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Sara Sanchez
University of Colorado at BoulderMeeting roles in:
Deglacial Changes in the Northern Hemisphere Atmospheric Circulation Recorded by Tehuantepec Gap Wind Upwelling
Paleoclimate data assimilation of coral δ18O indicates intensification of hydrological cycle over the 20th century
Stationarity of Indo-Pacific basin interactions across past and future climates
ENSO-driven hydrological variability in the tropical Pacific – sea surface salinity and oxygen isotope observations versus models
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