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Burke J Minsley

Biographic Data

ID7993540
NAMEBurke J Minsley
GIVEN NAMESBurke J
FAMILY NAMEMinsley
SIGNATUREMINSLEY B J
AFFILIATIONSUnited States Geological Survey
ORCID0000-0003-1689-1306
VERIFIEDYes
TOTAL WORKS3
TOTAL CITATIONS0
WORKS AS AUTHOR3
WORKS AS EDITOR0
FIRST PUBLICATION YEAR2018
LATEST PUBLICATION YEAR2020
H-INDEX0
  • Decadal-scale hotspot methane ebullition within lakes following abrupt permafrost thaw

    Open Access•Katey Walter Anthony, P Lindgren et al.•ARTICLE•Environmental Research Letters•2020

    Thermokarst lakes accelerate deep permafrost thaw and the mobilization of previously frozen soil organic carbon. This leads to microbial decomposition and large releases of carbon dioxide (CO 2 ) and methane (CH 4 ) that enhance climate warming. However, the time scale of permafrost-carbon emissions following thaw is not well known but is important for understanding how abrupt permafrost thaw impacts climate feedback. We combined field measuremen…

  • Investigating lake-area dynamics across a permafrost-thaw spectrum using airborne electromagnetic surveys and remote sensing time-series data in Yukon Flats, Alaska

    Open Access•David M Rey, Michelle A Walvoord et al.•ARTICLE•Environmental Research Letters•2019

    Lakes in boreal lowlands cycle carbon and supply an important source of freshwater for wildlife and migratory waterfowl. The abundance and distribution of these lakes are supported, in part, by permafrost distribution, which is subject to change. Relationships between permafrost thaw and lake dynamics remain poorly known in most boreal regions. Here, new airborne electromagnetic (AEM) data collected during June 2010 and February 2016 were used to…

  • Development of perennial thaw zones in boreal hillslopes enhances potential mobilization of permafrost carbon

    Open Access•Michelle A Walvoord, Clifford I Voss et al.•ARTICLE•Environmental Research Letters•2018

    Permafrost thaw alters subsurface flow in boreal regions that in turn influences the magnitude, seasonality, and chemical composition of streamflow. Prediction of these changes is challenged by incomplete knowledge of timing, flowpath depth, and amount of groundwater discharge to streams in response to thaw. One important phenomenon that may affect flow and transport through boreal hillslopes is development of lateral perennial thaw zones (PTZs),…

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  • Development of perennial thaw zones in boreal hillslopes enhances potential mobilization of permafrost carbon

    Open Access•Michelle A Walvoord, Clifford I Voss et al.•ARTICLE•Environmental Research Letters•2018

    Permafrost thaw alters subsurface flow in boreal regions that in turn influences the magnitude, seasonality, and chemical composition of streamflow. Prediction of these changes is challenged by incomplete knowledge of timing, flowpath depth, and amount of groundwater discharge to streams in response to thaw. One important phenomenon that may affect flow and transport through boreal hillslopes is development of lateral perennial thaw zones (PTZs),…

  • Investigating lake-area dynamics across a permafrost-thaw spectrum using airborne electromagnetic surveys and remote sensing time-series data in Yukon Flats, Alaska

    Open Access•David M Rey, Michelle A Walvoord et al.•ARTICLE•Environmental Research Letters•2019

    Lakes in boreal lowlands cycle carbon and supply an important source of freshwater for wildlife and migratory waterfowl. The abundance and distribution of these lakes are supported, in part, by permafrost distribution, which is subject to change. Relationships between permafrost thaw and lake dynamics remain poorly known in most boreal regions. Here, new airborne electromagnetic (AEM) data collected during June 2010 and February 2016 were used to…

  • Decadal-scale hotspot methane ebullition within lakes following abrupt permafrost thaw

    Open Access•Katey Walter Anthony, P Lindgren et al.•ARTICLE•Environmental Research Letters•2020

    Thermokarst lakes accelerate deep permafrost thaw and the mobilization of previously frozen soil organic carbon. This leads to microbial decomposition and large releases of carbon dioxide (CO 2 ) and methane (CH 4 ) that enhance climate warming. However, the time scale of permafrost-carbon emissions following thaw is not well known but is important for understanding how abrupt permafrost thaw impacts climate feedback. We combined field measuremen…

Climate change and permafrost (3 works) · Cryospheric studies and observations (3 works) · Ecology (3 works) · Environmental Science (3 works) · Geography (3 works) · Geology (3 works) · Hydrology (agriculture (3 works) · Oceanography (3 works) · Permafrost (3 works) · Arctic (2 works)

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