Freshwater flow to the San Francisco Bay‐Delta estuary over nine decades (Part 1): Trend evaluation. Issue 14 (25th May 2017)

• Record Type: Journal Article
• Authors: Hutton, Paul H.; Rath, John S.; Roy, Sujoy B.
• Is Part Of: Hydrological processes. Volume 31:Issue 14(2017)
• Page Start: 2500
• Page End: 2515
• Publication Date: 2017-05-25
• Subjects: Central Valley -- Delta outflow -- Mann–Kendall -- trend analysis -- unimpaired flows; Hydrology -- Periodicals; Hydrology -- Research -- Periodicals; Hydrologic models -- Periodicals; Hydrological forecasting -- Periodicals; 631.432
• DOI: 10.1002/hyp.11201
• Languages: English
• ISSNs: 0885-6087

Abstract

Abstract: The San Francisco Bay‐Delta estuary and its upstream watershed have been highly modified since exploration and settlement by Europeans in the mid‐18th century. Although these hydrologic alterations supported the growth of California's economy to the eighth largest in the world, they have been accompanied by significant declines in native aquatic species and subsequent efforts to reverse these declines through flow management. To inform ongoing deliberations on management of freshwater flows to the estuary, we examined a recent nine‐decade hydrologic record to evaluate seasonal and annual trends in reported Delta outflow. Statistically significant trends were observed in seasonal outflows, with decreasing trends observed in 4 months (February, April, May, and November) and increasing trends observed in 2 months (July and August). Trend significance in early‐to‐mid autumn (September and October) is ambiguous due to uncertainty associated with in‐Delta agricultural water use. In spite of increasing water use over the period examined, we found no statistically significant annual trend in Delta outflow, a result likely due to large inter‐annual variability. Linkages between outflow trends and changes in upstream flows and coincident developments such as reservoir construction and operation, out‐of‐basin imports and exports, and expansion of irrigated agriculture are discussed. To eliminate inter‐annual variability as a factor, change attribution is explored using modelled flows and fixed climatology in a companion paper.