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<strong>and</strong> communities vulnerable <strong>to</strong> wildfire in the<br />

western United States (Kitzberger et al., 2007).<br />

Aside from the immediate impacts of a wildfire<br />

(e.g., destruction of biomass, substantial altering<br />

of ecosystem function), the increased likelihood<br />

of high sediment deposition in streams <strong>and</strong><br />

flash flood events can present post-fire management<br />

challenges including impacts <strong>to</strong> soil<br />

stability on slopes <strong>and</strong> mudslides (e.g., Bisson<br />

et al., 2003). While the highly complex nature<br />

<strong>and</strong> substantially different ecologies of fireprone<br />

systems precludes one-size-fits-all fire<br />

management approaches (Noss et al., 2006),<br />

climate information can help managers plan for<br />

fire risk in the context of watershed management<br />

<strong>and</strong> post-fire impacts, including impacts<br />

on water resources. One danger is inundation<br />

of water s<strong>to</strong>rage <strong>and</strong> treatment facilities with<br />

sediment-rich water, creating potential for<br />

significant expense for pre-treatment of water<br />

or for facilities repair. Post-fire runoff can also<br />

raise nitrate concentrations <strong>to</strong> levels that exceed<br />

the federal drinking water st<strong>and</strong>ard (Meixner<br />

<strong>and</strong> Wohlgemuth, 2004).<br />

Work by Kuyumjian (2004), suggests that<br />

coordination among fire specialists, hydrologists,<br />

climate specialists, <strong>and</strong> municipal water<br />

managers may produce useful warnings <strong>to</strong><br />

downstream water treatment facilities about<br />

significant ash- <strong>and</strong> sediment-laden flows. For<br />

example, in the wake of the 2000 Cerro Gr<strong>and</strong>e<br />

fire in the vicinity of Los Alamos, New Mexico,<br />

catastrophic floods were feared, due <strong>to</strong> the<br />

fact that 40 percent of annual precipitation in<br />

northern New Mexico is produced by summer<br />

monsoon thunders<strong>to</strong>rms (e.g., Earles et al.,<br />

2004). Concern about water quality <strong>and</strong> about<br />

the potential for contaminants carried by flood<br />

waters from the grounds of Los Alamos Nuclear<br />

Labora<strong>to</strong>ry <strong>to</strong> enter water supplies prompted<br />

a multi-year water quality moni<strong>to</strong>ring effort<br />

(Gallaher <strong>and</strong> Koch, 2004). In the wake of the<br />

2002 Bullock Fire <strong>and</strong> 2003 Aspen Fire in the<br />

Santa Catalina Mountains adjacent <strong>to</strong> Tucson,<br />

Arizona, heavy rainfall produced floods that<br />

destroyed homes <strong>and</strong> caused one death in Canada<br />

del Oro Wash in 2003 (Ekwurzel, 2004),<br />

destroyed structures in the highly popular<br />

Sabino Canyon recreation area <strong>and</strong> deposited<br />

high sediment loads in Sabino Creek in 2003<br />

(Desilets et al., 2006). A flood in 2006 wrought<br />

a major transformation <strong>to</strong> the upper reaches of<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 />

the creek (Kreutz, 2006). Residents of Summerhaven,<br />

a small community located on Mt.<br />

Lemmon, continues <strong>to</strong> be concerned about the<br />

impacts of future fires on their water resources.<br />

In all of these situations, climate information<br />

can be helpful in assessing vulnerability <strong>to</strong> both<br />

flooding <strong>and</strong> water quality issues.<br />

Implementation/Application<br />

Little published research specifically targets<br />

interactions among climate, fire, <strong>and</strong> watershed<br />

dynamics (OFCM, 2007b). Publications on fireclimate<br />

interactions, however, provide a useful<br />

entry point for examining needs for <strong>and</strong> uses<br />

of climate information in decision processes<br />

involving water resources. A continuing effort<br />

<strong>to</strong> produce fire-climate outlooks was initiated<br />

through a workshop held in Tucson, Arizona, in<br />

late winter 2000. One of the goals of the workshop<br />

was <strong>to</strong> identify the climate information<br />

uses <strong>and</strong> needs of fire managers, fuel managers,<br />

<strong>and</strong> other decision makers. Another was <strong>to</strong><br />

actually produce a fire-climate forecast for the<br />

coming fire season. The project was initiated<br />

through collaboration involving researchers at<br />

the University of Arizona, the NOAA-funded<br />

Climate Assessment for the Southwest Project<br />

(CLIMAS), the Center for Ecological <strong>and</strong> Fire<br />

Applications (CEFA) at the Desert Research<br />

Institute in Reno, Nevada <strong>and</strong> the National<br />

Interagency Fire Center (NIFC) located in<br />

Boise, Idaho (Morehouse, 2000). Now called<br />

the National Seasonal Assessment Workshop<br />

(NSAW), the process continues <strong>to</strong> produce annual<br />

fire-climate outlooks (e.g., Crawford et al.,<br />

2006). The <strong>seasonal</strong> fire-climate forecasts produced<br />

by NSAW have been published through<br />

NIFC since 2004. During this same time period,<br />

111

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