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- Permafrost soils store nearly half of global soil carbon (C), and therefore permafrost thawing could lead to large amounts of greenhouse gas emissions via decomposition of soil organic matter. When ice-rich permafrost thaws, it creates a localized surface subsidence called thermokarst terrain, which changes the soil microenvironment. We used soil profile CO2 measurements to understand the response of belowground C emissions for different soil depths from upland tundra as a result of permafrost thaw and thermokarst development. We established sites in central Alaska, where permafrost thaw...AuthorsHanna Lee, Edward A.G. Schuur, Jason G. VogelKeywordsSourceJournal of Geophysical Research. 115: G01009. DOI: 10.1029/2008JG000906. 11 pYear2010
- Warming in the boreal forest of interior Alaska will have fundamental impacts on stream ecosystems through changes in stream hydrology resulting from upslope loss of permafrost, alteration of availability of soil moisture, and the distribution of vegetation. We examined stream flow in three headwater streams of the Caribou-Poker Creeks Research Watershed (CPCRW) in interior Alaska over a 30-year period to determine (i) how stream flow varied among streams draining watersheds with varying extents of permafrost and (ii) evaluate if stream hydrology is changing with loss of permafrost. The...AuthorsJeremy B. Jones, Amanda J. RinehartKeywordsSourceCanadian Journal of Forest Research. 40: 1210-1218Year2010
- The resilience and vulnerability of permafrost to climate change depends on complex interactions among topography, water, soil, vegetation, and snow, which allow permafrost to persist at mean annual air temperatures (MAATs) as high as +2 °C and degrade at MAATs as low as -20°C. To assess these interactions, we compiled existing data and tested effects of varying conditions on mean annual surface temperatures (MASTs) and 2 m deep temperatures (MADTs) through modeling, Surface water had the largest effect, with water sediment temperatures being ~10 °C above MAAT. A 50% reduction in snow...AuthorsM.Torre Jorgenson, Vladimir Romanovsky, Jennifer Harden, Yuri Shur, Jonathan O'Donnell, Edward A.G. Schuur, Mikhail Kanevskiy, Sergei MarchenkoKeywordsSourceCanadian Journal of Forest Research. 40: 1219-1236Year2010
- The microbial communities of high-latitude ecosystems are expected to experience rapid changes over the next century due to climate warming and increased deposition of reactive nitrogen, changes that will likely affect microbial community structure and function. In moist acidic tundra (MAT) soils on the North Slope of the Brooks Range, Alaska, substantial losses of C and N were previously observed after long-term nutrient additions. To analyse the role of microbial communities in these losses, we utilized 16S rRNA gene tag pyrosequencing coupled with community-level physiological profiling...AuthorsBarbara J. Campbell, Shawn W. Polson, Thomas E. Hanson, Michelle C. Mack, Edward A.G. SchuurSourceEnvironmental Microbiology. 12(7): 1842-1854Year2010
- In the boreal forests of Alaska, recent changes in climate have influenced the exchange of trace gases, water, and energy between these forests and the atmosphere. These changes in the structure and function of boreal forests can then feed back to impact regional and global climates. We examine the type and magnitude of the climate feedbacks from boreal forests in Alaska. Research generally suggests that the net effect of a warming climate is a positive regional feedback to warming. Currently, the primary positive climate feedbacks are likely related to decreases in surface albedo due to...AuthorsE.S. Euskirchen, A.D. McGuire, F.S. Chapin, T.S. RuppKeywordsSourceCanadian Journal of Forest Research. 40: 1336-1346Year2010
- We monitored the short-term (< 3 years) response of land birds to restoration treatments (thin, burn, and thin-burn) in dry forests located on the eastern slope of the Cascade Range in Washington. Overall avian community composition did not change among the treatments. However, individual species responses varied with the chipping sparrow showing lower density in treatments, whereas hermit thrush, mountain chickadee, white-headed woodpecker, western bluebird, American crow, and common raven increased in treatment units. Daily survival rates of nesting guilds were similar in treated versus...AuthorsWilliam Gaines, Maryellen Haggard, James Begley, John F. Lehmkuhl, Andrea LyonsKeywordsSourceForest Science. 56(1): 88-99Year2010
- We examined genetic structure and long-distance gene flow in two lichenized ascomycetes, Flavocetraria cucullata and Flavocetraria nivalis, which are widespread in arctic and alpine tundra. DNA sequences were obtained for 90 specimens (49 for F. cucullata and 41 for F. nivalis) collected from various locations in Europe, Asia and North America. Sequences of the nuclear internal transcribed spacer (ITS) + 5.8S ribosomal subunit gene region were generated for 89 samples, and supplemented by beta-tubulin (BTUB) and translation elongation factor 1-alpha gene (EFl) sequences for a subset of F....AuthorsJózsef Geml, Frank Kauff, Christan Brochmann, D.L. TaylorKeywordsSourceJournal of Biogeography. 37: 1529-1542Year2010
- We assessed the short-term effects of alternative designs of forested buffer treatments along headwater streams on small ground-dwelling mammals in managed forests in western Washington, USA. Over three summers (one pretreatment and two posttreatment), we trapped 19 mammalian species along 23 streams in the northern Coast Range. We compared faunal communities in unlogged controls with riparian treatments: (1) clearcuts (no buffer) to the stream bank, (2) clearcuts with continuous buffer strips from a few to 20 m each streamside, and (3) clearcuts with small patch (AuthorsMartin G. Raphael, Randall Wilk, Christopher S. Nations, Jeffrey D. RicklefsKeywordsSourceForest Ecology and Management. 260: 1567-1578Year2010
- The comparative analysis of a large set of long-term fertilization and thinning studies in the major forest types of interior Alaska is summarized. Results indicate that nutrient limitations may only occur during the early spring growth period, after which moisture availability is the primary control of tree growth on warm sites. The temperature dynamics of both air and soil set seasonal bounds on the nutrient and moisture dynamics for all forest types. Air and soil temperature limitations are the primary control of intraseasonal growth in the colder topographic locations in interior...AuthorsJ. Yarie, K. Van CleveSourceCanadian Journal of Forest Research. 40: 1325-1335Year2010
- Conserving biological diversity in a changing climate poses major challenges for land managers and society. Effective adaptive strategies for dealing with climate change require a socioecological systems perspective. We highlight some of the projected ecological responses to climate change in the Pacific Northwest, U.S.A and identify possible adaptive actions that federal forest managers could take. The forest landscape, ownership patterns and recent shift toward ecologically based forest management provide a good starting place for conserving biological diversity under climate change....AuthorsThomas A. Spies, Thomas W. Giesen, Fred Swanson, Jerry F. Franklin, Denise Lach, K. Norman JohnsonKeywordsSourceLandscape Ecology. 25(8): 1185-1199Year2010