Cerro Grande Fire

The smoke plume on May 11, 2000, reaches the panhandle of Oklahoma (NOAA image).

The Cerro Grande Fire was a disastrous forest fire in New Mexico, United States of America, that occurred in May 2000. The fire started as a controlled burn, and became uncontrolled owing to high winds and drought conditions. Over 400 families in the town of Los Alamos, New Mexico, lost their homes in the resulting 48,000-acre (190 km²) fire. Structures at Los Alamos National Laboratory were also destroyed or damaged, although without loss or destruction of any of the special nuclear material housed there. Amazingly, there was no loss of human life. The US General Accounting Office estimated total damages at $1 billion.

Prelude

Although wildfire is a natural part of the ecosystem of western forests, fire suppression began to be widespread in the late 19th century just as land-use patterns (e.g. intensive grazing) limited the cover which had formerly sustained and been sustained by low-intensity ground fires. High-density stands of small trees and thick underbrush permitted a natural periodic ground fire to leap into a high-intensity crown fire. There followed a century of fire suppression, during which large fires occurred on the Pajarito Plateau approximately every twenty years: an 1896 fire, several fires in the 1920s, a fire in 1946, the 1954 Water Canyon Fire, the 1977 La Mesa Fire, and the 1996 Dome Fire.

The 1977 La Mesa Fire served as a wake-up call: it burned 15,000 acres (60 km²) in Bandelier National Monument, but accelerated a change in attitudes within the National Park Service toward managing fire. On Bandelier National Monument, firebreaks were improved, as were fuel breaks, and in some areas trees were thinned. The 1996 Dome Fire burned 16,500 acres (67 km2) in nine days and threatened the southern section of Los Alamos National Laboratory. With flame lengths of hundreds of feet, the Dome fire was spectacular and it underscored the problems of passivity and neglect. The Interagency Wildfire Management Team was formed by representatives of Los Alamos National Laboratory, Los Alamos County, Bandelier National Monument, Santa Fe National Forest, State of New Mexico, and Pueblo agencies.

No amount of planning could control the weather, which provided abnormally high precipitation in the early-to-mid-1990s, followed by several years of severe drought. The consequence of these effects was that by 2000, conditions were nearly ideal for a major forest fire on the plateau. Deadfall in the forest had a moisture content lower than that of well-cured firewood. The heavy rains and snows of the mid-1990s had produced luxuriant undergrowth, while the onset of drought toward the end of the decade had dried it out and made it flammable. The stage was set for exactly what happened at Cerro Grande.

Origin

The fire originated as a controlled burn that was part of the 10-year Bandelier National Monument plan for reducing fire hazard within the monument. The starting point was high on Cerro Grande, a 10,200-foot (3110-m) summit on the rim of the Valles Caldera not far north of New Mexico State Road 4, the main highway through Los Alamos County. Like many mountains in the Jemez, Cerro Grande was mainly covered with coniferous forest, composed largely of ponderosa pine, Douglas fir, white fir and aspen trees, with a characteristic rincon (meadow) on its southern slopes near the summit. This grassy area also represented the headwaters of Frijoles Creek (Rito de los Frijoles), which flows southeast into Frijoles Canyon and on to the Rio Grande, passing en route the main tourist areas at Bandelier. The plan for the burn (see the NPS summary below) called for initial ignition ("Phase 1") to be in the rincon, followed by flanking fires ("Phase 2") along the slightly higher country east and west of Frijoles Creek. Ignition of the Phase 1 burn was scheduled for May 4, 2000.

In the aftermath of the disaster, Bandelier officials came under intense criticism for this plan, and particularly, for proceeding with it in the face of what appeared to be powerful contradictions. The main point of contention was wind. In the springtime, the Jemez Mountains are prone to high winds and low humidity which often create high to extreme fire danger. Critics insisted that the likelihood of such winds while the controlled burn was in progress was so great, and the risk of resulting loss of control so severe, that the burn should never have been attempted at that time of year. At the same time, Bandelier officials faced a most disagreeable dilemma.

Proceeding with the burn risked disaster if control was lost, as indeed happened. However, not doing the burn might also have been disastrous because the entire southern slope of Cerro Grande was tinder-dry and ready to ignite catastrophically in the event of a lightning strike (hardly unusual in the Jemez in the spring) or human carelessness with fire. The same winds that militated against starting the controlled burn might then have driven the uncontrolled fire toward Los Alamos, with terrible consequences. In any case, the controlled burn was indeed initiated on May 4, and things rapidly got out of hand.

Timeline

Aftermath

Flash floods

A particular concern was the possibility of flooding in areas downstream from the burned zone. The town of Los Alamos, the national laboratory, and the lower parts of the burned area are all situated on the Pajarito Plateau, an area of extensive canyons and mesas in which surface runoff tends to concentrate in the canyon bottoms. This tendency was exacerbated in Cerro Grande's aftermath by the fact that the soil in the burned areas had become hydrophobic, raising the specter of drastically increased water flow in the streams in the canyons that the existing streambeds may not have been able to handle. This concern, coupled with the prospect of monsoon rains that typically begin in about July in the area, made it urgent to deal with the possibility of flooding.

The highest priority for flood management involved the Los Alamos Critical Experiments Facility (LACEF), a remote site for conducting research in nuclear criticality safety that housed substantial quantities of special nuclear material. The LACEF laboratories were in the bottom of Pajarito Canyon. To protect LACEF, a large, temporary "dry dam" was constructed in the canyon upstream of LACEF to temporarily contain flash floods that might result if an intense thunderstorm happened to rain heavily on the terrain drained by Pajarito Canyon. Runoff was monitored at multiple stations in the headwater streams above Pajarito Canyon.

In the event, the monsoon of the summer of 2000 was not particularly intense, and damage from flooding was generally minimal. No severe flooding occurred in Pajarito Canyon before vegetation upstream had recovered sufficiently, over several years, to retain runoff, and the dry dam eventually was removed. Severe flooding did occur in upper Pueblo Canyon, significantly damaging Diamond Drive, one of the town's arterial roads.

Erosion

Although flash floods were fortuitously minimal, erosion nonetheless was substantial, and many miles of the 57-mile network of trails maintained by Los Alamos County were severely damaged. Canyon bottoms in particular were clogged with fallen trees and boulders washed down from above. Erosion might have been far worse, had there not been timely intervention.

A Burned Area Emergency Rehabilitation Team (BAER) was assigned to assess the damage and to implement a rehabilitation plan to reduce further natural resource damage. During July 2000, approximately 7000 hydromulching and hydroseeding flights by Air Tractors were carried out on 1,600 acres (6.5 km²) of the burned area to reduce erosion and speed revegetation. A local trail work organization, Volunteer Task Force, devoted many thousands of hours to rebuilding trails and planting trees. Local school children made many thousands of "seed balls", which they broadcast in the burned areas to accelerate regrowth of the vegetation. To control erosion mechanically, Los Alamos County work crews laid thousands of trees across slopes, and chipped other trees.

Damage to buildings

The presence of Los Alamos National Laboratory in and downstream of the burned area posed several unusual problems in remediation, beyond the ones resulting directly from destruction of some of the institution's buildings by fire.

Other problems arose from fire-generated soot which seeped into buildings, shorting out electrical equipment and clogging HEPA filters necessary to the operation of clean rooms at some of the laboratories. Resolving these problems took several years in some cases.

Meanwhile, the Federal Emergency Management Agency (FEMA) mobilized to provide relief to the residents of Los Alamos who had been burned out of their homes. A compound of portable buildings ("trailers"), known locally as FEMAville, was constructed on undeveloped land near the county rodeo grounds on North Mesa, providing housing for hundreds of displaced residents. Some residents complained about the timeliness and thoroughness of the FEMA response. The trailers became available only in late June 2000, after municipal utilities were completed and the trailers were delivered and hooked up to the utilities. By 2006, all the trailers were removed and most of the displaced residents were settled into new homes, although reconstruction of houses in the burned area continues as of 2008. In 2007 the former FEMAville site was proposed as a full-service RV park. This proposal was soundly rejected by residents and the FEMAville acreage remains open space.

Adjacent communities

Santa Clara Canyon, home to Puye Cliff Dwellings, was devastated by Cerro Grande. The people of Santa Clara Pueblo who formerly earned income through tourism now operate the Big Rock Casino in Española, New Mexico. On June 20, 2000, residents of Isleta and Sandia Pueblo hired four environmental engineers to permanently work with the Cerro Grande Wild Fire aftermath. A forty-member forestry crew with members from the Eight Northern Pueblos has built 3,000 small dams (to minimize siltation of Santa Clara Creek), and planted one million trees on 3,500 acres (14 km²).

Future

A re-examination of forest fire prevention techniques was already in progress at the time of the Cerro Grande Fire and received added impetus from the damage the fire inflicted. The far larger Rodeo-Chediski fire in Arizona, as well as several other fires in the western United States in 2002, completed the process of bringing forest fires into political focus, leading to the establishment of the Healthy Forests Initiative in 2003. This initiative remains controversial, and its applicability to the relatively sparse forests of the Jemez Mountains that were consumed in the Cerro Grande Fire is unclear. It is certainly clear, however, that significant thinning of the coniferous forest of the Jemez has occurred in the years following Cerro Grande.

The local community has also taken many steps to prevent and protect against future wildfires. Steps include removing vegetation around buildings to increase defensible space; replacing roof and sheathing materials (e.g. cedar shakes) with less flammable materials; and continued thinning and reduction of fuels in unburned wooded areas in and around town, particularly in the canyons below populated mesas.

A new book on the Cerro Grande Fire was published in the summer of 2010. Inferno by Committee (ISBN 9781426929878) gives a detailed history of the fire and what went wrong. The book is written by a professional fire-fighter.

Image gallery

Wikimedia Commons has media related to Cerro Grande wildfire, 2000.
The lasting effects of the Cerro Grande wildfire on the Quemazon Trail west of Los Alamos as seen in July 2014. The ground is littered with burnt logs. Burnt, limbless tree trunks fill the landscape, but pine trees and other vegetation have begun to sparsely populate this once baren burn area.
The lasting effects of the Cerro Grande wildfire on the Quemazon Trail west of Los Alamos as seen in July 2014. Scroll to view full panorama.

See also

References