David W Kicklighter
Datos Biográficos
| ID | 6016294 |
|---|---|
| NOMBRE | David W Kicklighter |
| NOMBRES | David W |
| APELLIDO | Kicklighter |
| FIRMA | KICKLIGHTER D W |
| AFILIACIONES | Marine Biological Laboratory |
| ORCID | 0000-0001-6820-2651 |
| VERIFICADO | Sí |
| TOTAL DE OBRAS | 6 |
| TOTAL DE CITAS | 4 |
| TOTAL COMO AUTOR | 6 |
| TOTAL COMO EDITOR | 0 |
| PRIMER AÑO DE PUBLICACIÓN | 2009 |
| AÑO MÁS RECIENTE DE PUBLICACIÓN | 2016 |
| ÍNDICE H | 1 |
Protected areas’ role in climate-change mitigation
Influence of changes in wetland inundation extent on net fluxes of carbon dioxide and methane in northern high latitudes from 1993 to 2004
© The Author(s), 2015. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Environmental Research Letters 10 (2015): 095009, doi:10.1088/1748-9326/10/9/095009
The impacts of recent permafrost thaw on land–atmosphere greenhouse gas exchange
Permafrost thaw and the subsequent mobilization of carbon (C) stored in previously frozen soil organic matter (SOM) have the potential to be a strong positive feedback to climate. As the northern permafrost region experiences as much as a doubling of the rate of warming as the rest of the Earth, the vast amount of C in permafrost soils is vulnerable to thaw, decomposition and release as atmospheric greenhouse gases. Diagnostic and predictive esti…
Permafrost degradation and methane
© The Author(s), 2013. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Environmental Research Letters 8 (2013): 035014, doi:10.1088/1748-9326/8/3/035014
Rising methane emissions in response to climate change in Northern Eurasia during the 21st century
We used a biogeochemistry model, the Terrestrial Ecosystem Model (TEM), to examine the methane (CH4) exchanges between terrestrial ecosystems and the atmosphere in Northern Eurasia from 1971 to 2100. Multiple model simulations using various wetland extent datasets and climate change scenarios were conducted to assess the uncertainty of CH4 fluxes, including emissions and consumption. On the basis of these simulations we estimate the current net e…
Possible decline of the carbon sink in the Mongolian Plateau during the 21st century
The Mongolian Plateau is dominated by grassland ecosystems. It frequently experiences drought and is underlain by permafrost in the north. Its complex responses of plant carbon uptake and soil carbon release to climate change are considered to have affected the global carbon cycle during the 21st century. Here we combine spatially explicit information on vegetation, soils, topography and climate with a process-based biogeochemistry model to asses…
Possible decline of the carbon sink in the Mongolian Plateau during the 21st century
The Mongolian Plateau is dominated by grassland ecosystems. It frequently experiences drought and is underlain by permafrost in the north. Its complex responses of plant carbon uptake and soil carbon release to climate change are considered to have affected the global carbon cycle during the 21st century. Here we combine spatially explicit information on vegetation, soils, topography and climate with a process-based biogeochemistry model to asses…
Rising methane emissions in response to climate change in Northern Eurasia during the 21st century
We used a biogeochemistry model, the Terrestrial Ecosystem Model (TEM), to examine the methane (CH4) exchanges between terrestrial ecosystems and the atmosphere in Northern Eurasia from 1971 to 2100. Multiple model simulations using various wetland extent datasets and climate change scenarios were conducted to assess the uncertainty of CH4 fluxes, including emissions and consumption. On the basis of these simulations we estimate the current net e…
Permafrost degradation and methane
© The Author(s), 2013. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Environmental Research Letters 8 (2013): 035014, doi:10.1088/1748-9326/8/3/035014
The impacts of recent permafrost thaw on land–atmosphere greenhouse gas exchange
Permafrost thaw and the subsequent mobilization of carbon (C) stored in previously frozen soil organic matter (SOM) have the potential to be a strong positive feedback to climate. As the northern permafrost region experiences as much as a doubling of the rate of warming as the rest of the Earth, the vast amount of C in permafrost soils is vulnerable to thaw, decomposition and release as atmospheric greenhouse gases. Diagnostic and predictive esti…
Influence of changes in wetland inundation extent on net fluxes of carbon dioxide and methane in northern high latitudes from 1993 to 2004
© The Author(s), 2015. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Environmental Research Letters 10 (2015): 095009, doi:10.1088/1748-9326/10/9/095009
Protected areas’ role in climate-change mitigation
Climate change (6 obras) · Environmental Science (6 obras) · Geology (6 obras) · Atmospheric sciences (5 obras) · Ecology (5 obras) · Geography (5 obras) · Climate change and permafrost (4 obras) · Climatology (4 obras) · Ecosystem (4 obras) · Greenhouse gas (4 obras)