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A Parsekian

Datos Biográficos

ID7995075
NOMBREA Parsekian
NOMBRESA
APELLIDOParsekian
FIRMAPARSEKIAN A
AFILIACIONESUniversity of Wyoming
ORCID0000-0001-5072-9818
VERIFICADOSí
TOTAL DE OBRAS3
TOTAL DE CITAS0
TOTAL COMO AUTOR3
TOTAL COMO EDITOR0
PRIMER AÑO DE PUBLICACIÓN2018
AÑO MÁS RECIENTE DE PUBLICACIÓN2021
ÍNDICE H0
  • Active layer thickness as a function of soil water content

    Open Access•Leah K Clayton, Kevin Schaefer et al.•ARTICLE•Environmental Research Letters•2021

    Active layer thickness (ALT) is a critical metric for monitoring permafrost. How soil moisture influences ALT depends on two competing hypotheses: (a) increased soil moisture increases the latent heat of fusion for thaw, resulting in shallower active layers, and (b) increased soil moisture increases soil thermal conductivity, resulting in deeper active layers. To investigate their relative influence on thaw depth, we analyzed the Field Measuremen…

  • Contrasting lake ice responses to winter climate indicate future variability and trends on the Alaskan Arctic Coastal Plain

    Open Access•Christopher D Arp, Benjamin M Jones et al.•ARTICLE•Environmental Research Letters•2018

    Strong winter warming has dominated recent patterns of climate change along the Arctic Coastal Plain (ACP) of northern Alaska. The full impact of arctic winters may be best manifest by freshwater ice growth and the extent to which abundant shallow ACP lakes freeze solid with bedfast ice by the end of winter. For example, winter conditions of 2016–17 produced record low extents of bedfast ice across the ACP. In addition to high air temperatures, t…

  • Inference of the impact of wildfire on permafrost and active layer thickness in a discontinuous permafrost region using the remotely sensed active layer thickness (ReSalt) algorithm

    Open Access•Roger Michaelides, Kevin Schaefer et al.•ARTICLE•Environmental Research Letters•2018

    The Yukon-Kuskokwim (YK) Delta is a region of discontinuous permafrost in the subarctic of southwestern Alaska. Many wildfires have occurred in the YK Delta between 1971-2015, impacting vegetation cover, surface soil moisture, and the active layer. Herein, we demonstrate that the remotely sensed active layer thickness (ReSALT) algorithm can resolve the post-fire active layer dynamics of tundra permafrost. We generated a stack of Advanced Land Obs…

Sin obras prominentes en esta página.

  • Contrasting lake ice responses to winter climate indicate future variability and trends on the Alaskan Arctic Coastal Plain

    Open Access•Christopher D Arp, Benjamin M Jones et al.•ARTICLE•Environmental Research Letters•2018

    Strong winter warming has dominated recent patterns of climate change along the Arctic Coastal Plain (ACP) of northern Alaska. The full impact of arctic winters may be best manifest by freshwater ice growth and the extent to which abundant shallow ACP lakes freeze solid with bedfast ice by the end of winter. For example, winter conditions of 2016–17 produced record low extents of bedfast ice across the ACP. In addition to high air temperatures, t…

  • Inference of the impact of wildfire on permafrost and active layer thickness in a discontinuous permafrost region using the remotely sensed active layer thickness (ReSalt) algorithm

    Open Access•Roger Michaelides, Kevin Schaefer et al.•ARTICLE•Environmental Research Letters•2018

    The Yukon-Kuskokwim (YK) Delta is a region of discontinuous permafrost in the subarctic of southwestern Alaska. Many wildfires have occurred in the YK Delta between 1971-2015, impacting vegetation cover, surface soil moisture, and the active layer. Herein, we demonstrate that the remotely sensed active layer thickness (ReSALT) algorithm can resolve the post-fire active layer dynamics of tundra permafrost. We generated a stack of Advanced Land Obs…

  • Active layer thickness as a function of soil water content

    Open Access•Leah K Clayton, Kevin Schaefer et al.•ARTICLE•Environmental Research Letters•2021

    Active layer thickness (ALT) is a critical metric for monitoring permafrost. How soil moisture influences ALT depends on two competing hypotheses: (a) increased soil moisture increases the latent heat of fusion for thaw, resulting in shallower active layers, and (b) increased soil moisture increases soil thermal conductivity, resulting in deeper active layers. To investigate their relative influence on thaw depth, we analyzed the Field Measuremen…

Climate change and permafrost (3 obras) · Cryospheric studies and observations (3 obras) · Environmental Science (3 obras) · Geology (3 obras) · Permafrost (3 obras) · Active layer (2 obras) · Arctic (2 obras) · Arctic and Antarctic ice dynamics (2 obras) · Atmospheric sciences (2 obras) · Layer (electronics (2 obras)

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