Publications
USGS research activities relevant to Alaska have yielded more than 9400 historical publications. This page features some of the most recent newsworthy research findings.
Filter Total Items: 3084
Conceptual data modeling of wildlife response indicators to ecosystem change in the Arctic Conceptual data modeling of wildlife response indicators to ecosystem change in the Arctic
Large research studies are often challenged to effectively expose and document the types of information being collected and the reasons for data collection across what are often a diverse cadre of investigators of differing disciplines. We applied concepts from the field of information or data modeling to the U.S. Geological Survey (USGS) Changing Arctic Ecosystems (CAE) initiative to...
Authors
Dennis H. Walworth, John M. Pearce
Landscape and local effects on occupancy and densities of an endangered wood-warbler in an urbanizing landscape Landscape and local effects on occupancy and densities of an endangered wood-warbler in an urbanizing landscape
Context Golden-cheeked warblers (Setophaga chrysoparia), an endangered wood-warbler, breed exclusively in woodlands co-dominated by Ashe juniper (Juniperus ashei) in central Texas. Their breeding range is becoming increasingly urbanized and habitat loss and fragmentation are a main threat to the species’ viability. Objectives We investigated the effects of remotely sensed local habitat...
Authors
Jennifer Reidy, Frank R. Thompson III, Courtney L. Amundson, Lisa O’Donnell
Potential for real‐time understanding of coupled hydrologic and biogeochemical processes in stream ecosystems: Future integration of telemetered data with process models for glacial meltwater streams Potential for real‐time understanding of coupled hydrologic and biogeochemical processes in stream ecosystems: Future integration of telemetered data with process models for glacial meltwater streams
While continuous monitoring of streamflow and temperature has been common for some time, there is great potential to expand continuous monitoring to include water quality parameters such as nutrients, turbidity, oxygen, and dissolved organic material. In many systems, distinguishing between watershed and stream ecosystem controls can be challenging. The usefulness of such monitoring can...
Authors
Diane M. McKnight, Karen D. Cozzetto, James D. S. Cullis, Michael N. Gooseff, Christopher Jaros, Joshua C. Koch, W. Berry Lyons, Roseanna M. Neupauer, Adam N. Wlostowski
Geologic framework of the Alaska Peninsula, southwest Alaska, and the Alaska Peninsula terrane Geologic framework of the Alaska Peninsula, southwest Alaska, and the Alaska Peninsula terrane
The Alaska Peninsula is composed of the late Paleozoic to Quaternary sedimentary, igneous, and minor metamorphic rocks that record the history of a number of magmatic arcs. These magmatic arcs include an unnamed Late Triassic(?) and Early Jurassic island arc, the early Cenozoic Meshik arc, and the late Cenozoic Aleutian arc. Also found on the Alaska Peninsula is one of the most complete
Authors
Frederic H. Wilson, Robert L. Detterman, Gregory D. DuBois
Surface melt dominates Alaska glacier mass balance Surface melt dominates Alaska glacier mass balance
Mountain glaciers comprise a small and widely distributed fraction of the world's terrestrial ice, yet their rapid losses presently drive a large percentage of the cryosphere's contribution to sea level rise. Regional mass balance assessments are challenging over large glacier populations due to remote and rugged geography, variable response of individual glaciers to climate change, and...
Authors
Larsen Chris F, E Burgess, A.A. Arendt, Shad O’Neel, A. J. Johnson, C. Kienholz
USGS Arctic Science Strategy USGS Arctic Science Strategy
The United States is one of eight Arctic nations responsible for the stewardship of a polar region undergoing dramatic environmental, social, and economic changes. Although warming and cooling cycles have occurred over millennia in the Arctic region, the current warming trend is unlike anything recorded previously and is affecting the region faster than any other place on Earth, bringing...
Authors
Mark Shasby, Durelle Smith
User’s guide to the North Pacific Pelagic Seabird Database 2.0 User’s guide to the North Pacific Pelagic Seabird Database 2.0
The North Pacific Pelagic Seabird Database (NPPSD) was created in 2005 to consolidate data on the oceanic distribution of marine bird species in the North Pacific. Most of these data were collected on surveys by counting species within defined areas and at known locations (that is, on strip transects). The NPPSD also contains observations of other bird species and marine mammals. The...
Authors
Gary S. Drew, John F. Piatt, Martin Renner
Estimating the abundance of the Southern Hudson Bay polar bear subpopulation with aerial surveys Estimating the abundance of the Southern Hudson Bay polar bear subpopulation with aerial surveys
The Southern Hudson Bay (SH) polar bear subpopulation occurs at the southern extent of the species’ range. Although capture–recapture studies indicate abundance was likely unchanged between 1986 and 2005, declines in body condition and survival occurred during the period, possibly foreshadowing a future decrease in abundance. To obtain a current estimate of abundance, we conducted a...
Authors
Martyn E. Obbard, Seth P. Stapleton, Kevin R. Middel, Isabelle Thibault, Vincent Brodeur, Charles Jutras
Monitoring population status of sea otters (Enhydra lutris) in Glacier Bay National Park and Preserve, Alaska: options and considerations Monitoring population status of sea otters (Enhydra lutris) in Glacier Bay National Park and Preserve, Alaska: options and considerations
After many decades of absence from southeast Alaska, sea otters (Enhydra lutris) are recolonizing parts of their former range, including Glacier Bay, Alaska. Sea otters are well known for structuring nearshore ecosystems and causing community-level changes such as increases in kelp abundance and changes in the size and number of other consumers. Monitoring population status of sea otters...
Authors
George G. Esslinger, Daniel Esler, S. Howlin, L.A. Starcevich
Summer declines in activity and body temperature offer polar bears limited energy savings Summer declines in activity and body temperature offer polar bears limited energy savings
Polar bears (Ursus maritimus) summer on the sea ice or, where it melts, on shore. Although the physiology of “ice” bears in summer is unknown, “shore” bears purportedly minimize energy losses by entering a hibernation-like state when deprived of food. Such a strategy could partially compensate for the loss of on-ice foraging opportunities caused by climate change. However, here we report...
Authors
J.P. Whiteman, H.J. Harlow, George M. Durner, R. Anderson-Sprecher, Shannon E. Albeke, Eric V. Regehr, Steven C. Amstrup, M. Ben-David
Soil surface organic layers in Arctic Alaska: spatial distribution, rates of formation, and microclimatic effects Soil surface organic layers in Arctic Alaska: spatial distribution, rates of formation, and microclimatic effects
Organic layers of living and dead vegetation cover the ground surface in many permafrost landscapes and play important roles in ecosystem processes. These soil surface organic layers (SSOLs) store large amounts of carbon and buffer the underlying permafrost and its contained carbon from changes in aboveground climate. Understanding the dynamics of SSOLs is a prerequisite for predicting...
Authors
Carson Baughman, Daniel H. Mann, David L. Verbyla, Michael L. Kunz
Tectonic and sedimentary linkages between the Belt-Purcell basin and southwestern Laurentia during the Mesoproterozoic ca. 1.60-1.40 Ga Tectonic and sedimentary linkages between the Belt-Purcell basin and southwestern Laurentia during the Mesoproterozoic ca. 1.60-1.40 Ga
Mesoproterozoic sedimentary basins in western North America provide key constraints on pre-Rodinia craton positions and interactions along the western rifted margin of Laurentia. One such basin, the Belt-Purcell basin, extends from southern Idaho into southern British Columbia and contains a >18-km-thick succession of siliciclastic sediment deposited ca. 1.47–1.40 Ga. The ca. 1.47–1.45...
Authors
James V. Jones, Christohper G Dainel, Michael F Doe