Extreme changes in stable hydrogen isotopes and precipitation characteristics in a landfalling Pacific storm

With a new automated precipitation collector we measured a remarkable decrease of 51‰ in the hydrogen isotope ratio (δ 2H) of precipitation over a 60-minute period during the landfall of an extratropical cyclone along the California coast on 21 March 2005. The rapid drop in δ 2H occurred as precipitation generation transitioned from a shallow to a much deeper cloud layer, in accord with synoptic-scale ascent and deep “seeder-feeder” precipitation. Such unexpected δ 2H variations can substantially impact widely used isotope-hydrograph methods. From extreme δ 2H values of −26 and −78‰, we calculate precipitation temperatures of 9.7 and −4.2°C using an adiabatic condensation isotope model, in good agreement with temperatures estimated [...]