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Displaying 21,741 - 21,750 of 65,202 Publications- Forest degradation can be defined as the loss of forest volume, biomass and/or forest productivity caused by natural or human influences. Achieving Reduced Emissions from Deforestation and Forest Degradation (REDD+) requires that deforestation and degradation can be efficiently, reliably, and cost-effectively detected and quantified, often where ground and aerial surveying is problematic. Therefore, remote sensing approaches, coupled with field and/or aerial data, offer possible solutions and efficiencies. While synoptic coverage using high-resolution data such as Landsat can provide...AuthorsDouglas Muchoney, Sharon HamannSourceIn: Mortenson, Leif A.; Halperin, James J.; Manley, Patricia N.; Turner, Rich L., eds. Proceedings of the international workshop on monitoring forest degradation in Southeast Asia. Gen. Tech. Rep. PSW-GTR-246. Albany, CA: U.S. Department of Agriculture, Forest Service, Pacific Southwest Research Station: p. 16Year2013
- Globally, approximately two-thirds of the world's forests are considered degraded, but practical, cost-effective tools for monitoring forest quality remain elusive. Techniques for monitoring deforestation and changes to forest carbon stocks are widespread and well published. However, techniques for monitoring forest degradation are relatively untested in developing countries despite their inclusion in the United Nations Framework Convention on Climate Change (UNFCCC) negotiations on Reducing Emissions from Deforestation and Forest Degradation (REDD+). The lack of a forest degradation...AuthorsJames Halperin, David GanzSourceIn: Mortenson, Leif A.; Halperin, James J.; Manley, Patricia N.; Turner, Rich L., eds. Proceedings of the international workshop on monitoring forest degradation in Southeast Asia. Gen. Tech. Rep. PSW-GTR-246. Albany, CA: U.S. Department of Agriculture, Forest Service, Pacific Southwest Research Station: 1-3Year2013
- Aims The spatial distribution of biotic and abiotic factors may play a dominant role in determining the distribution and abundance of plants in arid and semiarid environments. In this study, we evaluated how spatial patterns of microhabitat variables and the degree of spatial dependence of these variables influence the distribution and abundance of the endangered cactus Harrisia portoricensis. Methods We used geostatistical analyses of five microhabitat variables (e.g. vegetation cover, soil cover and light incidence) and recorded the abundance of H. portoricensis in 50 permanent plots...AuthorsJ. Rojas-Sandoval, E. J. Melendez-Ackerman, NO-VALUEKeywordsSourceJournal of Plant Ecology: doi: 10.1093/jpe/rtt1014.Year2013
- Nitrogen deposition, along with habitat losses and climate change, has been identified as a primary threat to biodiversity worldwide (Butchart et al., 2010; MEA, 2005; Sala et al., 2000). The source of this stressor to natural systems is generally twofold: burning of fossil fuels and the use of fertilizers in modern intensive agriculture. Each of these human enterprises leads to the release of large amounts of biologically reactive nitrogen (henceforth contracted to "nitrogen") to the atmosphere, which is later deposited to ecosystems. Because nitrogen is a critical element to all living...AuthorsChristopher M. Clark, Yongfei Bai, William D. Bowman, Jane M. Cowles, Mark E. Fenn, Frank S. Gilliam, Gareth K. Phoenix, Ilyas Siddique, Carly J. Stevens, Harald U. Sverdrup, Heather L. ThroopSourceIn: Levin S.A. (ed.) Encyclopedia of Biodiversity, second edition, Volume 5, Waltham, MA: Academic Press. pp. 519-536Year2013
- Industrial nitrogen (N) emissions in the Athabasca oil sands region (AOSR), Alberta, Canada, affect nitrate (NO3) and ammonium (NH4) deposition rates in close vicinity of industrial emitters. NO3-N and NH4-N open field and throughfall deposition rates were determined at various sites between 3 km and 113 km distance to the main oil sand operations between May 2008 and May 2009. NO3 and NH4 were analyzed for δ15N-NO3, δ18O-NO3, Δ17O-NO3 and δ15N-NH4. Marked differences in the δ18O and Δ17O values between industrial emissions and background deposition allowed for the estimation of minimum...AuthorsBernadette C. Proemse, Bernhard Mayer, Mark E. Fenn, Christopher RossKeywordsSourceEnvironmental Pollution. 182: 80-91Year2013
- Raster modeling is an integral component of spatial analysis. However, conventional raster modeling techniques can require a substantial amount of processing time and storage space, often limiting the types of analyses that can be performed. To address this issue, we have developed Function Modeling. Function Modeling is a new modeling framework that streamlines the raster modeling process by utilizing lazy reading methodologies. To assess the efficacy of Function Modeling, we compared the processing time and storage space required to execute six simulation using our newly developed...AuthorsJohn S. Hogland, Nathaniel Anderson, Greg G. JonesKeywordsSourceIn: Proceedings of the 36th Annual Meeting of the Council on Forest Engineering; July 8-10, 2013, Missoula, MT. Morgantown, WV: Council on Forest Engineering. Online: http://web1.cnre.vt.edu/forestry/cofe/documents/2013/Hogland_Anderson_Jones.pdfYear2013
- Climate change is predicted to increase both drought frequency and duration, and when coupled with substantial warming, will establish a new hydroclimatological model for many regions1. Largescale, warm droughts have recently occurred in North America, Africa, Europe, Amazonia and Australia, resulting in major effects on terrestrial ecosystems, carbon balance and food security2,3. Here we compare the functional response of above-ground net primary production to contrasting hydroclimatic periods in the late twentieth century (1975–1998), and drier, warmer conditions in the early twenty-first...AuthorsG. E. Ponce Campos, M. S. Moran, A. Huete, Y. Zhang, C. Bresloff, T.E. Huxman, D. Eamus, D. D. Bosch, A. R. Buda, S. A. Gunter, Tamara Heartsill Scalley, S. G. Kitchen, M. P. McClaran, Henry McNab, Diane Sutherland, J. A. Morgan, D. P. C. Peters, E. J. Sadler, M. S. Seyfried, P. J. StarksSourceNature 494:349 - 353.Year2013
- AuthorsB. A. Richardson, M. J. Richardson, NO-VALUESourcePages 101-116 in G. González, M. R. Willig, and R. B. Waide, editors. Ecological gradient analyses in a tropical landscape. Ecological Bulletins 54. Wiley-Blackwell, Hoboken, NJ.Year2013
- Wet,dry and throughfall deposition of N and S were measured for 2 years in three national parks in Washington State:Olympic,Mount Rainier,and North Cascades.Throughfall was measured using ion exchange resin (IER) collectors. A major objective of the study was to evaluate the effectiveness of IER throughfall measurements for monitoring deposition inputs,including cloudwater deposition, to forest stands in national parks and other protected areas. Wet deposition (0.9–2.0kgN-1ha-1yr)and throughfall (0.5–1.2kgN-1ha-1yr) deposition of inorganic N in the three parks were relatively low. Wet...AuthorsMark E. Fenn, Christopher Ross, Susan L. Schilling, William D. Baccus, Michael A. Larrabee, Rebecca A. LofgrenKeywordsSourceFor. Ecol. Manage. 302: 240-253Year2013
- Where a legacy of aggressive wildland fire suppression has left forests in need of fuel reduction, allowing wildland fire to burn may provide fuel treatment benefits, thereby reducing suppression costs from subsequent fires. The least-cost-plus-net-value-change model of wildland fire economics includes benefits of wildfire in a framework for evaluating suppression options. In this study, we estimated one component of that benefit the expected present value of the reduction in suppression costs for subsequent fires arising from the fuel treatment effect of a current fire. To that end, we...AuthorsRachel M. Houtman, Claire A. Montgomery, Aaron R. Gagnon, Dave E. Calkin, Thomas G. Dietterich, Sean McGregor, Mark CrowleySourceInternational Journal of Wildland Fire. doi: http://dx.doi.org/10.1071/WF12157Year2013