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Snow Pack in Fire Regimes

Snow Pack in Fire Regimes. Amanda Charobee Winter Ecology Spring 2012. Introduction. Until recently the United States has been fighting wild fires with a suppression policy.

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Snow Pack in Fire Regimes

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  1. Snow Pack in Fire Regimes Amanda Charobee Winter Ecology Spring 2012

  2. Introduction Until recently the United States has been fighting wild fires with a suppression policy. In an effort to control the loss of property and life the bureau of land management focuses the use of thinning and prescribed fire projects hoping to limit the fuel supplies to their historical ranges. (McKenzie et al. 2004)

  3. Introduction Continued • Fires remain a threat as they are primarily driven by weather conditions, not fuel. • Global warming/Climate change has the potential to significantly increase the fire regimes in dry areas like the Rockies. • With each new burn more carbon is released into the air, and respiration decreases leading to temperature increases. • Scientists are predicting a lengthening of the fire season in the western US due to this (Heyerdahl et al. 2008).

  4. A Winter Perspective Though many scientists study snow and its structure few have published much beyond its effects on the ecosystem. The snow is an integral part of the environment • It offers protection to prey from predators (David J. Huggard1993) • forms an insulated sanctuary for plants and animals • keeps the soil moist as plants give off radiation, which melts the snow. (Sturm 1992) A burned landscape has more sun and wind exposer then a healthy forest, it could produces abnormal snow pack where both flora and fauna suffer.

  5. The Question Do forest fires and prescribed burning affect the structure of the snowpack? Hypothesis: A burned landscape, can act as an ecological health indicator and show us the full extent of damage to the niche.

  6. Methods Pits were sampled in two different locations as examples of a healthy and burned environment: • Healthy--- Mountain Research Station:9,600 feet • Burned--- Gold Hill/ Four mile canyon at 9,200 Within each setting two pits were dug at random: • One in the trees • One in a clearing

  7. Methods Continued • Temperature gradient was formed with ten centimeter intervals. • Layers were tested for • hardness, density, and • flake structure.

  8. Healthy Landscape Forest 70 II-A2 67 II-B1 Hardness Clearing 46.5 46 II-A2 Hardness 42.5 II-B2 37.2 III_A1 II-B1 25.7 III-A3 19.5 III-A3 III-A3 10 III-B1 III-A2 6 III-B2 0 0

  9. Burned Landscape Forest 48 Depth (cm) II-B1 45 Clearing 39 II-B2 II-B1 Hardness Hardness 24 26 ICE 16 II-A2 III-A3 6 7 III-A3 ICE 0 0

  10. Forest Areas__ Healthy II-A2 II-B1 Burned Depth (cm) 48 II-B1 45 II-B2 Hardness II-B2 III_A1 III-A3 Hardness 24 ICE III-A3 16 III-A3 III-B1 6 III-A3 0

  11. Clearings Healthy 46 II-A2 42.5 Burned Hardness 39 II-B1 II-B1 Hardness 26 19.5 III-A3 II-A2 10 III-A2 6 7 ICE III-B2 0 0

  12. Summary of Results A Healthy Forest Snow cover: • Deep • variety of layers • contains old snow depth hoar present Burned Area’s Snow Cover: • large layers of ice • Snow is dense • No new snow on top layer Same for both: • Temperature gradient

  13. Discussion • What factors are responsible for the types of layers present in? • How do the layers affect one another? • How will the layer distribution affect the movement of animals? • What is happening to the terrain? • What happens to the lifespan of snow cover, and how does that affect the climate?

  14. In Conclusion • Fires have an observable effect on Snow layers. • This changes how the ecosystem is used by local organisms. • Prescribed burning may be degredating the overall health of the mountain ecosystem.

  15. Citations---- • Climatic Change, Wildfire, and Conservation Donald McKenzie, Ze'evGedalof, David L. Peterson and Philip Mote Conservation Biology , Vol. 18, No. 4 (Aug., 2004), pp. 890-902 Published by: Blackwell Publishing for Society for Conservation Biology Article Stable URL: http://www.jstor.org/stable/3589163 • Effect of Snow Depth on Predation and Scavenging by Gray Wolves David J. Huggard The Journal of Wildlife Management , Vol. 57, No. 2 (Apr., 1993), pp. 382-388 Published by: Allen Press Article Stable URL: http://www.jstor.org/stable/3809437 • Multi-Season Climate Synchronized Historical Fires in Dry Forests (1650-1900), Northern Rockies, USA Emily K. Heyerdahl, Penelope Morgan and James P. Riser II Ecology , Vol. 89, No. 3 (Mar., 2008), pp. 705-716 Published by: Ecological Society of America Article Stable URL: http://www.jstor.org/stable/27651593 • Needle Ice Striped Ground J. Ross Mackay and W. H. Mathews Arctic and Alpine Research , Vol. 6, No. 1 (Winter, 1974), pp. 79-84 Published by: INSTAAR, University of Colorado Article Stable URL: http://www.jstor.org/stable/1550372 • Snow Distribution and Heat Flow in the Taiga Matthew Sturm Arctic and Alpine Research , Vol. 24, No. 2 (May, 1992), pp. 145-152 Published by: INSTAAR, University of Colorado Article Stable URL: http://www.jstor.org/stable/1551534 • The Interaction of Fire, Fuels, and Climate across Rocky Mountain Forests TANIA SCHOENNAGEL, THOMAS T. VEBLEN and WILLIAM H. ROMME BioScience , Vol. 54, No. 7 (July 2004), pp. 661-676 Published by: University of California Press on behalf of the American Institute of Biological Sciences Article DOI: 10.1641/0006-3568(2004)054[0661:TIOFFA]2.0.CO;2 Article Stable URL: http://www.jstor.org/stable/10.1641/0006-3568%282004%29054%5B0661%3ATIOFFA%5D2.0.CO%3B2

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