Vignettes > Fire geomorphology: Fire-related erosion helps to shape our landscapes

Fire geomorphology: Fire-related erosion helps to shape our landscapes

Kerry Riley
Boise State University, Geoscience
Author Profile

Shortcut URL: http://serc.carleton.edu/60020

Location

Continent: North America
Country: United States
State/Province:Idaho
City/Town: Frank Church-River of No Return Wilderness
UTM coordinates and datum: none

Setting

Climate Setting: Northwest
Type: Process, Stratigraphy, Chronology

Figure 1 - (left) The large (~ 7,500 km2) Middle Fork Salmon River watershed, located in central Idaho, encompasses steep rugged terrain. Blue and red polygons show the contributing areas of ten recent debris-flow producing basins that have recently incised alluvial fans located at the tributary junction. The blue line is the main-stem Middle Fork Salmon River which flows south-west to north-east. The stars represent the locations of five nearby weather stations. (right) The location of the larger (~ 35,079 km2) Salmon River watershed is outlined with a blue polygon and the Middle Fork Salmon (MFSR) is outlined in red. Details


Figure 2 - Wildfires burned mid-elevation forests during the summer of 2006 and 2007 in central Idaho. A large fire-related debris flow followed these mixed severity fires. The debris flow deposit telescoped out of and incised through the historic perched fan. There is a 16 ft red raft in the left photo on the right side of the picture (upstream side of the fan). Details


Figure 3 - In the summer of 2008, a large fire-related debris flow was initiated near the watershed divide of a small steep tributary basin of the Middle Fork Salmon River. The large, sediment-charged flow, incised through old alluvial fan deposits, exposing past layers of deposition. Marginal levees can be seen adjacent to the incised channel. A person is circled in red and can be used for scale. Details


Figure 4 - Rill formation near a watershed divide following severe fire causing decreased infiltration, decreased surface roughness, and increased surface runoff. Details


Figure 5 - This figure compares the type of alluvial fan deposition over time. Sheetflood deposits consist of alternating lens of coarse and fine grain sediment. Debris flow deposits consist of large angular unsorted clasts that are matrix supported. Details


Figure 6 – The figure is of the subset used to calculate long-term sediment yields encompassing the last 6 ka. The x-axis is calibrated years BP moving forward in time from left to right with 0 cal yr BP being 1950 AD. The data in the inverted bar graph represents the sample count of the number of dated charcoal fragments creating the above smoothed curves. Red bars are lower basin samples and blue bars are upper basin samples. Curves are the cumulative sum of 14C age distributions and are not normalized. The black curve is a 100-yr running mean and represents all dated fires (n=49) collected from within all deposits types (i.e., debris flows, burn surfaces, hyper-concentrated flows, sheetfloods, and over-bank deposits). The blue curve (not smoothed) represents dated upper basin and the red curve (not smoothed) represents dated lower basin confidently identified as debris flow deposits. The numbered debris flows represents the total age constrained deposits within the 2 ka moving window. Mean debris flow frequency per sub-basin was calculated by averaging the number of debris flow deposits within individual alluvial fans per timescale (2000 yr). Middle Fork Salmon debris flow frequency is calculating by including the total number of debris flows entering the MFSR per timescale (accounting for only 10 debris flow producing sub-basins). Details


Description

The frequency of large wildfires has increased on all vegetated continents (Bowman et al., 2009). Wildfires can have profound influences on erosion rates, particularly in steep mountain basins. Fire-related erosion varies in both magnitude and impact as a function of burn severity, basin characteristics, and timing and intensity of local climate conditions (Cannon et al., 2001, Meyer and Pierce, 2003). This study evaluates fire-related sedimentation from small steep tributaries of the Middle Fork Salmon River (MFSR) in central Idaho (see figure 1) to evaluate the timing, frequency, and magnitude of fire-related erosion. Rates and magnitudes of sediment delivery from hillslopes to fluvial systems influence long-term landscape evolution, aquatic habitat, reservoir capacity, and infrastructure stability (e.g. roads and development).

Short-term sediment yields have been measured using sediment traps and gauges and are orders of magnitude lower than long-term (103-104 yr) sediment yield estimates. Sediments traps are not able to measure large debris flow events. We combine directly measured recent (1997-2008) fire-related debris flow sediment yields and reconstructed fire-related debris flow frequencies to quantify the contribution of fire-related debris flows to long-term (103-104) sediment yields. Holocene debris flow frequencies are estimated from ­­­­14C-dating charcoal fragments preserved in fire-related deposits exposed in incised alluvial fans.

Recent large debris flow events have occurred in years following moderate to high severity fires that burned densely vegetated north-facing slopes in the MFSR (see figure 2). Burn severity data was obtained from the Monitoring Trends in Burn Severity Project (USDA Forest Service/U.S. Geological Survey). These large events have incised into easily erodible, geothermally altered Idaho Batholith granite bedrock and alluvial fan surfaces, deposited material adjacent to the incised channel, (see figure 3) and deposited a new fan surface extending into the larger main channel. Observations suggest that modern large debris flows in the MFSR primarily initiate from increased surface runoff, rilling (concentrated water flow in small channels) and progressive sediment bulking (e.g. Meyers and Wells, 1997) from erosion within the channel (see figure 4). These type of debris flows differ from those generated by saturation of colluvial hollows, which can occur on both unburned (e.g. Iverson 1997) or burned (e.g. Meyer et al., 2001) hillslopes.

Fire influences hydrologic processes in watersheds by 1) reducing the amount and rate of infiltration (water on the ground entering the soil), 2) altering vegetation structure, density, and root stabilization of soils and 3) changing soil and sediment properties (Shakesby and Doerr, 2006). Fires decrease surface roughness by removing vegetation and organic litter and can increase the water repellency of soils (DeBano, 2000). All of these influences increase surface runoff during years following fire. This, in turn, increases erosion of surface sediments, rilling, and debris flows in small steep drainages during years immediately following fire. Recent fire-related debris flows in the MFSR have incised into older alluvial fans and delivered large amounts of sediment into the main channel.

Tributary junction alluvial fans are fan-shaped depositional landforms that form at junctions where higher gradient, sediment filled streams dump into larger lowland areas where streams lose energy. Fans are located where there is accommodation space available to store sediment over time. Incision of alluvial fans by subsequent large debris flows expose past deposits and facilitates investigation of fire-related sedimentation over longer timescales. Alluvial fans act as sediment traps, capturing large individual events over time, preserving a record of deposition that can span long timescales.

Approximately 50%, of study site fan deposit thicknesses, were identified as fire-related. Fans in more-forested basins contain ~74% fire-related deposits compared to ~40% in less-forested basins. This difference could be attributed to increased preservation of large woody material in more-forested basins or to more severe fires in more-forested basins. Although increased vegetation density retains more sediment on hillslopes, burning this vegetation, potentially leads to larger erosional responses (e.g. Cannon et al., 2001). In lower less-forested basins, sheetflooding events were more common and compose greater fan thickness (~26%) compared to more-forested basins (~4%). Sheetflood events make up ~13% of the total investigated fan thickness. This suggests that sheetflood events are smaller in magnitude and deliver less sediment to the fluvial network than debris flows, which compose 62% of total fan thickness. The remaining fan thickness was composed of overbank flood deposits, channel deposits, buried soils, or deposits that could not be confidently identified.

What climate conditions are associated with large fire-related debris flows preserved in the stratigraphic record?

Paleoclimate records from the lower Salmon River and from the headwaters of the MFSR suggest that late Pleistocene-early Holocene (14-8.5 ka) climate was generally wetter, cooler, and more variable, mid-Holocene (8.5 – 5.5 ka) climate was generally drier, warmer, and more stable, and late Holocene (4 ka - present) climate was generally cooler, wetter, and more variable (Davis et al., 2002; Whitlock et al., 2010). Mid-Holocene alluvial fan deposits compose ~4% of total dated deposit thickness (see figure 5), suggesting decreased sediment transport during warm, arid, stable climate conditions. Deposits that date between 14 - 8.5 ka and < 5.5 ka compose ~22% and ~74% of total dated fan thickness (see figure 5) suggesting increased sediment transport during cooler, wetter and more variable climate conditions.

How much sediment do fire-related debris flows contribute to long-term (103-104 yr) sediment yields?

Measured debris flow deposit volumes indicate sediment yields between 1,000–75,000 Mg/(km2.event) [Mg=106grams=1 metric ton]. Fire-related debris flow frequency is greatest during the last 2 ka. While this may reflect better preservation of younger deposits, it may also indicate elevated fire frequency and severity. Based on 39 fire-related debris flows, dated to the last 6 ka, and assuming past similar sediment yields are similar to modern yields, fire-related debris flows have contributed ~190 Mg/(km2.yr) (see figure 6). This suggests that fire is a major driver in long-term sediment yields, accounting for ~70% of a ~6500 yr basin-wide sediment yield for the larger Salmon River (Kirchner et al., 2001).

Climate-driven fires reflect changes in vegetation and are an important control on sediment delivery between the hillslope and fluvial channels in the MFSR. The frequency of fire-related debris flows was greatest during cooler, wetter, more variable climates throughout the Holocene. This suggests that climate is a primary driver of large episodic sediment delivery events that contribute significantly to long-term (103-104 yr) sediment yields in the MFSR. We hypothesize that large fires and debris flows in the MFSR are primarily driven by both increased fuel loads (expanded forest area) and increased sediment storage on hillslopes, punctuated by severe multi-decadal droughts and fires. Increased climate variability associated with the early and late Holocene produced both the fuels and droughts necessary for elevated sediment yields.

Associated References


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