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Climate & Land Use

Changing land use is placing increasing pressure on wildlife resources and requires more complicated analyses to identify potential consequences and trade-offs of management alternatives. Couple that with global climate change, and resource managers face unprecedented challenges in the management of natural resources. NOROCK works with managers in the northern Rockies and elsewhere to evaluate these changes and predict their impacts on terrestrial and aquatic ecosystems.  

Filter Total Items: 42

Evaluating the linkages between regional climate patterns, local climate data, and native Yellowstone cutthroat trout (Oncorhynchus clarkii bouvieri) and non-native brook trout (Salvelinus fontinalis) growth, survival, and life-history expressions.

Beyond large-scale climate models, it is becoming increasingly important to quantify how regional climate patterns link with in situ stream temperatures and hydrologic regimes and concomitantly, fish behavior, growth, and survival. Here, we are using comprehensive mark-recapture techniques to evaluate how changing climatic conditions are likely to influence native westslope cutthroat trout and non...
Evaluating the linkages between regional climate patterns, local climate data, and native Yellowstone cutthroat trout (Oncorhynchus clarkii bouvieri) and non-native brook trout (Salvelinus fontinalis) growth, survival, and life-history expressions.

Evaluating the linkages between regional climate patterns, local climate data, and native Yellowstone cutthroat trout (Oncorhynchus clarkii bouvieri) and non-native brook trout (Salvelinus fontinalis) growth, survival, and life-history expressions.

Beyond large-scale climate models, it is becoming increasingly important to quantify how regional climate patterns link with in situ stream temperatures and hydrologic regimes and concomitantly, fish behavior, growth, and survival. Here, we are using comprehensive mark-recapture techniques to evaluate how changing climatic conditions are likely to influence native westslope cutthroat trout and non...
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Forecasting the effects of climate change on the interactions of native and non-native salmonids

Changes in temperature and precipitation patterns under global climate change are expected to expand the range of suitable habitat for non-natives within stream networks, resulting in significant increases in the distribution and abundance of non-natives. However, our understanding of how landscape attributes can affect local thermal and hydrologic patterns suggests that changes in global climate...
Forecasting the effects of climate change on the interactions of native and non-native salmonids

Forecasting the effects of climate change on the interactions of native and non-native salmonids

Changes in temperature and precipitation patterns under global climate change are expected to expand the range of suitable habitat for non-natives within stream networks, resulting in significant increases in the distribution and abundance of non-natives. However, our understanding of how landscape attributes can affect local thermal and hydrologic patterns suggests that changes in global climate...
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Evaluating the reintroduction potential and limiting factors associated with anadromous fish reintroductions in the Upper Lewis River, WA

Hydropower facilities on the Lewis River, WA eliminated historic runs of anadromous species to the headwaters of the Lewis River. As anadromous reintroductions are considered and implemented, there remains considerable uncertainty in the viability of reintroductions in reservoir and tributary systems where large populations of non-native species persist and where spawning and rearing habitat may...
Evaluating the reintroduction potential and limiting factors associated with anadromous fish reintroductions in the Upper Lewis River, WA

Evaluating the reintroduction potential and limiting factors associated with anadromous fish reintroductions in the Upper Lewis River, WA

Hydropower facilities on the Lewis River, WA eliminated historic runs of anadromous species to the headwaters of the Lewis River. As anadromous reintroductions are considered and implemented, there remains considerable uncertainty in the viability of reintroductions in reservoir and tributary systems where large populations of non-native species persist and where spawning and rearing habitat may...
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Design, Analysis, Monitoring, and Conservation of Ecological Dynamics at Broad Scales

There is increasing recognition that the spatial context in which any ecological process or phenomenon occurs has great bearing on the outcome of that process. Since 1994, we have been working on numerous field investigations and conceptual developments to inform how ecological resources can be managed and conserved across jurisdictional boundaries and broad spatial extents. Because such spatially...
Design, Analysis, Monitoring, and Conservation of Ecological Dynamics at Broad Scales

Design, Analysis, Monitoring, and Conservation of Ecological Dynamics at Broad Scales

There is increasing recognition that the spatial context in which any ecological process or phenomenon occurs has great bearing on the outcome of that process. Since 1994, we have been working on numerous field investigations and conceptual developments to inform how ecological resources can be managed and conserved across jurisdictional boundaries and broad spatial extents. Because such spatially...
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Species and Ecosystem Responses to Global Change

We work with a diverse collection of researchers, resource managers, and conservation practitioners to address the “how” and “why” questions that underlie species-and ecosystem-level responses to long-term weather patterns. Although it is more challenging, this level of more-mechanistic understanding is critical for informing climate-adaptation actions and strategies. We use a diversity of study...
Species and Ecosystem Responses to Global Change

Species and Ecosystem Responses to Global Change

We work with a diverse collection of researchers, resource managers, and conservation practitioners to address the “how” and “why” questions that underlie species-and ecosystem-level responses to long-term weather patterns. Although it is more challenging, this level of more-mechanistic understanding is critical for informing climate-adaptation actions and strategies. We use a diversity of study...
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Gigapixel Imagery of Glacier National Park

View and dynamically explore high resolution gigapixel images of Glacier National Park with GigaPan panoramas taken by CCME staff. This collection of images serves as landscape documentation and as an interactive forum for public exploration of Glacier National Park’s changing landscapes. Search “ccme” at http://gigapan.org By accessing these links you are leaving a U.S. Department of Interior...
Gigapixel Imagery of Glacier National Park

Gigapixel Imagery of Glacier National Park

View and dynamically explore high resolution gigapixel images of Glacier National Park with GigaPan panoramas taken by CCME staff. This collection of images serves as landscape documentation and as an interactive forum for public exploration of Glacier National Park’s changing landscapes. Search “ccme” at http://gigapan.org By accessing these links you are leaving a U.S. Department of Interior...
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Repeat Photography Project

Repeat photography provides objective visual evidence of landscape change. USGS scientists created approximately sixty repeat photography pairs that document glacier change in Glacier National Park. These photograph pairs are available as a collection hosted by the USGS Photographic Library and are publicly available for download. Modern (1997 to 2019) photographs were taken from precisely the...
Repeat Photography Project

Repeat Photography Project

Repeat photography provides objective visual evidence of landscape change. USGS scientists created approximately sixty repeat photography pairs that document glacier change in Glacier National Park. These photograph pairs are available as a collection hosted by the USGS Photographic Library and are publicly available for download. Modern (1997 to 2019) photographs were taken from precisely the...
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Brief History of Glaciers in Glacier National Park

The history of glaciation in Glacier National Park spans thousands of years of glacial growth and recession, carving the steep and striking mountain features we see today. Glaciers have been present within the boundaries of present-day Glacier National Park since as early as 6,500 years ago (Munroe and others, 2012). These modest glaciers varied in size, tracking climatic trends, but did not grow...
Brief History of Glaciers in Glacier National Park

Brief History of Glaciers in Glacier National Park

The history of glaciation in Glacier National Park spans thousands of years of glacial growth and recession, carving the steep and striking mountain features we see today. Glaciers have been present within the boundaries of present-day Glacier National Park since as early as 6,500 years ago (Munroe and others, 2012). These modest glaciers varied in size, tracking climatic trends, but did not grow...
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Status of Glaciers in Glacier National Park

Glaciers on the Glacier National Park (GNP) landscape have ecological value as a source of cold meltwater in the otherwise dry late summer months, and aesthetic value as the park’s namesake features. USGS scientists have studied these glaciers since the late 1800s, building a body of research that documents widespread glacier change over the past century. Ongoing USGS research pairs long-term data...
Status of Glaciers in Glacier National Park

Status of Glaciers in Glacier National Park

Glaciers on the Glacier National Park (GNP) landscape have ecological value as a source of cold meltwater in the otherwise dry late summer months, and aesthetic value as the park’s namesake features. USGS scientists have studied these glaciers since the late 1800s, building a body of research that documents widespread glacier change over the past century. Ongoing USGS research pairs long-term data...
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Alpine Climatology of Glacier National Park

Glacier National Park is a topographically diverse region, making localized effects of elevation, aspect, and cold air drainage several of many important factors that necessitate a diversity of long-term climate monitoring sites. Additionally, many studies have shown more rapid warming at higher elevations across the Intermountain West, but with relatively few high-elevation stations available in...
Alpine Climatology of Glacier National Park

Alpine Climatology of Glacier National Park

Glacier National Park is a topographically diverse region, making localized effects of elevation, aspect, and cold air drainage several of many important factors that necessitate a diversity of long-term climate monitoring sites. Additionally, many studies have shown more rapid warming at higher elevations across the Intermountain West, but with relatively few high-elevation stations available in...
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Snow and Avalanche Research

Snow scientists with the USGS are unraveling specific weather, climate, and snowpack factors that contribute to large magnitude avalanches in an effort to understand these events as both a hazard and a landscape–level disturbance. The Snow and Avalanche Project (SNAP) advances our understanding of avalanche-climate interactions and wet snow avalanches, and improves public safety through innovative...
Snow and Avalanche Research

Snow and Avalanche Research

Snow scientists with the USGS are unraveling specific weather, climate, and snowpack factors that contribute to large magnitude avalanches in an effort to understand these events as both a hazard and a landscape–level disturbance. The Snow and Avalanche Project (SNAP) advances our understanding of avalanche-climate interactions and wet snow avalanches, and improves public safety through innovative...
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Secondary Glacier Network

The Secondary Glacier Network includes six glaciers (Chaney, Grinnell, Stanton, Agassiz, Swiftcurrent, Jackson-Blackfoot Glaciers) that form a north-south transect of approx. 60 km through the region, with Sperry Glacier just south of center. While these glaciers will be monitored less frequently than the benchmark glacier, Sperry, this network will provide data about the variability of processes...
Secondary Glacier Network

Secondary Glacier Network

The Secondary Glacier Network includes six glaciers (Chaney, Grinnell, Stanton, Agassiz, Swiftcurrent, Jackson-Blackfoot Glaciers) that form a north-south transect of approx. 60 km through the region, with Sperry Glacier just south of center. While these glaciers will be monitored less frequently than the benchmark glacier, Sperry, this network will provide data about the variability of processes...
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