Abstract:It is still unclear how El Niño Southern Oscillation (ENSO), the leading mode of global-scale interannual climate variability, will respond to global warming. The last deglaciation offers natural experimental conditions to observe the behavior of ENSO in a period of abrupt warming and sea level rise. Here we present a record of ENSO-related interannual variability of river discharge in Peru during the last deglaciation (17.3-13 kyr) and the Late Holocene (2.7-1.3 kyr), based on high-resolution records of Titan… Show more
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