A009-0010
High-Resolution Detection and Attribution for Extreme Precipitation over the Contiguous United States

Monday, 7 December 2020
Poster
Mark Daniel Risser, Lawrence Berkeley National Laboratory, Climate and Ecosystem Sciences Division, Berkeley, CA, United States, Michael F Wehner, Lawrence Berkeley National Laboratory, Berkeley, CA, United States, John P O'Brien, National Center for Atmospheric Research, Boulder, United States, Christina M Patricola, Iowa State University, Geological & Atmospheric Sciences, Ames, IA, United States, Travis Allen O'Brien, Lawrence Berkeley National Lab, Climate & Ecosystem Sciences Division, Berkeley, CA, United States, William Drew Collins, Berkeley Lab and UC Berkeley, Berkeley, CA, United States, Christopher J Paciorek, University of California, Berkeley, CA, United States and Huanping Huang, Dartmouth College, Department of Earth Sciences, Hanover, NH, United States
Abstract:
While various studies seek to quantify the anthropogenic influence on extreme precipitation in the historical record, there is a need for improved understanding of the (at times) conflicting conclusions on the presence of human-induced climate change on extreme precipitation. Here, we introduce a single framework for characterizing the historical signal (anthropogenic forcing) and noise (natural variability) in seasonal extreme precipitation over the last 120 years. An important aspect of our analysis is that we simultaneously isolate the individual effects of seven modes of climate variability while explicitly controlling for joint inter-mode relationships; furthermore, we utilize a spatial statistical analysis to translate trends from stations to a high-resolution grid. We find that (consistent with related work) the frequency of seasonal extreme precipitation is generally increasing for CONUS overall, but there are important local deviations from this trend. At a high resolution, we are able to isolate and detect a human influence on seasonal extremes in DJF and SON in spite of extremely large background variability. Finally, we use our framework to explain conflicting trends in extreme precipitation depending on the time period chosen for calculating trends.