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Eolian sediments Eolian sediments

The origin and nature of eolian (wind-blown) sediments are reviewed, with an emphasis on the occurrence of these features in the Quaternary. Eolian sediments consist of windblown sand, loess, and long-range-transported (LRT) dust, in order of decreasing particle size. Eolian sand forms some of the most dramatic landscapes in the world, particularly when these sediments are deposited as...
Authors
Daniel R. Muhs

The geography of islands The geography of islands

Islands come in all shapes, sizes and types, from tiny rocky outcrops, to enormous continental landmasses. The true number of islands distributed in the planet’s seas and oceans is still elusive. Recent efforts bolstered by an abundance of detailed satellite imagery and the sophistication of geographic information systems (GIS) are bringing real answers to those questions closer than...
Authors
Roger Sayre, Madeline Thomas Martin, Jill Janene Cress, Nick Holmes, Osgur McDermott-Long, Lauren Weatherdon, Dena Spatz, Keith VanGraafeiland, David Will

Climate and Ecological Disturbance Analysis of Engelmann spruce and Douglas fir in the Greater Yellowstone Ecosystem Climate and Ecological Disturbance Analysis of Engelmann spruce and Douglas fir in the Greater Yellowstone Ecosystem

The effects of anthropogenic climate change are apparent in the Greater Yellowstone Ecosystem (GYE), USA, with forest die-off, insect outbreaks, and wildfires impacting forest ecosystems. A long-term perspective would enable assessment of the historical range of variability in forest ecosystems and better determination of recent forest dynamics and historical thresholds. The objectives...
Authors
Brittany Rinaldi, R. Stockton Maxwell, Thomas Callahan, Rebecca Lynn Brice, Karen Heeter, Grant L. Harley

Increased burning in a warming climate reduces carbon uptake in the Greater Yellowstone Ecosystem despite productivity gains Increased burning in a warming climate reduces carbon uptake in the Greater Yellowstone Ecosystem despite productivity gains

1. The effects of changing climate and disturbance on mountain forest carbon stocks vary with tree species distributions and over elevational gradients. Warming can increase carbon uptake by stimulating productivity at high elevations but also enhance carbon release by increasing respiration and the frequency, intensity, and size of wildfires. 2. To understand the consequences of climate...
Authors
Paul D. Henne, Todd Hawbaker, Robert M. Scheller, Feng S Zhao, Hong S He, Wenru Xu, Zhiliang Zhu

Deglaciation of the Puget Lowland, Washington Deglaciation of the Puget Lowland, Washington

Recently obtained radiocarbon ages from the southern Puget Lowland and reevaluation of limiting ages from the Olympic Peninsula in the light of new light detection and ranging (LiDAR) data suggest that the Juan de Fuca and Puget lobes of the Cordilleran ice sheet reached their maximum extents after 16,000 calibrated yr B.P. Source areas for both lobes fed through a common conduit, likely...
Authors
Ralph A. Haugerud

Diverse cataclysmic floods from Pleistocene glacial Lake Missoula Diverse cataclysmic floods from Pleistocene glacial Lake Missoula

In late Wisconsin time, the Purcell Trench lobe of the Cordilleran ice sheet dammed the Clark Fork of the Columbia River in western Montana, creating glacial Lake Missoula. During part of this epoch, the Okanogan lobe also dammed the Columbia River downstream, creating glacial Lake Columbia in northeast Washington. Repeated failure of the Purcell Trench ice dam released glacial Lake...
Authors
Roger P. Denlinger, David L. George, Charles M. Cannon, Jim E. O'Connor, Richard B. Waitt

A comparison of the CMIP6 midHolocene and lig127k simulations in CESM2 A comparison of the CMIP6 midHolocene and lig127k simulations in CESM2

Results are presented and compared for the Community Earth System Model version 2 (CESM2) simulations of the middle Holocene (MH, 6 ka) and Last Interglacial (LIG, 127 ka). These simulations are designated as Tier 1 experiments (midHolocene and lig127k) for the Coupled Model Intercomparison Project phase 6 (CMIP6) and the Paleoclimate Modeling Intercomparison Project phase 4 (PMIP4)...
Authors
Bette L. Otto-Bliesner, Esther C. Brady, Robert A Tomas, Samuel Albani, Patrick J. Bartlein, Natalie M Mahowald, Sarah Shafer, Erik Kluzek, Peter J Lawrence, Gunter Leguy, Matthew Rothstein, Aleah Sommers

Tracking rates of postfire conifer regeneration vs. deciduous vegetation recovery across the western United States Tracking rates of postfire conifer regeneration vs. deciduous vegetation recovery across the western United States

Postfire shifts in vegetation composition will have broad ecological impacts. However, information characterizing postfire recovery patterns and their drivers are lacking over large spatial extents. In this analysis, we used Landsat imagery collected when snow cover (SCS) was present, in combination with growing season (GS) imagery, to distinguish evergreen vegetation from deciduous...
Authors
Melanie K. Vanderhoof, Todd Hawbaker, Andrea Ming Ku, Kyle Merriam, Erin Berryman, Megan Cattau

Accounting for land in the United States: Integrating physical land cover, land use, and monetary valuation Accounting for land in the United States: Integrating physical land cover, land use, and monetary valuation

Land plays a critical role in both economic and environmental accounting. As an asset, it occupies a unique position at the intersection of the System of National Accounts (SNA), the System of Environmental-Economic Accounting Central Framework (SEEA-CF), and (as a spatial unit) SEEA Experimental Ecosystem Accounting (SEEA-EEA), making land a natural starting point for developing natural...
Authors
Scott A. Wentland, Zachary H. Ancona, Kenneth J. Bagstad, James W. Boyd, Julie L. Hass, Marina Gindelsky, Jeremy G. Moulton

Soil respiration response to rainfall modulated by plant phenology in a montane meadow, East River, Colorado, USA Soil respiration response to rainfall modulated by plant phenology in a montane meadow, East River, Colorado, USA

Soil respiration is a primary component of the terrestrial carbon cycle. However, predicting the response of soil respiration to climate change remains a challenge due to the complex interactions between environmental drivers, especially plant phenology, temperature, and soil moisture. In this study, we use a 1‐D diffusion‐reaction model to calculate depth‐resolved CO2 production rates...
Authors
Mathew Winnick, Corey R. Lawrence, Maeve McCormick, Jennifer Druhan, Kate Maher

Spatially explicit reconstruction of post-megafire forest recovery through landscape modeling Spatially explicit reconstruction of post-megafire forest recovery through landscape modeling

Megafires are large wildfires that occur under extreme weather conditions and produce mixed burn severities across diverse environmental gradients. Assessing megafire effects requires data covering large spatiotemporal extents, which are difficult to collect from field inventories. Remote sensing provides an alternative but is limited in revealing post-fire recovery trajectories and the...
Authors
Wenru Xu, Hong He, Jacob S. Fraser, Todd Hawbaker, Paul D. Henne, Shengwu Duan, Zhiliang Zhu

Integrating physical and economic data into experimental water accounts for the United States: Lessons and opportunities Integrating physical and economic data into experimental water accounts for the United States: Lessons and opportunities

Water management increasingly involves tradeoffs, making its accounting highly relevant in our interconnected world. Physical and economic data about water in many nations are becoming more widely integrated through application of the System of Environmental-Economic Accounts for Water (SEEA-Water), which enables the tracking of linkages between water and the economy. We present the...
Authors
Kenneth J. Bagstad, Zachary H. Ancona, Julie L. Hass, Pierre D. Glynn, Scott Wentland, Michael Vardon, John P. Fay
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