Abstract

Abstract 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.

Highlights

  • Climate is a major driver of hydrologic conditions and varies on multiple time scales from sub-seasonal to decadal and centennial

  • The phases of the Pacific Decadal Oscillation (PDO), TAG, and West Pacific Warm Pool (WPWP) tend to persist over decadal time periods

  • During the past couple of decades, empirical data analysis and climate model simulations have improved the understanding of decadal climate variability (DCV)

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Summary

INTRODUCTION

Climate is a major driver of hydrologic conditions and varies on multiple time scales from sub-seasonal to decadal and centennial. This paper focuses on decadal climate variability (DCV) and its impacts on water resources. DCV and its hydrologic effects confound the attribution of observed anomalies to natural variability or climate change, which can confuse adaptation planning in the short, medium, and long term. It is very important to understand and, if possible, predict DCV effects on impacted sectors to inform water resources management in the short, medium, and long term. The examples illustrated here are from the United States, they are potentially applicable to other parts of the world

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