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data <strong>and</strong> forecast products that <strong>support</strong><br />

hydrologic <strong>and</strong> water supply forecasting<br />

efforts in the United States. In Section<br />

2.4, we provide a more detailed<br />

discussion of pathways for improving<br />

the skill <strong>and</strong> utility in hydrologic <strong>and</strong><br />

climate forecasts <strong>and</strong> data products.<br />

Section 2.5 contains a brief review<br />

of operational considerations <strong>and</strong> efforts<br />

<strong>to</strong> improve the utility of forecast<br />

<strong>and</strong> data products through efforts <strong>to</strong><br />

improve the forecast evaluation <strong>and</strong><br />

development process. These efforts<br />

include cases in which forecast providers<br />

<strong>and</strong> users have been engaged<br />

in sustained interactions <strong>to</strong> improve<br />

the use <strong>and</strong> utility of forecast <strong>and</strong><br />

data products, <strong>and</strong> have led <strong>to</strong> many<br />

improvements <strong>and</strong> innovations in the<br />

data <strong>and</strong> forecast products generated by national<br />

centers. In recent years, a small number of<br />

water resource agencies have also developed<br />

end-<strong>to</strong>-end forecasting systems (i.e. forecasting<br />

systems that integrate observations <strong>and</strong> forecast<br />

models with decision-<strong>support</strong> <strong>to</strong>ols) that utilize<br />

climate forecasts <strong>to</strong> directly inform hydrologic<br />

<strong>and</strong> water resources forecasts.<br />

2.2 HYDROLOGIC AND WATER<br />

RESOURCES: MONITORING AND<br />

PREDICTION<br />

The uses of hydrologic moni<strong>to</strong>ring <strong>and</strong> prediction<br />

products, <strong>and</strong> specifically those that are<br />

relevant for water, hazard <strong>and</strong> energy management,<br />

vary depending on the forecast lead<br />

time (Figure 2.1). The shortest climate <strong>and</strong><br />

hydrologic lead-time forecasts, from minutes<br />

<strong>to</strong> hours, are applied <strong>to</strong> such uses as warnings<br />

for floods <strong>and</strong> extreme weather, wind power<br />

scheduling, aviation, recreation, <strong>and</strong> wild fire<br />

response management. In contrast, at lead<br />

times of years <strong>to</strong> decades, predictions are used<br />

for strategic planning purposes rather than<br />

operational management of resources. At SI<br />

lead times, climate <strong>and</strong> hydrologic forecast applications<br />

span a wide range that includes the<br />

management of water, fisheries, hydropower<br />

<strong>and</strong> agricultural production, navigation <strong>and</strong><br />

recreation. Table 2.2 lists aspects of forecast<br />

products at these time scales that are relevant<br />

<strong>to</strong> decision makers.<br />

<strong>Decision</strong>-Support Experiments <strong>and</strong> Evaluations <strong>using</strong> Seasonal <strong>to</strong><br />

Interannual Forecasts <strong>and</strong> Observational Data: A Focus on Water Resources<br />

Figure 2.1 The correspondence of climate <strong>and</strong> hydrologic forecast lead time <strong>to</strong> user<br />

sec<strong>to</strong>rs in which forecast benefits are realized (from National Weather Service Hydrology<br />

Research Labora<strong>to</strong>ry). The focus of this Product is on climate <strong>and</strong> hydrologic forecasts with<br />

lead times greater than two weeks <strong>and</strong> up <strong>to</strong> approximately one year.<br />

2.2.1 Prediction Approaches<br />

The primary climate <strong>and</strong> hydrologic prediction<br />

approaches used by operational <strong>and</strong> research<br />

centers fall in<strong>to</strong> four categories: statistical,<br />

dynamical, statistical-dynamical hybrid, <strong>and</strong><br />

consensus. The first three approaches are objective<br />

in the sense that the inputs <strong>and</strong> methods<br />

are formalized, outputs are not modified on an<br />

ad hoc basis, <strong>and</strong> the resulting forecasts are<br />

potentially reproducible by an independent<br />

forecaster <strong>using</strong> the same inputs <strong>and</strong> methods.<br />

The fourth major category of approach, which<br />

might also be termed blended knowledge, requires<br />

subjective weighting of results from the<br />

other approaches. These types of approaches<br />

are discussed in Box 2.2.<br />

Other aspects of dynamical prediction schemes<br />

related <strong>to</strong> model physical <strong>and</strong> computational<br />

structure are important in distinguishing one<br />

model or model version from another. These<br />

aspects are primary indica<strong>to</strong>rs of the sophistication<br />

of an evolving model, relative <strong>to</strong> other<br />

models, but are not of much interest <strong>to</strong> the<br />

forecast user community. Examples include<br />

the degree of coupling of model components,<br />

model vertical resolution, cloud microphysics<br />

package, nature of data assimilation approaches<br />

<strong>and</strong> of the data assimilated, <strong>and</strong> the ensemble<br />

generation scheme, among many other forecast<br />

system features.<br />

Climate <strong>and</strong><br />

hydrologic leadtime<br />

forecasts<br />

range from<br />

minutes <strong>to</strong> years.<br />

33

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