The North Lake Tahoe Fire Protection District (NLTFPD) is located in the northeastern portion of the Lake Tahoe Basin, on the Nevada side of the Lake. The district serves the communities of Incline Village and Crystal Bay an area of approximately 16 square miles. The District’s Mutual Aid responsibilities cover an area of about 65 square miles. A summary of land management in the District’s service area is provided in Table 3-1.
Land Administration | Acres |
---|---|
Nevada State | 3,945 |
USFS | 9,925 |
Private/Municipal | 6,187 |
Total | 20,057 |
Source: TRPA and Washoe County GIS Databases |
The area has a permanent population of approximately 10,000 residents; however the population more than doubles during peak winter and summer recreational periods. The economy in the area is based primarily in tourism. Skiing and snowboarding, camping, hiking, mountain biking, fishing, summer water sports, and the Lake Tahoe Shakespeare Festival at Sand Harbor, bring thousands of tourists from all over the world to the area each year. (Nevada Commission on Tourism website).
Elevations within the NLTFPD range from 6,230 feet above mean sea level at Lake Tahoe to nearly over 9,600 feet at Rose Knob Peak east of Incline Village. The area is cut by several steep drainages, with Third Creek and Incline Creek the largest.
Washoe County has developed their FEMA hazard mitigation Plan in close cooperation with the NLTFPD. Pertinent elements of this report will be included the FEMA document.
Wildfire and ignition history was compiled from GIS data provided by the Lake Tahoe Basin Management Unit. This data included ignition points and wildfire perimeters for the NLTFPD. USFS staff members indicated that there are approximately 125 ignitions per year throughout the entire basin.
No fire perimeters are recorded in the database within the NLTFPD. Local fire protection districts are not required to report incidents within their districts to the US Forest Service. Each district tracks it’s own data. NLTFPD ignition and fire records are not mapped in a GIS and are not included in this report. NLTFPD staff reviewed this data and added major incidents where appropriate. Ignition data are categorized by source, either human or natural. As expected, many of the human ignition sources cluster around highways and recreational use areas, while natural ignitions tend to be located away from population centers.
The historical data suggests that large, catastrophic wildfires can occur in the district. Ignitions are common but generally do not expand into a sizeable wildfire. A professional fire department and relatively short response times have been effective in keeping fires controllable and short-lived. Good access on paved roads helps shorten the response time. To date, fire suppression resources have been able to stop ignitions from becoming large fires.
Climate may also contribute to the lack of large fires. Though still fire prone, the seasonal window at which the fuels are most explosive is fairly short, and suppression resources are increased during that time.
Wildfire history in the NLTFPD is illustrated by Figure 3-1.
The science of fire ecology is concerned with understanding how past fires have determined the present forest structure and species composition, and describing the role of fire in altering or maintaining forest structure and composition. A fire regime is defined as the frequency and severity of fire occurrence in a given forest type.
Some plant communities depend upon stand-replacing, high intensity fires. Lodgepole pine and fir forests evolved with the occurrence of infrequent, high-intensity, “stand destroying” wildfires that would have completely eliminated the existing forest stand. Few trees within the fire perimeter would have survived. The low frequency of fires in these plant communities would have allowed long periods of time for the accumulation of fuels and the reestablishment of vertical continuity (“ladder fuels”) and horizontal continuity (closed canopies) in the fuel strata. The resulting forest condition would have been conducive to the simultaneous combustion of all fuels during a single fire event.
Other plant communities such as Jeffrey pine forests evolved to burn frequently with low intensity. Under this historic fire regime, low-intensity surface fires would have reduced ground fuels of grasses and shrubs and would have suppressed regeneration of shade-tolerant white fir seedlings, leaving the mature Jeffrey pine trees protected by thick, fire-resistant bark unaffected. Forests with frequent fire occurrence would have had an open, “park-like” appearance with a sparse understory of grass or low shrubs. Though shaded by large, mature trees, the spacing between trees was sufficient to allow sunlight to reach the forest floor and encouraged regeneration of shade-intolerant species like ponderosa pine. Pockets of heavy fuels would have existed under these conditions, but their discontinuous nature reduced the likelihood that a fire would burn with enough intensity to affect mature trees. Frequent surface fires also would have removed accumulated dead and down woody fuels and the green “ladder fuels” that could otherwise have carried flames into the coniferous overstory, potentially provoking a catastrophic, stand-destroying crown fire.
The forest that regenerates with an infrequent, high-intensity crown fire regime is generally very dense and of a single age structure. This density often results in the exclusion of sunlight to the forest floor and subsequent recruitment of shade-tolerant species such as white fir, which contributes to extremely high fuel loadings in the understory.
Research by Dr. Alan Taylor, University of Pennsylvania Department of Geography, (Taylor et al. 2000) suggests that both forest types would have occurred naturally prior to early settlement in the Tahoe Basin but were separated by elevation at roughly the 8,000-foot contour. Above 8,000 feet, low temperatures and moisture high moisture conditions would have only infrequently allowed ignitions to grow into large fires. Below 8,000 feet, in warmer, drier areas, frequent ignitions would have occurred and resulted in consumption of the fuels. This constant consumption of fine fuels kept fuel loadings and fire intensity low.
Altered plant communities and fuel conditions and 20th century fire suppression policies have affected natural fire regimes. Areas that formerly burned with high frequency but low intensity (fires more amenable to control and intervention) now have large accumulations of unburned fuels, which once ignited, will burn at higher intensities.
The lower elevations of the Lake Tahoe Basin contain forest stands with highly altered fire regimes. The loggers of the 1860’s that worked in the region to satisfy the timber demands of the Comstock mines uniformly cut the native forests, originally characterized by uneven tree ages, wide spacings between trees in mature stands, and small openings created by other mortality. The forest that regenerated after this period of intensive logging activity developed into a uniform even-aged, closed canopy stand.
Gruell (2001) effectively illustrates this phenomenon in his book, Fire in Sierra Nevada Forests, A photographic interpretation of the ecological change since 1849. An example of paired photos taken from the same vantage point in Slaughterhouse Canyon north of Glenbrook, Nevada is shown below. The 1873 photo of an uncut forest clearly shows the forest floor and individual trees in the distance visible through the open canopy. The 1993 photo taken from the same alignment shows that the forest density is so high that individual trees can only be discerned at the forest edge. The current conditions, with a dense, almost continuous canopy and ladder fuels that reach to the forest floor are more reminiscent of high elevation forests that were naturally characterized by infrequent, high-intensity stand-replacing crown fires.
Today, most commercial and residential developments in the Tahoe Basin, i.e. those areas most needing protection from catastrophic wildfires, are concentrated in areas well below the 8,000-foot elevation where the fires would have been frequent, low-intensity, light-fuel clearing ground fires.
The recommendations in subsequent sections of this report outline tree densities and forest structures consistent with the forests seen in the historic photographs and are consistent with US Forest Service and Tahoe Regional Planning Agency management objectives to return Tahoe Basin forests to pre-European conditions.
The area served by the NLTFPD contains several natural and cultural resource features that could potentially be at risk during a wildland fire. These resources are described below and selected resource locations are illustrated by Figure 3-1.
The threat to watersheds is important to consider in the overall risk to Lake Tahoe. As the fire severity risk increases in the watershed, there is a greater risk of soil erosion damage in addition to a reduction in groundwater recharge.
The ability of a watershed to receive, store and transmit water is related to the geology, vegetation, and soil that characterizes the watershed. Fire has the potential to significantly alter vegetation and soil properties in a watershed, impacting critical hydrological functions such as interception, evapotranspiration, infiltration, soil moisture storage, and snow accumulation and melt. Impacts from alteration include increases in stream runoff, decrease in groundwater recharge, increase in erosion and sedimentation, and water quality degradation (Zwolinski 2000).
Removal of vegetative foliage, by fire, contributes to increased runoff, degradation of water quality, and decreased groundwater recharge. Vegetation plays an important role in rain and snow interception. A low severity fire that does not change the vegetation interception characteristics will have minimal impact on water yield. Fires that remove canopy foliage and litter material can result in considerable increases in runoff and soil erosion. Removal of vegetation canopy and duff allows more precipitation to reach the barren soil surface, resulting in increased soil surface erosion and degradation of water quality.
Infiltration can be reduced as heating from severe fires alters soil chemistry and can create hydrophobic layers (DeBano, 1981). Groundwater aquifer recharge can be hindered by these hydrophobic soil crust formations. Runoff and erosion are directly related to decreased infiltration and raindrop splash. The amount of sediment carried downstream, as a result, is dependent on soil properties and watershed geomorphology.
In the Lake Tahoe Basin, there are many areas with potentially threatening conditions in the forest. Tree density has increased consistently to the point where a wildfire occurring under a worst case scenario would potentially clear the watershed of trees and other vegetative cover. Such an event would likely render the watershed susceptible to severe flooding events and soil erosion of enormous magnitude.
The Nevada Natural Heritage Program lists nine species within the Incline Village and Crystal Bay urban interface that are identified as threatened or endangered and protected by federal or state law. These species are listed in Table 3-2.
Species Name | Common Name | Status |
---|---|---|
Onchorhynchus clarki henshawi | Lahontan cutthroat trout | ESA |
Accipiter gentilis | Northern goshawk | SP |
Aplodontia rufa californica | Mono Basin mountain beaver | SP |
Glaucomys sabrinus | Northern flying squirrel | SP |
Lepus americanus tahoensis | Sierra Nevada snowshoe hare | SP |
Martes americana | American marten | SP |
Pinus washoensis | Washoe pine | CY |
Rorippa subumbellata | Tahoe yellowcress | CE |
Strix occidentalis occidentalis | California spotted owl | SP |
CE = Listed as Critically Endangered by the state of Nevada CY = Protected as cactus, yucca or Christmas tree SP = State protected under NRS 501 |
The effects of fire on cultural and historical resources depend upon factors which vary from place to place such as fuels, terrain, site type, and cultural or historical materials present. The Cal-Vada Lodge Hotel located at the junction of Stateline Road and State Route 28 in Crystal Bay is the only site listed on the National Register of Historical Places in the North Lake Tahoe Fire Protection District.
Currently there are two fire safe councils in the district: Incline Village and Tyrolian Village. These chapters have been active in developing solutions for wildfire hazard mitigation projects within their community.
The North Lake Tahoe Fire Protection District has a long and successful fuels treatment program. In the early 1990s the district began to identify areas at extreme risk to life, property and safety from wildfire. With the help of professional foresters, they developed fuel treatment projects around community neighborhoods to lower the wildfire threat. Specifically, they treated large open areas between neighborhoods, creating greenbelts so that resultant fires would be of a lower, and likely controllable, intensity as they entered the community. Further, the reduction of fuels allowed better access to ignitions in these areas and slowed the rate of spread, making initial attack resources more effective in controlling fires.
Treatments were designed to create a halo around the community within which the probability of ignition was reduced and the probability of quick control was increased. Open space between neighborhoods, where a wind driven fire could spread uphill quickly, were given priority. These areas were treated with a variety of methods, including cut-pile-burn, and prescribed broadcast burns. Figure 3-2 shows the previous mitigation projects.
The US Forest Service and the State of Nevada have also completed fuels reduction treatments on some of the lots they own in Incline Village. Through its Urban Lots Program, the USFS has used the cut-pile-burn method to reduce fuels within communities.
Like any fire prevention activity, success can only be measured by the absence of a disaster. It is impossible to quantify the effectiveness of these treatments; however the lack of any large fires in the recent fire history indicates that the treatments have been effective. The removal of fuels and reintroduction of fire onto the landscape is consistent with the desired future condition and fire regime discussed in the fire ecology section above.
The TRPA and NLTFPD have entered into a Memorandum of Understanding (MOU) to streamline the process for homeowners seeking to create defensible space and eliminate fire hazards. Pursuant to NRS 474.160, the NLTFPD has the authority and responsibility to remove fire hazards on private or public premises within the district. Through the MOU, the TRPA has delegated to the NLTFPD the authority to issue tree removal permits within 30 feet of structures within the district. A copy of the MOU is provided in Appendix C.
To help facilitate public education regarding the identification and removal of fire hazard trees, the NLTFPD has developed a property evaluation checklist. The explanation provided with the checklist describes the general requirements to comply with state and local fire safety ordinances. A copy of the checklist and explanation is provided in Appendix D.
Tree and vegetation removal on private land in the Lake Tahoe Basin is regulated by the TRPA Code of Ordinances.
Projects that involve funding from a federal source or that are on land managed by a federal agency must comply with the National Environmental Policy Act (NEPA) and the Land and Resource Management Plan (Lake Tahoe Basin Management Unit, 1988) as amended by the Sierra Nevada Forest Plan Amendment, 2004, in addition to the TRPA Code of Ordinances described above. The National Environmental Policy Act enacted in 1969 requires Federal agencies to evaluate and disclose the effects of proposed actions on the human environment in a written statement that addresses:
Compliance with NEPA regulations begins with an internal screening process. If a preliminary review determines that the proposed action will not have any significant effect on the quality of the human environment, either individually or cumulatively, and that therefore neither an Environmental Assessment (EA) or an Environmental Impact Statement (EIS) is required (40 CFR 1508.4), then a categorical exclusion may exist, and no further environmental documentation is necessary or required. Some actions covered in an existing EA or EIS prepared by a Federal agency may not require analysis in a completely new document. Actions which are neither categorically excluded, already covered in an existing document, nor normally subject to EIS requirements, must be analyzed in an EA to determine if an EIS is in fact necessary or required.
An EA is a brief public document that discusses the need for, and alternatives to, a proposed action. The document provides sufficient evidence and analysis to support either a determination of no significant impacts, or a determination to prepare an EIS. If the EA confirms that the impacts of the proposed action are not significant, then a Finding of No Significant Impact (FONSI) is issued, and the NEPA review process is complete. If the EA reveals a significant impact, the proposed action cannot be approved unless it is either analyzed in an EIS, or modified to avoid significant impacts.
An EIS is a detailed document that requires extensive public involvement, facilitates interagency coordination, and provides the basis for permit approvals and other legal clearances that may be required for the proposed action. There are several mandatory steps in the EIS process, including public scoping meetings, publication of a notice of intent in the Federal Register, preparation and circulation of draft and final versions of the document, formal public hearings, and inclusion of public comments and responses to those comments in the final EIS.
It is anticipated that the fuel hazard mitigation projects proposed in this assessment (described in Chapter 7.0) will fall under a categorical exclusion or an EA. The US Forest Service LTBMU is currently following the Forest Service Handbook Interim Directive 1909.15-2003-1 and 1909.15-2003-2 (published in the Federal Register June 5, 2003). The Interim Directive contains several categorical exclusions that could apply to the proposed fuel hazard mitigation projects. Projects may be categorically excluded from an EA or EIS only if there are no extraordinary circumstances related to the project, including, but not limited to, threatened or endangered species, wetlands, archaeological sites or historic properties.
Figure 3-1Fire History and Potentially At-Risk Resources |
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Figure 3-2Previous Wildfire Mitigation Projects |