Abstract

Abstract. In this study, we examine the potential of snow water equivalent data assimilation (DA) using the ensemble Kalman filter (EnKF) to improve seasonal streamflow predictions. There are several goals of this study. First, we aim to examine some empirical aspects of the EnKF, namely the observational uncertainty estimates and the observation transformation operator. Second, we use a newly created ensemble forcing dataset to develop ensemble model states that provide an estimate of model state uncertainty. Third, we examine the impact of varying the observation and model state uncertainty on forecast skill. We use basins from the Pacific Northwest, Rocky Mountains, and California in the western United States with the coupled Snow-17 and Sacramento Soil Moisture Accounting (SAC-SMA) models. We find that most EnKF implementation variations result in improved streamflow prediction, but the methodological choices in the examined components impact predictive performance in a non-uniform way across the basins. Finally, basins with relatively higher calibrated model performance (> 0.80 NSE) without DA generally have lesser improvement with DA, while basins with poorer historical model performance show greater improvements.

Highlights

  • In the snow-dominated watersheds of the western US, spring snowmelt is a major source of runoff (Barnett et al, 2005; Clark and Hay, 2004; Singh and Kumar, 1997; Slater and Clark, 2006)

  • The impacts of the snow water equivalent (SWE) data assimilation (DA) on forecast accuracy can be assessed through verification of post-adjustment simulations using “perfect” future forcing, we demonstrate the performance of SWE DA by initializing seasonal ensemble streamflow prediction (ESP) forecasts for a streamflow forecast product that is widely used in water management, the snowmelt period runoff volume from

  • We note that the ensemble observations of 7-day window can have a larger variance than the 3-month window, and as large as the 1-year window in some cases

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Summary

Introduction

In the snow-dominated watersheds of the western US, spring snowmelt is a major source of runoff (Barnett et al, 2005; Clark and Hay, 2004; Singh and Kumar, 1997; Slater and Clark, 2006) In such basins, the initial conditions of the basin, primarily in the form of snow water equivalent (SWE), drive predictability out to seasonal timescales (Wood et al, 2005; Wood and Lettenmaier, 2008; Mahanama et al 2012; Staudinger and Seibert, 2014; Wood et al, 2016). Spatial interpolation of SWE measurements is typically used

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