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Projecting Climate Change Impacts on Channel Depletion in the Sacramento–San Joaquin Delta of California in the 21st Century

Sohrab Salehi, Seyed Ali Akbar Salehi Neyshabouri (), Andrew Schwarz and Minxue He ()
Additional contact information
Sohrab Salehi: Department of Civil and Environmental Engineering, Tarbiat Modares University, Tehran P.O.Box 14115-111, Iran
Seyed Ali Akbar Salehi Neyshabouri: Department of Civil and Environmental Engineering, Tarbiat Modares University, Tehran P.O.Box 14115-111, Iran
Andrew Schwarz: California Department of Water Resources, Sacramento, CA 95814, USA
Minxue He: California Department of Water Resources, Sacramento, CA 95814, USA

Forecasting, 2024, vol. 6, issue 4, 1-26

Abstract: The Sacramento–San Joaquin Delta (Delta) is a critical hub of California’s statewide water distribution system. Located at the confluence of California’s two largest rivers, the Sacramento River and the San Joaquin River, the Delta features a complex network of braided channels and over a hundred islands, most of which are located below sea level. The Delta’s complex nature and low-lying topography make it a unique hydrological area pertinent to climate change studies. This paper aims to estimate and explore the potential effects of climate change on the hydrological features of the Delta, especially Net Channel Depletion (NCD), which is one of the main contributors to the Net Delta Outflow (NDO). Downscaled CMIP6 General Circulation Model outputs are used to generate plausible future climate data. The Delta Channel Depletion model (DCD) is used to simulate daily hydrological processes for 61 plausible future climate scenarios. Simulation models are applied to the historical period (1930–2014) and projected future periods (2016–2100). A thorough water balance is computed in the DCD simulation model, offering insights into various elements in the hydrological cycle. Key hydrological features such as crop evapotranspiration, seepage, drainage, and runoff are simulated. Potential changes in NCD, calculated as the sum of diversions and seepage minus drainage, are also examined. The study identified a wide range of increases in NCD across all scenarios in the future period relative to the average of the historical period. These increases are projected to vary from 0.3% up to 20%. Moreover, a spatial analysis conducted across diverse regions of the Delta highlights notable variations in depletion across these areas. The results of this research indicate an anticipated increased stress on water resources, necessitating the adoption of innovative strategies to manage extreme events effectively and ensure the sustainability and resilience of water resource management.

Keywords: Sacramento–San Joaquin delta; climate change; deep uncertainty; hydrological simulation; net channel depletion; CMIP6 (search for similar items in EconPapers)
JEL-codes: A1 B4 C0 C1 C2 C3 C4 C5 C8 M0 Q2 Q3 Q4 (search for similar items in EconPapers)
Date: 2024
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