Publications
Filter Total Items: 1423
Past climate variability and change in the Arctic and at high latitudes Past climate variability and change in the Arctic and at high latitudes
Paleoclimate records play a key role in our understanding of Earth's past and present climate system and in our confidence in predicting future climate changes. Paleoclimate data help to elucidate past and present active mechanisms of climate change by placing the short instrumental record into a longer term context and by permitting models to be tested beyond the limited time that...
Authors
Richard B. Alley, Julie Brigham-Grette, Gifford H. Miller, Leonid Polyak
Fire behavior, weather, and burn severity of the 2007 anaktuvuk river tundra fire, North Slope, Alaska Fire behavior, weather, and burn severity of the 2007 anaktuvuk river tundra fire, North Slope, Alaska
In 2007, the Anaktuvuk River Fire (ARF) became the largest recorded tundra fire on the North Slope of Alaska. The ARF burned for nearly three months, consuming more than 100,000 ha. At its peak in early September, the ARF burned at a rate of 7000 ha d-1. The conditions potentially responsible for this large tundra fire include modeled record high summer temperature and record low summer
Authors
Benjamin M. Jones, Crystal A. Kolden, Randi Jandt, John T. Abatzoglou, Frank Urban, Christopher D. Arp
Is the track of the Yellowstone hotspot driven by a deep mantle plume? - Review of volcanism, faulting, and uplift in light of new data Is the track of the Yellowstone hotspot driven by a deep mantle plume? - Review of volcanism, faulting, and uplift in light of new data
Geophysical imaging of a tilted mantle plume extending at least 500 km beneath the Yellowstone caldera provides compelling support for a plume origin of the entire Yellowstone hotspot track back to its inception at 17 Ma with eruptions of flood basalts and rhyolite. The widespread volcanism, combined with a large volume of buoyant asthenosphere, supports a plume head as an initial phase...
Authors
Kenneth L. Pierce, Lisa A. Morgan
Structural development of high-temperature mylonites in the Archean Wyoming province, northwestern Madison Range, Montana Structural development of high-temperature mylonites in the Archean Wyoming province, northwestern Madison Range, Montana
The Crooked Creek mylonite, in the northwestern Madison Range, southwestern Montana, is defined by several curved lenses of high non-coaxial strain exposed over a 7-km-wide, northeast-trending strip. The country rocks, part of the Archean Wyoming province, are dominantly trondhjemitic to granitic orthogneiss with subordinate amphibolite, quartzite, aluminous gneiss, and sills of...
Authors
Karl S. Kellogg, David W. Mogk
Eolian sediments and processes Eolian sediments and processes
No abstract available.
Authors
D.R. Muhs
Climatic and limnologic setting of Bear Lake, Utah and Idaho Climatic and limnologic setting of Bear Lake, Utah and Idaho
Bear Lake is a large alkaline lake on a high plateau on the Utah-Idaho border. The Bear River was partly diverted into the lake in the early twentieth century so that Bear Lake could serve as a reservoir to supply water for hydropower and irrigation downstream, which continues today. The northern Rocky Mountain region is within the belt of the strongest of the westerly winds that...
Authors
W.E. Dean, W.A. Wurtsbaugh, V.A. Lamarra
Major- and trace-element characterization, expanded distribution, and a new chronology for the latest Pleistocene Glacier Peak tephras in western North America Major- and trace-element characterization, expanded distribution, and a new chronology for the latest Pleistocene Glacier Peak tephras in western North America
The Glacier Peak tephra beds are among the most widespread and arguably some of the most important late Pleistocene chronostratigraphic markers in western North America. These beds represent a series of closely-spaced Plinian and sub-Plinian eruptions from Glacier Peak, Washington. The two most widespread beds, Glacier Peak 'G' and 'B', are reliably distinguished by their glass major and...
Authors
S.C. Kuehn, D.G. Froese, P. E. Carrara, F.F. Foit, N.J.G. Pearce, P. Rotheisler
A formal framework for scenario development in support of environmental decision-making A formal framework for scenario development in support of environmental decision-making
Scenarios are possible future states of the world that represent alternative plausible conditions under different assumptions. Often, scenarios are developed in a context relevant to stakeholders involved in their applications since the evaluation of scenario outcomes and implications can enhance decision-making activities. This paper reviews the state-of-the-art of scenario development...
Authors
M. Mahmoud, Yajing Liu, H. Hartmann, S. Stewart, T. Wagener, D. Semmens, R. Stewart, H. Gupta, D. Dominguez, F. Dominguez, D. Hulse, R. Letcher, Brenda Rashleigh, C. Smith, R. Street, J. Ticehurst, M. Twery, Delden H. van, R. Waldick, D. White, L. Winter
Late Quaternary paleoclimate of western Alaska inferred from fossil chironomids and its relation to vegetation histories Late Quaternary paleoclimate of western Alaska inferred from fossil chironomids and its relation to vegetation histories
Fossil Chironomidae assemblages (with a few Chaoboridae and Ceratopogonidae) from Zagoskin and Burial Lakes in western Alaska provide quantitative reconstructions of mean July air temperatures for periods of the late-middle Wisconsin (~39,000-34,000 cal yr B.P.) to the present. Inferred temperatures are compared with previously analyzed pollen data from each site summarized here by...
Authors
Joshua Kurek, Les C. Cwynar, Thomas A. Ager, Mark B. Abbott, Mary E. Edwards
The glacial/deglacial history of sedimentation in Bear Lake, Utah and Idaho The glacial/deglacial history of sedimentation in Bear Lake, Utah and Idaho
Bear Lake, in northeastern Utah and southern Idaho, lies in a large valley formed by an active half-graben. Bear River, the largest river in the Great Basin, enters Bear Lake Valley ???15 km north of the lake. Two 4-m-long cores provide a lake sediment record extending back ???26 cal k.y. The penetrated section can be divided into a lower unit composed of quartz-rich clastic sediments...
Authors
J. G. Rosenbaum, C.W. Heil
Geology and geomorphology of Bear Lake Valley and upper Bear River, Utah and Idaho Geology and geomorphology of Bear Lake Valley and upper Bear River, Utah and Idaho
Bear Lake, on the Idaho-Utah border, lies in a fault-bounded valley through which the Bear River flows en route to the Great Salt Lake. Surficial deposits in the Bear Lake drainage basin provide a geologic context for interpretation of cores from Bear Lake deposits. In addition to groundwater discharge, Bear Lake received water and sediment from its own small drainage basin and sometimes...
Authors
M.C. Reheis, B.J.C. Laabs, D. S. Kaufman
The origin and paleoclimatic significance of carbonate sand dunes deposited on the California Channel Islands during the last glacial period The origin and paleoclimatic significance of carbonate sand dunes deposited on the California Channel Islands during the last glacial period
No abstract available.
Authors
Daniel R. Muhs, Gary Skipp, R. Randall Schumann, Donald L. Johnson, John P. McGeehin, Jossh Beann, Joshua Freeman, Timothy A. Pearce, Zachary Muhs Rowland