Publications
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Interactive effects of fire, soil climate, and moss on CO2 fluxes in black spruce ecosystems of interior Alaska Interactive effects of fire, soil climate, and moss on CO2 fluxes in black spruce ecosystems of interior Alaska
Fire is an important control on the carbon (C) balance of the boreal forest region. Here, we present findings from two complementary studies that examine how fire modifies soil organic matter properties, and how these modifications influence rates of decomposition and C exchange in black spruce (Picea mariana) ecosystems of interior Alaska. First, we used laboratory incubations to...
Authors
Jonathan A. O’Donnell, Merritt R. Turetsky, Jennifer W. Harden, Kristen L. Manies, L.E. Pruett, Gordon Shetler, Jason C. Neff
Quaternary science reviews Pacific Basin tsunami hazards associated with mass flows in the Aleutian arc of Alaska Quaternary science reviews Pacific Basin tsunami hazards associated with mass flows in the Aleutian arc of Alaska
We analyze mass-flow tsunami generation for selected areas within the Aleutian arc of Alaska using results from numerical simulation of hypothetical but plausible mass-flow sources such as submarine landslides and volcanic debris avalanches. The Aleutian arc consists of a chain of volcanic mountains, volcanic islands, and submarine canyons, surrounded by a low-relief continental shelf...
Authors
Christopher F. Waythomas, Philip Watts, Fengyan Shi, James T. Kirby
Nonlinear processes in volcanoes Nonlinear processes in volcanoes
No abstract available
Authors
Bernard A. Chouet
Interactions between soil thermal and hydrological dynamics in the response of Alaska ecosystems to fire disturbance Interactions between soil thermal and hydrological dynamics in the response of Alaska ecosystems to fire disturbance
Soil temperature and moisture are important factors that control many ecosystem processes. However, interactions between soil thermal and hydrological processes are not adequately understood in cold regions, where the frozen soil, fire disturbance, and soil drainage play important roles in controlling interactions among these processes. These interactions were investigated with a new...
Authors
Shuhua Yi, A. David McGuire, Jennifer Harden, Eric Kasischke, Kristen L. Manies, Larry Hinzman, Anna K. Liljedahl, J. Randerson, Heping Liu, Vladimir E. Romanovsky, Sergey S. Marchenko, Yongwon Kim
Improved prediction and tracking of volcanic ash clouds Improved prediction and tracking of volcanic ash clouds
During the past 30 years, more than 100 airplanes have inadvertently flown through clouds of volcanic ash from erupting volcanoes. Such encounters have caused millions of dollars in damage to the aircraft and have endangered the lives of tens of thousands of passengers. In a few severe cases, total engine failure resulted when ash was ingested into turbines and coating turbine blades...
Authors
Larry G. Mastin, Peter Webley
The post-Mazama northwest rift zone eruption at Newberry Volcano, Oregon The post-Mazama northwest rift zone eruption at Newberry Volcano, Oregon
The northwest rift zone (NWRZ) eruption took place at Newberry Volcano ~7000 years ago after the volcano was mantled by tephra from the catastrophic eruption that destroyed Mount Mazama and produced the Crater Lake caldera. The NWRZ eruption produced multiple lava flows from a variety of vents including cinder cones, spatter vents, and fissures, possibly in more than one episode...
Authors
Daniele McKay, Julie M. Donnelly-Nolan, Robert A. Jensen, Duane E. Champion
Many monstrous Missoula floods down channeled scabland and Columbia Valley, Washington Many monstrous Missoula floods down channeled scabland and Columbia Valley, Washington
The late Wisconsin Missoula floods are Earth's largest known discharges of fresh water. They carved Washington's Channeled Scabland--made famous by J H. Bretz's writings in the 1920s to 1950s--and deposited sporadic huge gravel bars in the Scab-lands and Columbia valley. Since the late 1970s the great floods have been shown to number several score and to have been released as gigantic...
Authors
Richard B. Waitt, Roger P. Denlinger, Jim O’Connor
A multidisciplinary effort to assign realistic source parameters to models of volcanic ash-cloud transport and dispersion during eruptions A multidisciplinary effort to assign realistic source parameters to models of volcanic ash-cloud transport and dispersion during eruptions
During volcanic eruptions, volcanic ash transport and dispersion models (VATDs) are used to forecast the location and movement of ash clouds over hours to days in order to define hazards to aircraft and to communities downwind. Those models use input parameters, called “eruption source parameters”, such as plume height H, mass eruption rate Ṁ, duration D, and the mass fraction m63 of...
Authors
Larry G. Mastin, Marianne C. Guffanti, R. Servranckx, P. Webley, S. Barsotti, K. Dean, A. Durant, John W. Ewert, A. Neri, W.I. Rose, David J. Schneider, Lee Siebert, B. Stunder, G. Swanson, A. Tupper, A. Volentik, Christopher F. Waythomas
Diverse lavas from closely spaced volcanoes drawing from a common parent: Emmons Lake Volcanic Center, Eastern Aleutian Arc Diverse lavas from closely spaced volcanoes drawing from a common parent: Emmons Lake Volcanic Center, Eastern Aleutian Arc
Emmons Lake Volcanic Center (ELVC) on the lower Alaskan Peninsula is one of the largest and most diverse volcanic centers in the Aleutian Arc. Since the Middle Pleistocene, eruption of ~ 350 km3 of basalt through rhyolite has produced a 30 km, arc front chain of nested calderas and overlapping stratovolcanoes. ELVC has experienced as many as five major caldera-forming eruptions, the most...
Authors
M. Mangan, T. Miller, C. Waythomas, F. Trusdell, A. Calvert, P. Layer
Tracking magma volume recovery at Okmok Volcano using GPS and an unscented kalman filter Tracking magma volume recovery at Okmok Volcano using GPS and an unscented kalman filter
Changes beneath a volcano can be observed through position changes in a GPS network, but distinguishing the source of site motion is not always straightforward. The records of continuous GPS sites provide a favorable data set for tracking magma migration. Dense campaign observations usually provide a better spatial picture of the overall deformation field, at the expense of an episodic...
Authors
T. Fournier, Jeffrey T. Freymueller, Peter Cervelli
Features of lava lake filling and draining and their implications for eruption dynamics Features of lava lake filling and draining and their implications for eruption dynamics
Lava lakes experience filling, circulation, and often drainage depending upon the style of activity and location of the vent. Features formed by these processes have proved difficult to document due to dangerous conditions during the eruption, inaccessibility, and destruction of features during lake drainage. Kilauea Iki lava lake, Kilauea, Hawai'i, preserves many such features, because...
Authors
W.K. Stovall, Bruce F. Houghton, A.J.L. Harris, D. A. Swanson
A frozen record of density-driven crustal overturn in lava lakes: The example of Kilauea Iki 1959 A frozen record of density-driven crustal overturn in lava lakes: The example of Kilauea Iki 1959
Lava lakes are found at basaltic volcanoes on Earth and other planetary bodies. Density-driven crustal foundering leading to surface renewal occurs repeatedly throughout the life of a lava lake. This process has been observed and described in a qualitative sense, but due to dangerous conditions, no data has been acquired to evaluate the densities of the units involved. Kilauea Iki pit...
Authors
W.K. Stovall, Bruce F. Houghton, A.J.L. Harris, D. A. Swanson