GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • Blackwell Publishing Ltd  (3)
  • Cham :Springer International Publishing AG,  (1)
  • 1
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Climatic changes. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (246 pages)
    Edition: 1st ed.
    ISBN: 9783319569284
    Series Statement: Advances in Global Change Research Series ; v.63
    Language: English
    Note: Intro -- Dedication -- Foreword -- Preface -- Acknowledgments -- Contents -- Contributors -- Chapter 1: Assessing Climate Change Effects in the Northern Rockies -- 1.1 Introduction -- 1.2 Northern Rockies Adaptation Partnership Process -- 1.3 Toward Implementation of Climate-Smart Management -- 1.4 A Brief Tour of the Northern Rockies -- 1.4.1 Western Rockies Subregion -- 1.4.2 Central Rockies Subregion -- 1.4.3 Eastern Rockies Subregion -- 1.4.4 Greater Yellowstone Area Subregion -- 1.4.5 Grassland Subregion -- References -- Chapter 2: Historical and Projected Climate in the Northern Rockies Region -- 2.1 Introduction -- 2.2 Climate Model Overview -- 2.3 Methods Used to Assess Future Climate in the Northern Rockies Region -- 2.4 Projected Future Climate in the Northern Rockies -- References -- Chapter 3: Effects of Climate Change on Snowpack, Glaciers, and Water Resources in the Northern Rockies -- 3.1 Introduction -- 3.2 Mechanisms for Climate Change Effects on Hydrology -- 3.3 Effects of Climate Change on Snowpack and Glaciers -- 3.4 Effects of Climate Change on Streamflow -- 3.4.1 Future Streamflow Projections -- 3.5 Adapting Water Resources and Management to Climate Change -- References -- Chapter 4: Effects of Climate Change on Cold-Water Fish in the Northern Rockies -- 4.1 Introduction -- 4.2 Analytical Approach -- 4.2.1 Assessment Area -- 4.2.2 Climate Change Scenarios -- 4.2.3 Fish Species -- 4.2.4 Trout Distribution Models -- 4.3 Vulnerability of Native Trout to Climate Change -- 4.3.1 Stream Temperature -- 4.3.2 Cutthroat Trout -- 4.3.3 Bull Trout -- 4.3.4 Additional Fish Species -- 4.4 Applying the Assessment -- 4.5 Adapting Fish Species and Fisheries Management to Climate Change -- 4.5.1 Adaptation Options -- 4.5.2 Principles of Climate-Smart Management -- References. , Chapter 5: Effects of Climate Change on Forest Vegetation in the Northern Rockies -- 5.1 Introduction -- 5.1.1 Climate Change Assessment Techniques -- 5.1.2 Forest Vegetation Responses to Climate -- 5.1.3 Biotic and Abiotic Disturbances -- 5.2 Climate Change Effects on Tree Species -- 5.2.1 Ponderosa Pine (Pinus ponderosa) -- 5.2.2 Douglas-Fir (Pseudotsuga menziesii) -- 5.2.3 Western Larch (Larix occidentalis) -- 5.2.4 Western White Pine (Pinus monticola) -- 5.2.5 Grand Fir (Abies grandis) -- 5.2.6 Western Redcedar (Thuja plicata) -- 5.2.7 Western Hemlock (Tsuga heterophylla) -- 5.2.8 Lodgepole Pine (Pinus contorta var. latifolia) -- 5.2.9 Limber Pine (Pinus flexilis) -- 5.2.10 Subalpine Fir (Abies lasiocarpa) -- 5.2.11 Engelmann Spruce (Picea engelmannii) -- 5.2.12 Mountain Hemlock (Tsuga mertensiana) -- 5.2.13 Alpine Larch (Larix lyallii) -- 5.2.14 Whitebark Pine (Pinus albicaulis) -- 5.2.15 Quaking Aspen (Populus tremuloides) -- 5.2.16 Cottonwood (Populus spp.) -- 5.2.17 Green Ash (Fraxinus pennsylvanica) -- 5.3 Effects of Climate Change on Broader Vegetation Patterns -- 5.4 Natural Resource Issues and Management -- 5.4.1 Landscape Heterogeneity -- 5.4.2 Timber Production -- 5.4.3 Carbon Sequestration -- 5.5 Adapting Forest Vegetation and Management to Climate Change -- 5.5.1 Adaptation Strategies and Tactics -- References -- Chapter 6: Effects of Climate Change on Rangeland Vegetation in the Northern Rockies -- 6.1 Introduction -- 6.2 Rangeland Vegetation -- 6.3 Management Issues -- 6.4 Assessing the Effects of Climate Change on Rangelands -- 6.4.1 Montane Grasslands -- 6.4.2 Montane Shrubs -- 6.4.3 Short Sagebrushes -- 6.4.4 Sprouting Sagebrush Species -- 6.4.5 Wyoming Big Sagebrush and Basin Big Sagebrush -- 6.4.6 Mountain Big Sagebrush -- 6.4.7 Northern Great Plains -- 6.5 Adapting Rangeland Vegetation and Management to Climate Change. , References -- Chapter 7: Effects of Climate Change on Ecological Disturbance in the Northern Rockies -- 7.1 Introduction -- 7.2 Wildfire -- 7.2.1 Overview -- 7.2.2 Potential Future Wildfire Regimes and Wildfire Occurrence -- 7.2.3 Potential Interactions Between Wildfire and Other Disturbances -- 7.3 Bark Beetles -- 7.3.1 Overview -- 7.3.2 Drivers of Bark Beetle Outbreaks -- 7.3.3 Potential Effects of Climate Change on Bark Beetles -- 7.3.4 Projected Effects of Climate Change on Bark Beetle Populations -- 7.4 White Pine Blister Rust -- 7.4.1 Overview -- 7.4.2 Effects of Climate Change on WPBR -- 7.4.3 Interactions with Other Disturbance Processes -- 7.5 Forest Diseases -- 7.5.1 Overview -- 7.5.2 Effects of Climatic Variability and Change on Forest Diseases -- 7.5.3 Forest Pathogen Interactions -- 7.6 Nonnative Plants -- 7.6.1 Overview -- 7.6.2 Effects of Climate Change on Nonnative Species -- References -- Chapter 8: Effects of Climate Change on Wildlife in the Northern Rockies -- 8.1 Climate-Wildlife Interactions -- 8.2 Communities and Habitat -- 8.3 Species Sensitivity to Climate Change -- 8.3.1 American Beaver (Castor canadensis) -- 8.3.2 American Pika (Ochotona princeps) -- 8.3.3 Canada Lynx (Lynx canadensis) -- 8.3.4 Fisher (Pekania pennanti) -- 8.3.5 Moose (Alces alces) -- 8.3.6 Northern Bog Lemming (Synaptomys borealis) -- 8.3.7 Pronghorn (Antilocapra americana) -- 8.3.8 Pygmy Rabbit (Brachylagus idahoensis) -- 8.3.9 Townsend's Big-Eared Bat (Corynorhinus townsendii) -- 8.3.10 Ungulates (Elk, Mule Deer, White-Tailed Deer) -- 8.3.11 Wolverine (Gulo gulo) -- 8.3.12 Brewer's Sparrow (Spizella breweri) -- 8.3.13 Flammulated Owl (Otus flammeolus) -- 8.3.14 Greater Sage-Grouse (Centrocercus urophasianus) -- 8.3.15 Harlequin Duck (Histrionicus histrionicus) -- 8.3.16 Mountain Quail (Oreortyx pictus) -- 8.3.17 Pygmy Nuthatch (Sitta pygmaea). , 8.3.18 Ruffed Grouse (Bonasa umbellus) -- 8.3.19 Columbia Spotted Frog (Rana luteiventris) -- 8.3.20 Western Toad (Anaxyrus boreas) -- 8.4 Adapting Wildlife and Wildlife Management to Climate Change -- References -- Chapter 9: Effects of Climate Change on Recreation in the Northern Rockies -- 9.1 Introduction -- 9.2 Relationships Between Climate Change and Recreation -- 9.3 Outdoor Recreation in the Northern Rockies -- 9.4 Assessing the Vulnerability of Recreation to Climate Change -- 9.4.1 Current Conditions and Management -- 9.4.2 Warm-Weather Activities -- 9.4.3 Cold-Weather Activities -- 9.4.4 Wildlife Activities -- 9.4.5 Gathering Forest Products -- 9.4.6 Water-Based Activities (Not Including Fishing) -- 9.4.7 Summary -- 9.5 Adapting Recreation and Recreation Management to Climate Change -- 9.5.1 Adaptation by Recreation Participants -- 9.5.2 Adaptation by Federal Land Management -- References -- Chapter 10: Effects of Climate Change on Ecosystem Services in the Northern Rockies -- 10.1 Introduction -- 10.2 Ecosystem Services on Public Lands in the Northern Rockies -- 10.3 Social Vulnerability and Adaptive Capacity -- 10.4 Assessing the Effects of Climate Change on Ecosystem Services -- 10.4.1 Water Quantity -- 10.4.2 Water Quality, Aquatic Habitats, and Fish -- 10.4.3 Building Materials and Wood Products -- 10.4.4 Mining Materials -- 10.4.5 Forage for Livestock -- 10.4.6 Viewsheds and Clean Air -- 10.4.7 Regulation of Soil Erosion -- 10.4.8 Carbon Sequestration -- 10.4.9 Summary -- References -- Chapter 11: Effects of Climate Change on Cultural Resources in the Northern Rockies -- 11.1 Background and Cultural Context -- 11.2 Climate Change Effects on Cultural Resources -- 11.2.1 Primary Effects and Stressors -- 11.2.2 Spatial and Temporal Risk Assessment -- 11.3 Adapting Cultural Resources and Management to Climate Change -- References. , Chapter 12: Toward Climate-Smart Resource Management in the Northern Rockies -- 12.1 Partnership and Process -- 12.1.1 Increasing Organizational Capacity to Address Climate Change -- 12.1.2 Implementation: The Path Forward -- References -- Index.
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Global change biology 1 (1995), S. 0 
    ISSN: 1365-2486
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering , Geography
    Notes: Growth response of subalpine fir (Abies lasiocarpa) to climate was studied across its local geographical and elevation range in the Olympic Mountains, Washington. A dendroecological analysis of subalpine fir across a range of elevations (1350-1850 m) and annual precipitation (125-350 cm y−1), was used to compare environmental factors affecting growth. Climate-growth relationships were explored using Pearson product-moment correlation coefficients; partial correlation analysis was used to assess relationships among site chronologies and climatic variables. Radial growth is negatively correlated with winter precipitation at high elevation and wet sites, but not at low and middle elevation dry sites. Growth is positively correlated with current growing season temperature at all sites; however, growth is negatively correlated with previous year August temperature, indicating that climate affects growth in subsequent years. Positive correlations between growth and summer precipitation during the growing season at low and middle elevation dry sites suggest that soil moisture is partially limiting to growth on these sites. If the climate of the Pacific Northwest becomes warmer and drier, then subalpine fir growth may increase at high elevation and wet sites, but may decrease at lower elevation dry sites in the Olympic Mountains. However, the growth response of subalpine fir to potentially rapid climate change will not be uniform because subalpine fir grows over a wide range of topographic features, habitats, and local climates at different geographical scales. A comparison of growth response to current growing season temperature suggests that the temperature-related growth response of subalpine fir is not adequately described by the parabolic curve used in JABOWA-based models.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Global change biology 1 (1995), S. 0 
    ISSN: 1365-2486
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering , Geography
    Notes: Dendroecological techniques were used to describe the variation in growth response of subalpine fir (Abies lasiocarpa)to climate across a range of elevations (1350–1850 m) and annual precipitation (125–350 cm y−1) in the Olympic Mountains, Washington. Correlation analysis is used to describe individual growth-climate relationships. Growth response is quantified in years with unusually warmer, colder, wetter, and drier climates during the period 1895–1990. Combinations of climatic variables that result in unusually fast or slow growth years are also described. Differences in growth-climate relationships among sites, and among individuals from the same site, emphasize within-species variability in response to climate. Growth was not significantly faster or slower on the majority of sites for extreme climate years examined. Few climate variables are correlated with growth of the majority of individuals on most sites, suggesting that some individuals are relatively unresponsive to climate. Individual growth-climate correlations also indicate an increase in the percentage of individuals whose growth is significantly correlated with a climate variable, as the value of the mean site growth correlation increases for that climate variable. Individual differences in growth-climate relationships probably result from microsite variation (soil depth, soil moisture, wind, insolation) and from individual genetic differences. Descriptions of tree species response to climate change need to incorporate both individual and site variation in growth response to climate in order to accurately represent existing environmental heterogeneity.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Journal of the American Water Resources Association 40 (2004), S. 0 
    ISSN: 1752-1688
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Architecture, Civil Engineering, Surveying , Geography
    Notes: : A network of 32 drought sensitive tree-ring chronologies is used to reconstruct mean water year flow on the Columbia River at The Dalles, Oregon, since 1750. The reconstruction explains 30 percent of the variability in mean water year (October to September) flow, with a large portion of unexplained variance caused by underestimates of the most severe low flow events. Residual statistics from the tree-ring reconstruction, as well as an identically specified instrumental reconstruction, exhibit positive trends over time. This finding suggests that the relationship between drought and streamflow has changed over time, supporting results from hydrologic models, which suggest that changes in land cover over the 20th Century have had measurable impacts on runoff production. Low pass filtering the flow record suggests that persistent low flows during the 1840s were probably the most severe of the past 250 years, but that flows during the 1930s were nearly as extreme. The period from 1950 to 1987 is anomalous in the context of this record for having no notable multiyear drought events. A comparison of the flow reconstruction to paleorecords of the Pacific Decadal Oscillation (PDO) and El Nino/Southern Oscillation (ENSO) support a strong 20th Century link between large scale circulation and streamflow, but suggests that this link is very weak prior to 1900.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...