This paper introduces a novel framework for a process-informed, differential assessment of credibility across various spatial and point-based downscaling methodologies, including both complex and simple statistical approaches, as well as dynamical downscaling. The methods assessed include a convolutional neural network (CNN), the locally constructed analog method (LOCA), the statistical downscaling model (SDSM), quantile delta mapping (QDM), simple spatial interpolation plus bias correction, the Regional Climate Model (RegCM) and the Weather Research and Forecasting Model (WRF). For proof of concept of our framework, our study focuses specifically on the physical consistency of wet days in a location in the southern US Great Plains. We find that all downscaling methods perform credibly when the parent global climate model (GCM) performs credibly. However, complex statistical methods like CNN, LOCA, and SDSM exacerbate inaccuracies when the GCM outputs are unreliable, performing worse as the GCM’s credibility decreases. On the other hand, simpler methods like QDM and bias-correction generally retain the GCM’s credibility. Notably, dynamical models can mitigate issues inherited from GCMs, enhancing the overall credibility of the data. These results highlight the need for careful evaluation of complex statistical downscaling techniques and suggest that further scrutiny is warranted. Finally, we summarize our process-informed analysis of credibility into a relative credibility metric, offering a quantifiable way to compare different downscaling approaches, and we provide guidance on the application and expansion of our framework for future research.

Alan M. Rhoades

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The 1997 New Year’s flood event was the most costly in California’s history. This compound extreme event was driven by a category 5 atmospheric river that led to widespread snowmelt. Extreme precipitation, snowmelt, and saturated soils produced heavy runoff causing widespread inundation in the Sacramento Valley. This study recreates the 1997 flood using the Regionally Refined Mesh capabilities of the Energy Exascale Earth System Model (RRM-E3SM) under prescribed ocean conditions. Understanding the processes causing extreme events inform practical efforts to anticipate and prepare for such events in the future, and also provides a rich context to evaluate model skill in representing extremes. Three California-focused RRM grids, with horizontal resolution refinement of 14km down to 3.5km, and six forecast lead times, 28 December 1996 at 00Z through 30 December 1996 at 12Z, are assessed for their ability to recreate the 1997 flood. Planetary to synoptic scale atmospheric circulations and integrated vapor transport are weakly influenced by horizontal resolution refinement over California. Topography and mesoscale circulations, such as the Sierra barrier jet, are prominently influenced by horizontal resolution. The finest resolution RRM-E3SM simulation best represents storm total precipitation and storm duration snowpack changes. Traditional time-series and causal analysis frameworks are used to examine runoff sensitivities state-wide and above major reservoirs. These frameworks show that horizontal resolution plays a more prominent role in shaping reservoir inflows, namely the magnitude and time-series shape, than forecast lead time, 2-to-4 days prior to the 1997 flood onset.