32 Observations and Modelling of ENSO and Other Aspects of Short-term Climate Variability During the Holocene
Saturday, 26 July 2003
8:00 AM - 12:00 PM
DID SUPPRESSION OF EL NIÑO CAUSE MID-HOLOCENE DROUGHT IN SOUTHWESTERN NORTH AMERICA?
Paper number: 32-7
Program: SYMPOSIA
Time: 10:30 AM – 10:50 AM
Authors
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Roger Y. AndersonUniv New Mexico, Albuquerque, NM
Abstract
Elevation of the water table in Estancia basin presently is regulated by a balance between evaporation from the playas that occupy the blowouts and recharge of aquifers in the adjacent Manzano Mountains. Isotopic analyses of precipitation and groundwater reveal that recharge originates primarily as winter moisture, which is augmented during El Niños and significantly diminished during La Niñas. Thus, the late Holocene rise in the water table, as well as the low water table during the middle Holocene (blowouts and lunettes) may reflect the mid-Holocene suppression of El Niño, followed by its increasing influence during the late Holocene, as suggested by numerical models and recent geologic evidence from South America and Australia.