Abstract

This work surveys the performance of several empirical models, all recalibrated to a common data set, that were developed over the past 25 years to relate freshwater flow and salinity in the San Francisco Estuary (estuary). The estuary’s salinity regime—broadly regulated to meet urban, agricultural, and ecosystem beneficial uses—is managed in spring and certain fall months to meet ecosystem objectives by controlling the 2 parts per thousand bottom salinity isohaline position (referred to as X2). We tested five empirical models for accuracy, mean, and transient behavior. We included a sixth model, employing a machine learning framework and variables other than outflow, in this survey to compare fitting skill, but did not subject it to the full suite of tests applied to the other five empirical models. Model performance was observed to vary with hydrology, year, and season, and in some cases exhibited unique limitations as a result of mathematical formulation. However, no single model formulation was found to be consistently superior across a wide range of tests and applications. One test revealed that the models performed equally well when recalibrated to a uniformly perturbed input time-series. Thus, while the models may be used to identify anomalies or seasonal biases (the latter being the subject of a companion paper), their use as inverse models to infer freshwater outflow to the estuary from salinity observations is not expected to improve upon the absolute accuracy of existing outflow estimates. This survey suggests that, for analyses that span a long hydrologic record, an ensemble approach—rather than the use of any individual model on its own—may be preferable to exploit the strengths of individual models.

Highlights

  • Salinity intrusion in estuarine and deltaic waters is a natural phenomenon, in developed watersheds the extent and timing can be heavily influenced by freshwater withdrawals and upstream water management and use

  • When X2 is estimated from observed data at fixed locations, the value is computed by interpolation; a standardized interpolation methodology has not been identified within the scientific community, and the stations vary with respect to their representativeness laterally across the estuary

  • The methods used in this survey of X2 isohaline empirical models of the estuary were founded on the development and assembly of outflow and salinity data sets spanning nearly a century (WYs 1922 through 2017), and recalibration of the empirical models described above to a common period

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Summary

Introduction

Salinity intrusion in estuarine and deltaic waters is a natural phenomenon, in developed watersheds the extent and timing can be heavily influenced by freshwater withdrawals and upstream water management and use. VOLUME 19, ISSUE 4, ARTICLE 3 adversely affect native estuarine ecosystems as well as human uses of freshwater in proximity to estuaries and has been subject to study and management in many parts of the world (Sklar and Browder 1998; Murray Darling Basin Ministerial Council 1999; Reinert and Peterson 2008; Fernández-Delgado et al 2007). This is true in California, with its relatively dry and variable (both intra- and interannually) Mediterranean climate. X2 is defined as the position of the 2.64 milliSiemens per cm (mS cm–1) surface isohaline (CSWRCB 2000)

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