NSF Award
2303352
The specific research effort for this project involves providing proxy-based global estimates of the spatiotemporal changes in temperature and hydroclimate after large volcanic eruptions. A global picture of proxy-estimated climate responses to volcanism is now possible because of new paleoclimate data assimilation products, which may provide new insights into how volcanoes influence changes in surface temperatures, hydroclimate, and climate dynamics. <br/><br/>The ultimate aim of the project is to quantify risks and improve societal preparedness for climatic variations influenced by large volcanic eruptions.<br/><br/>The research team intends to achieve the project’s research goals by assessing the temporal persistence of responses across multiple paleoclimate data assimilation outputs and ground-truth the estimates against other state-of-the-art proxy reconstructions and documentary evidence. The researchers will also characterize how dynamic climate responses are manifest in reconstructed sea-surface temperature and atmospheric pressure indices, as well as the positioning of the Intertropical Convergence Zone (ITCZ). All of these responses will be assessed seasonally and in terms of eruption latitudes. The proxy-based estimates will in turn be compared to an ensemble of Common Era simulations to characterize the dynamical responses to volcanic eruptions and understand associated uncertainties in the proxy-based products, volcanic forcing estimates, and the coupled climate models.<br/><br/>The potential Broader Impacts include training two graduate students, hosting an annual workshop event for undergraduates aimed at encouraging careers in science, and recruiting women and underrepresented minorities through the AGU Bridge Program.<br/><br/>This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.
