Can Southern California Wildland Conflagrations be Stopped? · 2019. 10. 29. · p,o, BOX 245,...

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PACIFIC , SOUTHWEST .. Forest and Range : Experiment Station FOREST SERVICE U,S, DEPARTMENT OF AGRICULTURE p,o, BOX 245, BERKELEY, CALIFORNIA 94701 USDA FOREST SERVICE GENERAL TECHNICAL REPORT psw- 7 11974 Can Southern California Wildland Conflagrations be Stopped? Clive M. Countryman

Transcript of Can Southern California Wildland Conflagrations be Stopped? · 2019. 10. 29. · p,o, BOX 245,...

  • PACIFIC, SOUTHWEST.. Forest and Range: Experiment Station

    FOREST SERVICEU,S, DEPARTMENT OF AGRICULTUREp,o, BOX 245, BERKELEY, CALIFORNIA 94701

    USDA FOREST SERVICE

    GENERAL TECHNICAL

    REPORT psw- 7 11974

    Can Southern California

    Wildland Conflagrationsbe Stopped?

    Clive M. Countryman

  • CONTENTSPage

    Introduction 1

    The Fire Problem .

    Climate, Fuels, Topography, and People Create Fire Problem

    Relatively Few Fires Become Conflagrations 2

    Conflagrations Are Most Frequent During Santa Ana Winds 2

    Suppression of Santa Ana Fires Is Difficult 3

    Fire Control as a Solution 4

    Fire Prevention Has Limited Value 4

    Effect of Organizational Problems on Fire Size is Small . . . . .. 4

    Firefighting Techniques and Equipment are Not Adequate 4

    Increased Fire Control Force is Only a Partial Answer 5

    A Solution Through Fuel Modification .... . . . . . . . . . . . .. 6

    Rotational Burning Creates a Mosaic of Age Classes 6

    Adverse Effects .. . . . . . . . . . . . . . . . . . . . . . . . . . ., 7

    High Costs 7

    Possible Increased Fire Hazard 7

    Fuel-Breaks Provide Strips of Modified Fuel 8

    Fuel-Type Mosaics Can Lower Energy Output 9

    Fuel-Type Mosaics Can Be Created in Many Ways 9

    Fuel-Type Mosaics Are Not a Quick Cure 10

    Complete and Coordinated Planning is Essential 10

  • Countryman, Clive M.1974. Can southern California wildland conflagrations be stopped?

    Pacific Southwest Forest and Range Exp. Stn., Berkeley, Calif.,11 p. (USDA Forest Servo Gen. Tech. Rep. PSW-7)

    In southern California, many fires start and burn under conditions thatpermit their control with little burned acreage and fire damage. In contrast,under other conditions of weather and topography, on a small group offires, control effort is relatively ineffective; they become large and destruc-tive. A major reason for these "conflagration fires" is the extreme difficultyof stopping the head of a hot, fast-running fire in dry fuels and strong winds.No radically new concept of suppression can be anticipated. The bestprospect for alleviation of the problem is modification of the vegetation toreduce fuel energy output. In a fuel-type mosaic containing large areas oflight fuels, where conventional suppression will be effective, potential con-flagrations could be brought under control while relatively small. Creationof the fuel-type mosaic will require coordinated area-by-area planning anda variety of techniques.

    Oxford: 432.16(794):187x424.5

    Retrieval Terms: fue management; southern California; high intensity fires;flash fuels; fuel modification; chaparral fues.

  • 'lle 1970 fire season was one of the worst in Cali-fornia's long history of disastrous fire seasons-certainly the worst in recent years. More than500,000 acres of watershed and timber were burned,most of them in the short period between September25 and October 4. The loss of 16 lives can be attrib-uted to the fire activity. More than 700 homes andother structures were burned, and fire damage andsuppression costs have been estimated at$233,000,000. The damages will continue to mount,since the threat of flood and erosion will continueuntil protective vegetative cover returns to the de-nuded watersheds-in some areas this will take manyyears.

    California does not have an exclusive corner on thelarge-scale, high-intensity fires often called conflagra-tions or conflagration fires. In 1970, several such firesin Washington State destroyed extensive areas of tim-ber. The Trapper Peak and Sundance fires burned inIdaho and Montana in 1967. Other regions also havelarge wildland fires from time to time. But conflagra-tions in other areas are usually infrequent, with sev-eral to many years elapsing between "bad" seasons.In California, large and devastating fires occur nearlyevery year. Statistics compiled by the U.S. ForestService indicate that the California region consistent-ly accounts for about 42 percent of the bumed areaand 55 percent of the reported damage in the Nation-al Forests within the contiguous United States. Mostof the California conflagrations occur in the southernhalf of the State, the area south of the TehachapiMountains being particularly susceptible.

    The gravity of the southern California fire problemhas long been recognized. But despite years of effortby control agencies and research, the fires continue tooccur with alarming regularity, and damages and sup-pression costs continue to grow.

    This paper describes the causes and characteristicsof the conflagration tires in southern California, andevaluates present and proposed efforts to find a solu-tion. A unified program aimed at the one element ofconflagration fires that can be practicably modified-the fuel-is outlined.

    THE FIRE PROBLEM

    Climate, Fuels, Topography,and People Create Fire Problem

    Why are there so many fires in southern Cali-fornia? Primarily because the Mediterranean climateand a distinctive complex of topography and fuelcreate conditions favorable to major fires dUringevery month of the year. The winters are mild, withinfrequent short rainy periods. A long period withoutrain often extends from early spring to late fall orearly winter. Steep and rugged mountains, cut bynumerous canyons, border most of the major cities.Much of the mountain land is covered with a densegrowth of flammable chaparral shrubs, such as cha-mise, manzanita, ceanothus, and scrub oak. On thelower slopes and foothills, this heavy growth givesway to lighter, but extremely flammable vegetation,such as sage, buckwheat, and various grasses andforbs. Some of the higher ridges are covered withconifers-mostly pine-interspersed with chaparraland grass. During the late winter and early springgrowing season, the vegetation usually contains largeamounts of moisture-providing there has beenenough rain to start growth at all. But with the onsetof the long rainless season, the annual plants die, andthe shrubs lose much of their moisture. By Septem-ber, some of the living plants, such as charnise, can beignited with a match, and the dead and dry annualscan be touched off by a spark. After a fire, many ofthe plant species sprout prolifically, and otllers re-generate from seed left in the soil. Within 10 to 20years, enough standing fuel has developed and deadmaterial accumulated to permit the area to burn hotand fast again.

    The great population influx into southern Cali-fornia has vastly complicated the fire hazard createdby natural conditions. Residential subdivisions and in-dividual houses have been pushing farther and fartherinto the mountains. Houses are often perched onledges bulldozed into the steep slopes, or are crowdedon sharp ridges and in narrow canyons. The conifer-covered ridges do not escape this influx-wherever

  • private land is available, homes and resort communi-ties abound. Campgrounds, picnic areas, and organiza-tion camps dot the public lands in these areas. Theresult is a fire control problem probably withoutparallel elsewhere in the world.

    Relatively Few Fires Become Conflagrations

    All fires that start in California do not have thepotential for becoming large and damaging. Localvariations in weather, fuels, topography, and the lo-cation of the fire may limit the rate and extent of firespread, and create wide variations in the difficulty offire control. And wildland fire control forces are high-ly effective. As a result, the vast majority of fires arecontrolled while still small. In the 5-year period end-ing in 1968, less than 1 percent of the fires on Cali-fornia National Forests became 300 acres or larger,and less than 4 percent larger than 100 acres. EvendUring the unusually severe conditions between Sep-tember 25 and October 4, 1970, less than 5 percentof the fires reached 300 acres or more. It is the fewfires that escape early control, however, that do mostof the damage-80 to 90 percent of the total. And itis these fires that must be stopped if the southernCalifornia conflagration problem is to be solved.

    Conflagrations Are Most FrequentDuring Santa Ana Winds

    During most of the year, southern California haswesterly winds and a marine climate. Hot days canoccur almost any time during the year, but are mostfrequent during the summer and early fall. Because ofthe marine influence, the air is seldom excessivelydry. Overcast days even in summer are not unusual.Relative humidity, and hence fuel moisture also,usually reach fairly high levels at night. Under theseconditions, fires can usually be controlled whensmall-most within a short time after they start. Oc-casionally, however, when the weather is particularlydry or windy, a fire will escape early control andbecome large and damaging. Such fires are relativelyrare under the marine climate, however.

    Most of the large fires in southern California occurwhen the marine airflow is replaced by the fOehn-type Santa Ana winds. Originating as cold, dry airhigh in the troposphere, these winds sweep downfrom the Great Basin area, warming by compressionand becoming more dry as they come. Reaching theground near the desert rim, they roar down the moun-tain slopes and canyons to the sea. Wind speeds mayreach 100 miles per hour in exposed areas, and rela-tive humidity frequently approaches the vanishingpoint. The rough, broken topography and high wind

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    speeds create highly turpulent air flow in the manycanyons. Wind direction in these areas may switch180 degrees and back again in a few seconds.

    The Santa Ana "season" ordinarily starts in middleor late September. Santa Ana periods increase in fre-quency during October and November and begin totaper off in December. A second peak in Santa Anafrequency may Occur in March (table 1).

    Table I-Number of Santa Ana periods by monthssouthern California 1951-60

    Month Frequency Average days

    September 11 4.4October 19 4.5November 26 5.0December 18 3.7January 7 1.7February 10 1.9March 17 2.5April 8 1.8May 7 1.4June 4 4.5July 2 2.5August 0 0

    Santa Ana periods that occur in fall and earlywinter, before the rains begin, generally create thegreatest conflagration hazard, as the moisture contentof both dead and living fuel is then likely to be at itslowest ebb. Because of the rapid drying of all fuelsunder Santa Ana conditions, however, major fires canoccur later in the year, particularly when winter rain-fall is light. For example, three fires starting in themountains at the edge of Los Angeles during a SantaAna on March 16, 1964, burned a total of 11 ,650acres, destroyed 20 houses, and severely damaged 10others.

    The Santa Ana winds usually follow a typical pat-tern of development and regression. In their initialphase, the strong winds reach the ground suddenlyand follow the terrain configurations. The tempera-ture is often high, and the relative humidity remainslow both day and night. With these conditions, livingfuels become parched and the dead fuels quickly be-come tinder dry. Because the dry Santa Ana air isrelatively heavier than the more moist marine air, thewinds tend to "channel," flowing through the moun-tain passes and down the main drainages. Betweenthese areas the wind is often light. The initial phase ofthe Santa Ana can usually be measured in hours, butoccasionally may last 2 or 3 days.

    When the area on the lee side of the mountainsfills with the dry, heavy air, and the offshore pressuregradient begins to weaken, the strong Santa Ana 1

    [;

  • winds begin to lift above the ground, bringing somemoderation in the wind speed at the surface. Thisprocess begins at low elevations first, and then pro-gresses upward until only the higher slopes and ridgeshave the strong winds. The high-speed winds may sur-face again intermittently, particularly at night. Wherewinds are light, thermal up-slope and up-canyon air-flow will develop during this phase of the Santa Ana,as it normally does under the marine climate. The airremains extremely dry, however, and the wind overthe ridges is opposite in direction to marine airflow.This phase of the Santa Ana lasts for varying times-usually 2 or 3 days, but sometimes a week or more,

    As the offshore gradient continues to weaken, themarine air begins to intrude again, first along thecoast, and then pushing further inland as onshorepressure gradient builds. Although burning conditionsin this phase of a Santa Ana have been greatly mod-erated, it is a period of high hazard for firefighters. Inthe area where the marine and Santa Ana air meet,the wind can be highly variable in speed and direc-tion. The fuels remain extremely dry, and fires canflare up qUickly and move rapidly, particularly inrough terrain. Most firefighting accidents in southernCalifornia occur during this phase of a Santa Ana.Finally the Santa Ana winds cease, the fuels begin topick up moisture from the marine air, and normalweather conditions again prevail.

    Suppression of Santa Ana Fires is Difficult

    Controlling a fire that starts in a wind affectedarea during the initial phase of a Santa Ana is anenormously difficult task. The dry fuels permit firesto start easily and build up quickly. Within a fewminutes spot fires begin to appear. The fire is then sowidespread that it is usually beyond hope of controlby initial attack forces. Driven by the strong wind,the fire spreads rapidly. It is not unusual for a fullydeveloped fire in chaparral to enlarge at the rate of 4to 6 square miles per hour dUring the initial phase ofa Santa Ana. Spot fires are numerous, sometimes upto a mile ahead of the main fire and occasionally asmuch as 4 miles. Because of the spot fires, roughtopography, and turbulent wind, the fire front is oftenextremely ragged-the effective fire front may be verydeep, with rapidly enlarging spot fires and movingtongues of fire as much as a mile ahead of the mainbody of fire. The smoke from the fire is held close tothe ground by the wind, cutting visibility to near zeroin many areas.

    As tlle fire grows, so does the difficulty of control-ling it. Barriers that could have been used by fire-fighting crews to make a stand against a fire under the

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    marine climate become ineffective as a hail of burningembers is driven into the unburned fuel ahead of thefire-Santa Ana fires have been known to cross free-ways without slowing. Long distance spotting be-comes more prevalent as the fire enlarges. Densesmoke, and blowing sand, dust, and ashes make con-trol work slow and arduous. Because of the rapid firespread, numerous spot fires, poor visibility, and thelarge and deep fire front, the hazard to the firefight-ing force is extreme. Some of the usual firefightingtools and techniques also become ineffective.

    Thus, the fire often continues to spread rapidlywith the wind until the fire head runs out of fuel orthe initiai phase of the Santa Ana ends. But eventhen, the fire is not over. Control forces are still facedwith the monumental task of constructing manymiles of fireline to stop the lateral and rearwardspread of the flames. If the wind continues, aqdi-tional rapid fire runs, parallel to the initial run, mayoccur. Because of the rugged topography, access tothe fire edge is nearly impossible in many places, andfeasible locations for control lines are few and farbetween. Also, considerable time is required to con·struct effective control lines. As a result, the fire maydouble or even triple in size during the final controloperations, even though burning conditions havemoderated.

    Usually, little can be done to stop the head of afire during the initial phase of a Santa Ana, but effec-tive work is often possible at the rear and much ofthe flanks of the fire. Because of the strong wind,large sections of the rear of the fire oftentimes goout, and frequently the flanks are relatively free ofmany of the problems that plague firefighters at thehead of the fire. Thus, it would appear that if fire·fighting efforts were concentrated on the rear andflanks of the fire, control could be effected soon afterthe head of the fire stops. And this technique is fre·quently used in other areas where fires burn understrong winds. Unfortunately, however, the "people"problem often precludes the effective use of thisstrategy in southern California. In this area it is nowunlikely that a fire can become large without homes,communities, and various other improvements beingin its path. Because of this threat, it is frequentlynecessary to divert a large part of the available con·trol force to the evacuation of people and the protec-tion of structures and improvements. Often onlytoken effort can be made toward control of the rearand flanks of the fire until the fire head stops. Thisproblem becomes particularly acute when severalmajor fires are burning at once and fire control forcesare thinly spread.

  • FIRE CONTROL AS A SOLUTION

    Much effort has been devoted to the abatement ofthe conflagration fire problem through improved firecontrol, and further endeavors in this area are beingmade or have been proposed. They include fire pre-vention activities, development of organizationalstructures and procedures for multifire and multi-agency fire suppression, increases in fire controlforces and their efficiency, and improvements in fire-fighting techniques and equipment. Over the years,substantial increases in the effectiveness and effi-ciency of fire control operations in general have beenachieved. No apparent drop in the number of confla-gration fires has resulted, however, and the economicand human losses directly attributable to these firescontinue to mount. There are several reasons for thiscondition.

    Fire Prevention Has Limited Value

    Fire prevention has received considerable attentionas a possible means of eliminating or reducing thenumber of conflagration fires; obviously a fire thatdoes not start will not have to be controlled. Duringthe critical fire weather period of September 25 toOctober 5, 1970, the fire control agencies greatly in-tensified their fire prevention efforts. This action un-doubtedly prevented many fires that would otherwisehave further overloaded the fire control forces. Butfire prevention programs appear to have little effecton those indifferent to the consequences of carelessuse of fire and fire starting agents. Arson fires are notsusceptible to fire prevention programs, and neitherare accidental fires such as those caused by motorizedvehicle and other equipment accidents. Despite inten-sive fire prevention in 1970, the number of fire startsset a record.

    All fires do not have conflagration potential; firesstarting in some areas and from some causes are morelikely than others to become conflagrations. Al-though fire prevention programs may reduce the totalnumber of fire starts, even the best of fire preventionis not likely to significantly affect the number of firestarts that can become conflagrations.

    In one area, however, fire prevention action couldhave significant impact. In California during 1970,about 55 percent of the burned area resulted fromfires started by powerlines. In southern California,the figure was 68 percent, and included some of themost devastating fires. Although these 1970 figureswere probably higher than normal, powerlines areknown to be consistently a major cause of conflagra-tion fires. Usually caused by strong winds, most such

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    fires start in extreme fire weather, and often in ex-posed areas of difficult access. Almost all powerlinefires are started by secondary or "feeder" lines, notthe major transmission systems. New types of con-ductors and techniques to put these powerlinesunderground have been developed. Application ofthis technology could virtually eliminate powerlinefires and would substantially reduce the burned acre-age in southern California-perhaps by as much as 50percent.

    Effect of Organizational Problemson Fire Size is Small

    In southern California, several fire control agenciesoften must work together and provide mutual assis-tance during fire control operations on large fires anddUring multiple fire situations. The mutual aid be-tween agencies in this area is perhaps the best any-where in the nation, and it has been effectively usedmany times. It is probably inevitable, however, thatsome problems will arise between agencies that differin organizational structure and power to. act-especially during the confusion of multiple fires ofmajor proportions.

    Changes in fire control organization and pro-cedures, particularly for critical fire situations, havebeen considered as a means of reducing the conflagra-tion fire problem. Studies aimed at the developmentof sophisticated organizational structures and of tech-niques and procedures for highly centralized controlof fire suppression operations have been undertaken.But interagency problems have been largely procedur-al and administrative. They have had little effect onthe number of conflagration fires or tlle area thatthey burn. Thus, although more sophisticated organi-zation and operational procedures may possibly ef-fect more economic fire suppression, this line of at-tack does not appear to hold much promise for abate-ment of the conflagration fire problem.

    Firefighting Techniques andEquipment Are Not Adequate

    A fire that starts in an exposed area under a strongwind and dry fuel conditions, and with extensiveareas of dense chaparral ahead of it, has a high proba-bility of becoming a major fire unless it is suppressedalmost immediately. Most chaparral fuels have nearlyideal characteristics for rapid combustion under dryand windy conditions, and the heat energy producedby a large and rapidly moving fire is tremendous. Forexample, a fire enlarging at the rate of 4 square milesper hour will produce 400 to 800 billion Btu's of heatper hour-about the same as burning 3 to 6 million

  • gallons of gasoline. And the greatest heat productionis at the head of the fire. Because of the enormousenergy output of an intense chaparral fire, presentfire suppression methods and equipment are generallyineffective in stopping the head of a hot, fast-runningfire in a strong wind. This is the primary problem inthe control ofconflagration fires.

    Fire suppression methods have not changed basi-cally since organized fire control began; equipmentand techniques already in use have been improvedand modified. Thus, bulldozers and other mechanicalequipment are now used for much of the firebreakconstruction that was formally done manually, butfirebreaks still remain the basic fire control method.Fire tankers and portable pumps have replaced thebucket brigade, and these have been supplementedwith aerial delivery of water and fire retardants.Chemical retardants have been used in fire suppres-sion since ancient times, but today better formula-tions and delivery methods have made their use morewidespread.

    Further improvement in firefighting techniquesand equipment has been strongly supported in thesearch for an answer to conflagration fires. For ex-ample, soon after the 1970 fire disaster, the sugges-tion was made that massive air attack with fire retar-dants would provide quick control of conflagrationfires. Over-all, however, the potential for "victorythrough air power" does not appear bright. The useof air tankers in the conditions in which conflagrationfires burn is beset with difficulties. The hazard oflow-level flying in rough terrain and turbulent windsmay often preclude the use of aircraft at all. Air tank-ers do not provide an efficient method of retardantapplication; a sizable part of the retardant delivered iswasted-even under favorable conditions. And on themany spot fires and deep ragged front of a conflagra-tion fire, delivery of extremely large volumes of fireretardants or water is required for any significant ef-fect on fire behavior.

    The effectiveness of fire retardants also decreasesrapidly as fire intensity increases. Fire retardants arejust that; they can be. used to retard or slow a fire,but seldom extinguish it even under moderate burn-ing conditions. It is essential that fire crews andequipment be able to work on the fire edge very soonafter the retardant is applied if fire spread is to bestopped and the retardant drop is to be of any value.In conflagration fires, the opportunities to do so areusually limited to the flanks and rear of the fire be-cause of difficult access and the extreme hazard atthe head of the fire. Like other fire control tech-niques, air attack is stymied by the nature of the

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    conflagration fire and the conditions under which itburns.

    Quick control of conflagration fires will probablyrequire a radically new concept or technique in firesuppression. Such a breakthrougll is not imminent,and it is improbable that one will appear soon. Sup-pression of conflagration fires does not appear amen-able to solution with present technology.

    Increased Fire Control ForceIs Only a Partial Answer

    Public wildland firefighting forces in southern Cali-fornia are probably the best of their kind in theworld. Well trained and well led, and with a largeamount of generally good equipment, they do an ex-traordinary job of suppressing fires and protectingproperty in difficult and hazardous situations. With-out a firefighting force of this quality, losses fromwildland fires would be vastly greater. But higherwages, greater operating and equipment costs, andappropriations that have not kept pace with these

    rising costs, are resulting in erosion of the strengthand quality of public fire fighting forces. Highlytrained and experienced initial attack crews are be-coming smaller or fewer in number. Some firefightingequipment cannot be fully manned, or cannot beused at all because of lack of manpower. The effectof this shrinking firefighting capability is felt mostwhen critical fire weather and numerous fires occurover wide areas. When this happens there are notenough fire crews and equipment to handle the situa-tion, and some fires become large that otherwisecould have been stopped when small.

    On the National Forests, the manpower problemhas recently been ameliorated to some extent by in-creased authorization to use emergency firefightingfunds during the fire season. But this must be con-sidered a stop-gap measure-it does not provide thecadre of well trained and experienced firemen neededto direct season personnel and to insure safety andefficiency in firefighting.

    Since present fire fighting techniques are not gen-erally effective in stopping the head of a conflagra-tion fire, most of the effect of strengthened firefight-ing resources can be expected for non-conflagrationsituations. And fires under such conditions accountfor only 10 to 20 percent of the burned acreage. Theimpact on conflagration fires is not likely to be great.Many of the fires tllat start during Santa Ana andother severe fire weatller are beyond hope of earlycontrol before fire fighting forces can reach them-some before they are discovered-because of rapidspread, difficult access, or botll. Under these condi-

  • tions, it simply is not economically feasible to haveenough crews and equipment to stop all fires immedi-ately after they start; the protected area is too large,the access too difficult, and the number of daysduring the fire season they are really needed in largenumbers too few. While augmented fire control re-sources can ease the strain on firefighting agencies,reduce the number of fires and burned area for non-conflagration situations, and possible effect earliercontrol of some conflagrations, the final answer tothe conflagration fire problem is not likely to befound in more men and equipment alone.

    A SOLUTION THROUGH FUEL MODIFICATION

    If conflagration fires cannot be prevented fromstarting, and cannot be controlled before becominglarge, must such fires be accepted as inevitable insouthern California? I think not. The behavior ofwildland fire is determined primarily by the weather,the topography, and the fuel. Little can be doneabout weather or topography. But wildland fuels,which supply the energy that makes some fires un-controllable, are subject to modification and manage-ment. Limited fuel modification is, in fact, the basicprinciple of most control methods now in use. De-priving a fire of continued energy by removing all ofthe fuel in a band or firebreak around the fire, orputting water and chemicals on the fuel so that it willburn slowly or not at all, is fuel modification.

    People have been changing the characteristics ofvegetation as a fuel, intentionally and unintention-ally, since prehistoric times. World-wide, vast areashave been cleared of native vegetation to providefarming and grazing lands, and sites for .cities. Today,road construction, timber harvesting, silviculturalpractices, grazing use, watershed development, rec-reational use, wildlife management practices-all re-sult in modification of wildland fuels. In some areas,man-made air pollution has altered the vegetation andadded to the amount of high flammable dead mate-rial. Man-caused fires quickly change the vegetation,and repeated fires may effect long-term changes inthe fuel characteristics. Fire prevention and qUickcontrol of fire in areas where fires have occurrednaturally in the past can result in the build-up offlammable vegetation that makes fires more intenseand damaging when they do occur.

    What kind of fuel modification is needed to stopsouthern California conflagration fires? The crux ofthe problem is the high energy output of chaparralfuels in extreme burning conditions. When a firereaches an extensive area of low fuel loading, or slow-

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    burning fuel, or where the chaparral is interspersedwith such fuel, the energy output drops over the firefront or at least many segments of it. Fire suppressionmethods then again become effective along much ofthe fire front, and firefighting forces can safely con-centrate effort on the few relatively high-intensitysections and can take quick advantage oflulls in burn·ing conditions. What is needed then, is to create a fuelcomplex whose energy output even in the worst burn-ing conditions is low enough to pennit firefightingforces to contain the fire.

    Fuel modification is an accepted practice to reoduce fire hazard and to aid in fire control. In timberareas, debris left from logging and silvicultural treat-ments is often reduced by burning or mechanicaltreatment. Prescribed fire is used in forest stands inthe southern United States and some parts of theWest to reduce the amount of fuel. In some regions,extensive areas of brush have been converted to grassor timber.

    Although some fire control experts have long rec-ognized the extensive areas of heavy chaparral as theprimary cause of southern California's conflagrationproblem, no comprehensive plan has been put forthto reduce the hazard through extensive fuel modifi-cation and management. The disastrous 1970 fireseason, however, and the growing realization thatfurther large increases in fire control and fire preven-tion may not be helpful, have focused attention onfuel modification and management as a solution. Sev-eral approaches have been proposed or undertaken.

    Rotational Burning Creates aMosaic of Age Classes

    Rotational burning is one method of fuel modifi-cation that has recently been strongly recommendedfor southern California. After a wildfire, chaparraldoes not burn easily again until the shrubs have re-grown and dead fuel has accumulated. This regrowthmay require 10 to 20 years or more, depending onthe weather, soils, and intensity of the wildfire. In anarea that has been subject to numerous fires over aperiod of years, the chaparral tends to appear in amosaic of age classes, some parts of the mosaic nothaving sufficient fuel to support an intensive fire. Ifthe mosaic contains enough areas of young chaparraland these areas are favorably distributed, conflagra-tion fires are unlikely, as the large expanses of heavyfuels needed for such fires are lacking. Under therotational burning concept, tlle mosaic of age classeswould be artificially created by intentionally burningportions of the area each year under conditions inwhich a fire can be controlled and confined to a de-

  • sired size. The mosaic is to be maintained by repeatedburning at intervals sufficiently short to prevent ac-cumulations of highly flammable material.

    This general technique has been successfully ap-plied for many years in the pine timber stands of theSouthern States, where low intensity fires are used atintervals to remove accumulated dead material andunwanted understory vegetation. It has also been ex-tensively applied in the eucalyptus forests of Aus-tralia.

    But chaparral stands are not the same as timberstands. Although rotational burning is a valuable tech-nique for fuel modification in the areas for which itwas developed, its application to southern Californiachaparral presents certain problems.

    Adverse Effects

    Southern California chaparral can become flam-mable enough to burn intensely within 20 years aftera wildfire. Hence, for rotational burning to be effec-tive, the interval between prescribed burns must beshort-perhaps 15 years or less. Wildfires seldom burnan area with this frequency; it is more probable that40 to 50 years will elapse between successive largefires over the same area-some areas have not burnedfor 70 years or more. Because of the shorter timebetween burns, the average annual burned area can besubstantially greater under a full rotational burningprogram than without. Thus, rotational burning willnot necessarily reduce the amount of area burned; itmay just replace a few large fires with numeroussmaller ones.

    Loss of buildings and other improvements directlyfrom prescribed fire is unlikely. Flood and erosiondamage, impairment of water quality, air pollutionfrom smoke, and similar undesirable fire effects willoccur from prescribed burning, however, just as fromwildfire. Esthetically, rotational burning is not likelyto be much of an improvement over wildfires-a fewlarge fire scars will be replaced with many smallerones. In time, the accumulated adverse effects ofrotational burns may not be smaller-and may evenbe greater-than those that would occur from wild-fires.

    High CostsUnlike timber stands, much of the chaparral in

    southern California has little readily burnable surfacefuel. Most of the fuel is standing, and a large part ofit-65 to 85 percent-is living, with high moisturecontent. The dead fuel is fairly uniformly distributedthrough the living material. The chaparral fuel bedsare also quite porous-a little solid material occupies alarge volume of space. For example, in a typical stand

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    of chamise 6 feet tall, to total standing fuel is equiv-alent to a solid layer less than one-fourth inch thick.With these characteristics, southern California chapar-ral does not burn easily in its natural condition unlessthe burning conditions are well up in the scale ofseverity-relatively dry fuels and at least moderatewind speeds.

    Under such circumstances, fire burns and spreadsjust as hot and fast outside a planned burn area asinside. Thus, prescribed burning in the natural fuelwould require considerable prefire firebreak construc-tion and a sizable control force on hand during theburning to reduce the risk of escape fires to an ac-ceptable' minimum. This would be costly, and thecosts would recur each time the area is burned. Thereare also relatively few days dUring the year when thefuels are dry enough to burn well and burning condi-tions are such that risk of fire escape is not excessive.Hence rotational burning over an area the size ofsouthern California would require that manpower andequipment be available in quantity.

    To increase the amount of fuel consumed and toallow effective burning during periods when vegeta-tion will not normally burn, the chaparral may betreated. Mechanical crushing of part or all of thebrush in place is most effective. This reduces the fuelbed porosity and decreases the moisture content ofthe living material to a point where it will burn well.Herbicides or desiccating agents to increase theamount of dead and dry material may also be used.But these treatments materially increase costs, andalso must be repeated each time the area is burned.

    Possible Increased Fire Hazard

    Whether rotational burning in chaparral will ac-tually reduce the fuel loading and fire hazard formore than a short time is open to question. Wildfiresduring severe burning conditions remove a large partof the fuel; in the more intense fires nearly all of it isburned. Under the moderate conditions in which pre-scribed fires must be conducted, the abovegroundportions of most of the shrubs will be killed. But ofsuch material, only the portions less than one-halfinch in diameter can normally be expected to be con-sumed by the fire. In the dry southern California cli-mate, little of the dead and standing shrub skeletonswill decay before the next prescribed burn. Thus,rotational burning can add to the amount of deadfuel present-the fuel that is so important in deter-mining the flammability of chaparral.

    The possible long-range effects of rotational burn-ing on fuel characteristics must also be considered.Fire has long played a role in the species composition

  • of southern California chaparral. Those species thatcould not withstand occasional fires were simplyeliminated. When lightning was the main source ofignitions, most fires were probably small and burnedwith low intensity, since lightning is usually asso-ciated with poor burning conditions and also tends tooccur in the same general areas. Although it is likelythat there were some large fires, it is also likely thatmost of these burned with low or moderate intensity,because the development of the weather and fuelmoisture conditions needed for intense fires followingan ignition by lightning is a rare event. But with theadvent of man-caused fire sources, the fire potentialhas changed. Man-caused fire ignitions now occurmuch more frequently than those from lightning, andoften occur when intense fires can develop.

    The intensive fire protection which has kept thenumber and frequency of large fires low despite thelarge number of fire starts, is sometimes cited as thecause of fuel buildup and conflagration fires. There islittle evidence, however, that the fuel buildup was lessand that the chaparral lands of southern Californiaburned over more frequently under the lightning fireregime than under present conditions. Rather, thelow- or moderate-intensity lightning fires appear tohave been replaced with high-intensity man-causedfires.

    Since man has become the primary fire startingagent, it is quite probable that the species composi-tion of the chaparral has been changing. Species thatcan survive occasional low- or moderate-intensity firescan be eliminated by repeated high-intensity fires,and such fires now burn most of the area. For ex-ample, there is some indication that the hard chapar-ral in some areas is being replaced by buckwheat andsage, which burn hot and have an extreme rate of firespread. Long-lived species, such as big-cone spruce,that withstood earlier fires are disappearing.

    To be effective, rotational burning must be doneat intervals that are shorter than wildfires are likely toburn the same area. Prescribed fires will generally beof lower intensity than conflagrations, but the re-peated burning at short intervals can be expected toincrease the fire stress on the chapparal and thespecies composition may move to a more flammabletype.

    Although rotational burning, in concept, mayseem an appropriate step toward alleviation of theconflagration fire problem, the difficulties of puttingthe method into practice and its potential adverseeffects suggest that its widespread use in southernCalifornia may be inadvisable. Rotational burningshould probably be confined to situations where

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    other and more permanent fuel modification is notfeasible.

    Fuel-Breaks Provide Strips of Modified Fuel

    During the 1930's, a program was undertaken tobreak up the extensive areas of chaparral in southernCalifornia through a system of firebreaks. Alongmany of the major ridges all fuel was removed in aband 300 to 500 feet wide, and lesser firebreaks ofthe same type were constructed along the spur ridges.The primary purpose of the firebreak system was toprovide barriers that would stop the spread of firewithout the necessity of using fire crews in hazardoussituations or in areas of difficult access. This attemptat conflagration control had disadvantages, however.The firebreaks were expensive to construct and main-tain even with the relatively low cost manpower sup-plied by the Civilian Conservation Corps and similarprograms. The swaths cut through the chaparral wereunsightly, and erosion from the bared soil was amajor problem. Perhaps most important, the un-manned firebreaks failed to stop the spread of fire inthe conditions under which conflagrations occur.With the termination of the emergency labor pro-grams, the firebreak concept was largely abandoned.

    When the difficult fire season of 1955 again em-phasized the problem of extensive areas of chaparralwithout adequate access, the general concept of pre-constructed firebreaks was revived; but with impor-tant differences. Now, instead of leaving the treatedareas completely devoid of vegetation as was done infirebreak construction, the tall and dense chaparral isremoved and replaced with vegetation that burns lessintensely-usually grass. Only a narrow strip near themiddle of the modified band of fuel is kept free ofvegetation to serve as an access way and a place wherebackfiring or burning out can be started. The edges ofthe band are usually made irregular and a few shrubsmay be left within the band to give a more naturalappearance. These modified bands or "fuel-breaks"vary in width, but are usually 100 to 400 feet wideand are strategically located for fighting fires. Theirchief value comes from the rapidity with which a firebarrier can be made in the light fuel, either by re-moval of the vegetation with manpower and equip-ment, or more often by burning the fuel in advanceof the wildfire.

    Fuel-breaks are intended to be manned for use infire control. But like the firebreaks that precededthem, they are not effective in stopping the head of ahot, fast-running fire in a strong wind. As the band ofmodified fuel is relatively narrow, the hazard at thehead of the fire is still great; often precluding man-

  • ning of the fuel-break at all. And the spotting prob-lems, along with the difficulty of safely burning outeven light fuel in adverse wind conditions, frequentlymakes fuel-breaks an ineffective barrier to fire in ex-treme conditions.

    A considerable number of miles of fuel-breakshave been constructed. But because of their limita-tions in fire control, and also because they are gener-ally widely spaced, fuel-breaks have not had a greatimpact in reducing the burned area or damage causedby conflagration fires. Fuel modification of this typecan be effective for less than severe conditions, how-ever, and on some parts of conflagration fires. And amore intensive fuel-break system than presently existscould broaden their usefulness. But fuel-breaks aloneare not a complete answer to conflagration fires.

    Fuel-Type Mosaics Can Lower Energy Output

    The basic philosophy of both fuel-break construc-tion and rotational burning-the replacement of densechaparral with low energy fuels-holds promise forsolution of the conflagration fire problem. In prac-tice, however, each method has limitations. The bestapproach to conflagration control through fuel modi-fication appears to be the creation of a mosaic of fueltypes rather than the mosaic of chaparral age classesenvisioned in rotational burning. Extensive areas ofchaparral can be broken up by areas of low-energyfuels, thereby providing the fuel situation in whichfire suppression techniques are now effective in con-flagration conditions. Native chaparral will still bepresent, but will tend to appear in "islands" ratherthan uninterrupted stands.

    The primary purpose of wildland fire control is theminimization or prevention of fire damage; if fires didnot do damage there would be no need to suppressthem. Because it is unrealistic to expect that all firescan be prevented, some fire damage is bound to occureven with the best of fire control and any reasonabletype and amount of fuel modification. The fuel-typemosaic is designed to assure the control of a fire be-fore it can do an unacceptable amount of damage.The amount of fuel modification needed, then, ispartly determined by the direct and indirect fire dam-age potential in any given area. For high-value water-sheds, the acceptable fire size may be less than 100acres, while in areas of low fire damage potential,burns of several thousand acres may not representintolerable damage.

    Fire behavior also determines the amount and kindof fuel modification required, and this is controlledby the weather, the fuels, and the topography.Topography varies widely over southern California,

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    and local weather also varies greatly from place toplace even under severe conditions. Natural fuel pat-terns are controlled largely by the soils and climateand these are also variable-some areas cannot sup-port the kind and amount of vegetation that creates aconflagration hazard. In some areas little or no fuelmodification will be needed, in others the conven-tional fuel-break will be adequate, and in still othersthe fuel modification must be extensive to keep thefire damage within acceptable limits. The amount andkind of fuel modification, then, must be determinedby a broad survey of southern California.

    Fuel-Type Mosaics Can Be Created in Many Ways

    The opportunities and methods for developingfuel-type mosaics are numerous. Where soils and cli-mate permit, chaparral can be replaced with grass as itoften is on fuel-breaks. Low-volume and slow-burningplants adaptable to harsh sites are being sought outand developed through research and can be used toreplace native vegetation-some plantings have al-ready been made. Use of waste water to irrigate se-lected plant species to create "green belts" of hard-to-burn vegetation has been demonstrated to be feasible.Thinning of native vegetation to develop recreationareas, such as campgrounds and picnic areas, whencombined with modification of fuel on adjacent areascan provide zones where fire can be readily stopped.Golf courses and land planted to useful crops makeexcellent fire barriers, and encouragement throughzoning, tax policies, or subsidies of the use of privateland in selected areas for these purposes will aid inthe development of fuel-type mosaics.

    Many communities in southern California nowhave ordinances requiring the clearing of dense vege-tation from around structures. Along with theseordinances have come intensive education and infor-mation programs for homeowners in landscapingtechniques to lessen the fire hazard to their homes,and in self-help measures that can be used to helpprotect their property from wildfire. When applied,all these have been effective in reducing fire losses.Most fire control agencies would like to see existingordinances strengthened and expanded to includeprovision for adequate water supplies and accessroads for firefighting in housing developments inwildlands, and also to include requirements for fire-resistant building material and construction. There isalso growing interest in revamping zoning regulationsto prevent building at all in areas where protection ofstructures from fire would be extremely hazardousand difficult, if not impossible.

    Although fuel reduction around individual struc-

  • tures can be effective in reducing fire losses, this ac-tion does little to reduce fire size, since the modifiedfuel areas are seldom continuous enough to providean adequate fire barrier. But the fuel reduction meas-ures could be expanded community-wide, extendedinto adjacent wildlands, and combined with adequateaccess roads, water supplies, and fire-resistant build-ings. Then areas so modified would be relatively safefrom wildland fire, and would also provide a barrierto the spread of conflagrations. In effect, housingdevelopments in wildlands could become an asset toconflagration control instead of a liability.

    In southern California, compared with other partsof the State, relatively little effort has been made toconvert chaparral to grass, particularly on publiclands. Mainly this is because suitable areas for conver-sion are generally too small and grass production toolow to make their use attractive for grazing-the eco-nomic benefits gained from grazing use alone do notoffset the conversion and maintenance costs and thecosts of handling livestock in small and scatteredareas. But for grass areas to be most effective in con-flagration control, the volume of grass must be keptlow. An effective way to do this is through livestockgrazing. Thus, a land management policy for publiclands allowing for free or subsidized use of convertedchaparral lands could be justifiable in the interst offire control.

    Few chaparral shrubs are palatable to livestock orgame; hence fuel reduction or modification throughlivestock use is not generally workable. Many of thesaltbrush species, however, including natives, are high-ly palatable and nutritious-some have a nutritionalvalue comparable to alfalfa. Because of their highmineral content, the living material in most salt-brushes burns slowly, and they are well adapted toharsh sites. They develop considerable dead materialwith age, however, and can become nearly as flam-mable as chaparral when mature. But managed live-stock use of chaparral lands converted to saltbrushcan keep both the amount of dead material and totalfuel loading low. Hence, free or subsidized use ofsuch lands can result in an effective and durable con-flagration barrier.

    Similarly, low-cost leasing or subsidized use ofpublic lands for agriculture, or for recreational devel-opment by private interests, where the area affectedcan be of sufficient extent, would encourage thechaparral modification needed for conflagration con-trol.

    Fuel-Type Mosaics Are Not a Quick CureIn an area the size of southern California, develop-

    ment of fuel-type mosaics cannot be accomplished in

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    a short time. Means of financing must be found, andenabling legislation and policies may have to be for-mulated to permit effective development of sometypes of mosacis. And public acceptance of suchWidespread changes in the wildlands must be ob-tained.

    First, costs of fuel-type mosaics are likely to behigh. But besides quick control of fires during severeconditions and substantial reduction of fire damage,important side benefits can accrue. Recreation oppor-tunities should be increased, wildlife habitat im-proved, more forage produced, and in some areaswater yield increased. When properly planned, fuel-type mosaics can also result in a more pleasing land-scape than extensive areas of a uniform vegetativetype.

    Because fire damage is the major consideration infire control, first priority in the development of fuel-type mosaics should be given to areas where fire dam-age is likely to be great. When these are reasonablysecure, the mosaics can then be expanded to areas oflesser damage potential. It is possible that in someareas adequate fuel-type mosaics cannot be createdbecause of extremely steep terrain and poor soils. Inthese, rotational burning may be judiciously used.

    Complete and Coordinated Planning Is .&sential

    In essence, the envisioned fuel modification willreplace the present wildland vegetation patterns withplanned and managed ones. To achieve this, completeand coordinated plans must be developed. As firedoes not recognize administrative boundaries, suchplanning will involve not only fire control agencies,but also local governments, land use planning com-missions, and sometimes private interests. Social, eco-nomic, land use, and environmental impacts must bedetermined and evaluated, and the best combinationsof fuel modification to achieve adequate fuel-typemosaics for a given area established. Inputs into theseplans will be needed from fire control and fire be-havior experts, meteorologists, land-use planningspecialists, economists, landscape architects, plantecologists, biologists, recreation planners, and wild-land research groups.

    Much of the technology needed to create fuel-typemosaics is now available, is being developed, or issusceptible to development through research. Manyof the techniques by which type conversion can bedone have been demonstrated to be feasible. What isneeded now is a comprehensive action plan that willeffectively bring this technology to bear on the onefactor controlling fire behavior that can successfullybe managed and manipulated-the fuel.

    ·::U.s.COVERNMENT PRINTING OFFICE 1978-789-805/43

  • To some, the extensive "monkeying with nature"required to replace the present wildland vegetationpatterns with planned and managed ones may seemabhorrent. But the impact of man and man-causedfires has already had a massive effect on the naturalvegetation, so much so that it is difficult if not impos-sible to specify what a "natural" vegetative pattern in

    southern California really is. And this impact willcontinue as long as conflagrations are a part of theenvironment. The only alternative to planned andmanaged vegetation patterns in southern Californiaappears to be acceptance of the great economic dam-age, threat to human life, and the unpleasant estheticand environmental effects of unmanageable wildfire.

    The Author _

    CLIVE M. COUNTRYMAN heads fire behavior studies at the PacificSouthwest Forest ana Range Experiment Station, with headquarters at theForest Fire Laboratory, Riverside, Calif. He earned a bachelor's degree inforestry at the University of Washington in 1940, and joined the ForestService the following year.

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  • The Forest Service of the U.S. Department of Agriculture· .. Conducts forest and range research at more than 75 locations from Puerto Rico to

    Alaska and Hawaii.· .. Participates with all State forestry agencies in cooperative programs to protect and im-

    prove the Nation's 395 million acres of State, local, and private forest lands.· .. Manages and protects the 187-million-acre National Forest System for sustained yield

    of its many products and services.

    The Pacific Southwest Forest and Range Experiment Stationrepresents the research branch of the Forest Service in California and Hawaii.

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