter-hemispheric seesaw temperature anomalies; with warmer Boreal latitudes and Austral cooling, as characteristics of interglacial stages (Justino . . .
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