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Incorporating decadal climate variability information in the operation and design of water infrastructure

Dados Bibliográficos

ID21697102
AutoresJesper Olsen (0000-0002-4445-5520, Charlottesville Medical Research, autor correspondente), J Rolf Olsen (Charlottesville, VA, USA), Vikram M Mehta (0000-0003-3841-034X, Center for Research on the Changing Earth System (CRCES), Clarksville, MD, USA), Harvey Hill (0000-0003-1980-8678, University of Saskatchewan)
Ano2021
Volume23
FascículoS1
Páginas232-249
Data de publicação2021-12-01
Peer ReviewedSim
Open AccessSim
TipoARTICLE
PeriódicoWater Policy (JOURNAL)
Identificadores do periódicoISSN: 1366-7017 • E-ISSN: 1996-9759
EditoraIWA Publishing (PUBLISHER • GB)
DOI10.2166/wp.2021.267
OpenAlexW4200559447
IdiomaEN
Referências citadas45

The high thermal and mechanical inertia of the oceans results in slow changes in sea surface temperatures (SSTs). Changes in SSTs, in turn, can impact atmospheric circulation including water vapor transport, precipitation, and temperatures throughout the world. The Pacific Decadal Oscillation (PDO), the tropical Atlantic SST gradient variability, and the West Pacific Warm Pool are patterns of natural climate variability that tend to persist over decadal time periods. There are current efforts to produce decadal climate predictions, but there is limited understanding if this information can be used in water resources management. Understanding the current state of decadal climate variability (DCV) phenomena and the probability of persisting in that state may be useful information for water managers. This information could improve forecasts that aid operations and short-term planning for reservoir management, domestic and industrial water supplies, flood risk management, energy production, recreation, inland navigation, and irrigation. If conditions indicate a higher likelihood of drought, reservoir managers could reduce flood storage space and increase storage for conservation purposes. Improved forecasts for irrigation could result in greater efficiencies by shifting crops and rotational crop patterns. The potential benefits of using a forecast must be balanced against the risk of damages if the forecast is wrong. Seasonal forecasts using DCV information could also be used to inform drought triggers. If DCV indices indicate that the climate has a higher probability of dry conditions, drought contingency plans could be triggered earlier. Understanding of DCV phenomena could also improve long-range water resources planning. DCV can manifest itself in relatively short-term hydrologic records as linear trends that complicate hydrologic frequency analysis, which has traditionally assumed that hydrologic records are stationary

Climate change · Climatology · Flood myth · Geography · Meteorology · Pacific decadal oscillation · Precipitation · Sea surface temperature · Water resources · Climate variability and models · Environmental Science · Flood Risk Assessment and Management · Hydrology and Watershed Management Studies · Ecology · Oceanography

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