The Intra‐Seasonal Oscillation of Precipitation δ¹⁸O Over the Asian Equatorial and Monsoon Regions

Abstract

Understanding the spatiotemporal patterns of stable water isotopes in precipitation and vapor is important for the reconstruction of paleoclimate from various isotope archives, large-scale atmospheric circulation, hydrological cycles, and ecology studies. Specifically, unraveling the controls on stable isotopologues of tropical rainfall is critical for the extraction of paleoclimate information from tropical ice core (