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Amy Breen

Dados Biográficos

ID7993017
NOMEAmy Breen
PRENOMESAmy
SOBRENOMEBreen
ASSINATURABREEN A
AFILIAÇÕESUniversity of Alaska Fairbanks
ORCID0000-0002-1109-3906
VERIFICADOSim
TOTAL DE OBRAS10
TOTAL DE CITAÇÕES0
OBRAS COMO AUTOR10
OBRAS COMO EDITOR0
PRIMEIRO ANO DE PUBLICAÇÃO2012
ANO MAIS RECENTE DE PUBLICAÇÃO2024
ÍNDICE H0
  • Post-drainage vegetation, microtopography and organic matter in Arctic drained lake basins

    Open Access•Juliane Wolter, Benjamin M Jones et al.•ARTICLE•Environmental Research Letters•2024

    Wetlands in Arctic drained lake basins (DLBs) have a high potential for carbon storage in vegetation and peat as well as for elevated greenhouse gas emissions. However, the evolution of vegetation and organic matter is rarely studied in DLBs, making these abundant wetlands especially uncertain elements of the permafrost carbon budget. We surveyed multiple DLB generations in northern Alaska with the goal to assess vegetation, microtopography, and …

  • Local-scale heterogeneity of soil thermal dynamics and controlling factors in a discontinuous permafrost region

    Open Access•Chen Wang, Ian Shirley et al.•ARTICLE•Environmental Research Letters•2024

    In permafrost regions, the strong spatial and temporal variability in soil temperature cannot be explained by the weather forcing only. Understanding the local heterogeneity of soil thermal dynamics and their controls is essential to understand how permafrost systems respond to climate change and to develop process-based models or remote sensing products for predicting soil temperature. In this study, we analyzed soil temperature dynamics and the…

  • Landscape-scale characterization of Arctic tundra vegetation composition, structure, and function with a multi-sensor unoccupied aerial system

    Open Access•Dedi Yang, Bailey D Morrison et al.•ARTICLE•Environmental Research Letters•2021

    The Arctic is experiencing some of the most rapid climate change on Earth, with strong impacts on tundra ecosystems that are characterized by high land-surface and vegetation heterogeneity. Previous studies have explored this complexity using satellite remote sensing, however these typically coarse spatial resolution data have generally missed sub-pixel heterogeneity, leaving critical gaps in our understanding of tundra vegetation dynamics from t…

  • Shallow soils are warmer under trees and tall shrubs across Arctic and Boreal ecosystems

    Open Access•Heather Kropp, M M Loranty et al.•ARTICLE•Environmental Research Letters•2020

    Soils are warming as air temperatures rise across the Arctic and Boreal region concurrent with the expansion of tall-statured shrubs and trees in the tundra. Changes in vegetation structure and function are expected to alter soil thermal regimes, thereby modifying climate feedbacks related to permafrost thaw and carbon cycling. However, current understanding of vegetation impacts on soil temperature is limited to local or regional scales and lack…

  • Infrastructure Development Accelerates Range Expansion of Trembling Aspen ( Populus tremuloides , Salicaceae) into the Arctic

    Open Access•Daniel Ackerman, Amy Breen•ARTICLE•ARCTIC•2016

    Interacting forces of climate change and increased human activity in the Arctic are driving rapid changes in ecosystem structure, function, and biodiversity. One such change is the northern range expansion of tree species. We present the first account of the boreal tree species trembling aspen (Populus tremuloides, Salicaceae) growing beyond the latitudinal treeline in the northern foothills of the Brooks Range, Alaska. The four trembling aspen s…

  • Consequences of changes in vegetation and snow cover for climate feedbacks in Alaska and northwest Canada

    Open Access•E S Euskirchen, Alec Bennett et al.•ARTICLE•Environmental Research Letters•2016

    Changes in vegetation and snow cover may lead to feedbacks to climate through changes in surface albedo and energy fluxes between the land and atmosphere. In addition to these biogeophysical feedbacks, biogeochemical feedbacks associated with changes in carbon (C) storage in the vegetation and soils may also influence climate. Here, using a transient biogeographic model (ALFRESCO) and an ecosystem model (DOS-TEM), we quantified the biogeophysical…

  • Biomass offsets little or none of permafrost carbon release from soils, streams, and wildfire

    Open Access•Benjamin W Abbott, Jeremy B Jones et al.•ARTICLE•Environmental Research Letters•2016

    As the permafrost region warms, its large organic carbon pool will be increasingly vulnerable to decomposition, combustion, and hydrologic export. Models predict that some portion of this release will be offset by increased production of Arctic and boreal biomass; however, the lack of robust estimates of net carbon balance increases the risk of further overshooting international emissions targets. Precise empirical or model-based assessments of t…

  • Rescuing Valuable Arctic Vegetation Data for Biodiversity Models, Ecosystem Models and a Panarctic Vegetation Classification

    Open Access•Donald A Walker, Inger G Alsos et al.•ARTICLE•ARCTIC•2013

    TEST 02 - Elsevier's Scopus, the largest abstract and citation database of peer-reviewed literature. Search and access research from the science, technology, medicine, social sciences and arts and humanities fields

  • Modeling the effects of fire severity and climate warming on active layer thickness and soil carbon storage of black spruce forests across the landscape in interior Alaska

    Open Access•Hélène Genet, A D McGuire et al.•ARTICLE•Environmental Research Letters•2013

    There is a substantial amount of carbon stored in the permafrost soils of boreal forest ecosystems, where it is currently protected from decomposition. The surface organic horizons insulate the deeper soil from variations in atmospheric temperature. The removal of these insulating horizons through consumption by fire increases the vulnerability of permafrost to thaw, and the carbon stored in permafrost to decomposition. In this study we ask how w…

  • The footprint of Alaskan tundra fires during the past half-century

    Open Access•Adrian V Rocha, M M Loranty et al.•ARTICLE•Environmental Research Letters•2012

    © IOP Publishing, 2012. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Environmental Research Letters 7 (2012): 044039, doi:10.1088/1748-9326/7/4/044039

Sem obras proeminentes nesta página.

  • The footprint of Alaskan tundra fires during the past half-century

    Open Access•Adrian V Rocha, M M Loranty et al.•ARTICLE•Environmental Research Letters•2012

    © IOP Publishing, 2012. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Environmental Research Letters 7 (2012): 044039, doi:10.1088/1748-9326/7/4/044039

  • Rescuing Valuable Arctic Vegetation Data for Biodiversity Models, Ecosystem Models and a Panarctic Vegetation Classification

    Open Access•Donald A Walker, Inger G Alsos et al.•ARTICLE•ARCTIC•2013

    TEST 02 - Elsevier's Scopus, the largest abstract and citation database of peer-reviewed literature. Search and access research from the science, technology, medicine, social sciences and arts and humanities fields

  • Modeling the effects of fire severity and climate warming on active layer thickness and soil carbon storage of black spruce forests across the landscape in interior Alaska

    Open Access•Hélène Genet, A D McGuire et al.•ARTICLE•Environmental Research Letters•2013

    There is a substantial amount of carbon stored in the permafrost soils of boreal forest ecosystems, where it is currently protected from decomposition. The surface organic horizons insulate the deeper soil from variations in atmospheric temperature. The removal of these insulating horizons through consumption by fire increases the vulnerability of permafrost to thaw, and the carbon stored in permafrost to decomposition. In this study we ask how w…

  • Infrastructure Development Accelerates Range Expansion of Trembling Aspen ( Populus tremuloides , Salicaceae) into the Arctic

    Open Access•Daniel Ackerman, Amy Breen•ARTICLE•ARCTIC•2016

    Interacting forces of climate change and increased human activity in the Arctic are driving rapid changes in ecosystem structure, function, and biodiversity. One such change is the northern range expansion of tree species. We present the first account of the boreal tree species trembling aspen (Populus tremuloides, Salicaceae) growing beyond the latitudinal treeline in the northern foothills of the Brooks Range, Alaska. The four trembling aspen s…

  • Consequences of changes in vegetation and snow cover for climate feedbacks in Alaska and northwest Canada

    Open Access•E S Euskirchen, Alec Bennett et al.•ARTICLE•Environmental Research Letters•2016

    Changes in vegetation and snow cover may lead to feedbacks to climate through changes in surface albedo and energy fluxes between the land and atmosphere. In addition to these biogeophysical feedbacks, biogeochemical feedbacks associated with changes in carbon (C) storage in the vegetation and soils may also influence climate. Here, using a transient biogeographic model (ALFRESCO) and an ecosystem model (DOS-TEM), we quantified the biogeophysical…

  • Biomass offsets little or none of permafrost carbon release from soils, streams, and wildfire

    Open Access•Benjamin W Abbott, Jeremy B Jones et al.•ARTICLE•Environmental Research Letters•2016

    As the permafrost region warms, its large organic carbon pool will be increasingly vulnerable to decomposition, combustion, and hydrologic export. Models predict that some portion of this release will be offset by increased production of Arctic and boreal biomass; however, the lack of robust estimates of net carbon balance increases the risk of further overshooting international emissions targets. Precise empirical or model-based assessments of t…

  • Shallow soils are warmer under trees and tall shrubs across Arctic and Boreal ecosystems

    Open Access•Heather Kropp, M M Loranty et al.•ARTICLE•Environmental Research Letters•2020

    Soils are warming as air temperatures rise across the Arctic and Boreal region concurrent with the expansion of tall-statured shrubs and trees in the tundra. Changes in vegetation structure and function are expected to alter soil thermal regimes, thereby modifying climate feedbacks related to permafrost thaw and carbon cycling. However, current understanding of vegetation impacts on soil temperature is limited to local or regional scales and lack…

  • Landscape-scale characterization of Arctic tundra vegetation composition, structure, and function with a multi-sensor unoccupied aerial system

    Open Access•Dedi Yang, Bailey D Morrison et al.•ARTICLE•Environmental Research Letters•2021

    The Arctic is experiencing some of the most rapid climate change on Earth, with strong impacts on tundra ecosystems that are characterized by high land-surface and vegetation heterogeneity. Previous studies have explored this complexity using satellite remote sensing, however these typically coarse spatial resolution data have generally missed sub-pixel heterogeneity, leaving critical gaps in our understanding of tundra vegetation dynamics from t…

  • Post-drainage vegetation, microtopography and organic matter in Arctic drained lake basins

    Open Access•Juliane Wolter, Benjamin M Jones et al.•ARTICLE•Environmental Research Letters•2024

    Wetlands in Arctic drained lake basins (DLBs) have a high potential for carbon storage in vegetation and peat as well as for elevated greenhouse gas emissions. However, the evolution of vegetation and organic matter is rarely studied in DLBs, making these abundant wetlands especially uncertain elements of the permafrost carbon budget. We surveyed multiple DLB generations in northern Alaska with the goal to assess vegetation, microtopography, and …

  • Local-scale heterogeneity of soil thermal dynamics and controlling factors in a discontinuous permafrost region

    Open Access•Chen Wang, Ian Shirley et al.•ARTICLE•Environmental Research Letters•2024

    In permafrost regions, the strong spatial and temporal variability in soil temperature cannot be explained by the weather forcing only. Understanding the local heterogeneity of soil thermal dynamics and their controls is essential to understand how permafrost systems respond to climate change and to develop process-based models or remote sensing products for predicting soil temperature. In this study, we analyzed soil temperature dynamics and the…

Climate change and permafrost (10 obras) · Ecology (10 obras) · Environmental Science (10 obras) · Geography (10 obras) · Geology (9 obras) · Cryospheric studies and observations (8 obras) · Ecosystem (8 obras) · Arctic (7 obras) · Physical geography (7 obras) · Taiga (6 obras)

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