Jennifer Harden, PhD (Former Employee)
Science and Products
Filter Total Items: 144
Soil physical, chemical, and gas-flux characterization from Picea mariana stands near Erickson Creek, Alaska Soil physical, chemical, and gas-flux characterization from Picea mariana stands near Erickson Creek, Alaska
Fire is a particularly important control on the carbon (C) balance of the boreal forest, and fire-return intervals and fire severity appear to have increased since the late 1900s in North America. In addition to the immediate release of stored C to the atmosphere through organic-matter combustion, fire also modifies soil conditions, possibly affecting C exchange between terrestrial and...
Authors
Jonathan A. O’Donnell, Jennifer W. Harden, Kristen L. Manies
Soil data from different-age Picea mariana stands near Delta Junction, Alaska Soil data from different-age Picea mariana stands near Delta Junction, Alaska
One objective of the U.S. Geological Survey\'s Fate of Carbon in Alaskan Landscapes (FOCAL) project is to study the effects of fire and soil drainage on soil carbon storage in boreal forests. For this purpose, the project has measured the soil carbon content in several chronosequences (time since disturbance) of various soil-drainage types. One such chronosequence near Delta Junction...
Authors
Kristen L. Manies, Jennifer W. Harden
Patterns of NPP, GPP, respiration, and NEP during boreal forest succession Patterns of NPP, GPP, respiration, and NEP during boreal forest succession
We combined year‐round eddy covariance with biometry and biomass harvests along a chronosequence of boreal forest stands that were 1, 6, 15, 23, 40, ∼74, and ∼154 years old to understand how ecosystem production and carbon stocks change during recovery from stand‐replacing crown fire. Live biomass (Clive) was low in the 1‐ and 6‐year‐old stands, and increased following a logistic pattern...
Authors
M. L. Goulden, A.M.S. Mcmillan, G.C. Winston, A.V. Rocha, K.L. Manies, J.W. Harden, B. P. Bond-Lamberty
The effect of fire and permafrost interactions on soil carbon accumulation in an upland black spruce ecosystem of interior Alaska: Implications for post-thaw carbon loss The effect of fire and permafrost interactions on soil carbon accumulation in an upland black spruce ecosystem of interior Alaska: Implications for post-thaw carbon loss
High‐latitude regions store large amounts of organic carbon (OC) in active‐layer soils and permafrost, accounting for nearly half of the global belowground OC pool. In the boreal region, recent warming has promoted changes in the fire regime, which may exacerbate rates of permafrost thaw and alter soil OC dynamics in both organic and mineral soil. We examined how interactions between...
Authors
J. A. O'Donnell, J.W. Harden, A. D. McGuire, M.Z. Kanevskiy, M.T. Jorgenson, X. Xu
Water and heat transport in boreal soils: Implications for soil response to climate change Water and heat transport in boreal soils: Implications for soil response to climate change
Soil water content strongly affects permafrost dynamics by changing the soil thermal properties. However, the movement of liquid water, which plays an important role in the heat transport of temperate soils, has been under-represented in boreal studies. Two different heat transport models with and without convective heat transport were compared to measurements of soil temperatures in...
Authors
Z. Fan, J. C. Neff, J.W. Harden, T. Zhang, H. Veldhuis, C.I. Czimczik, G.C. Winston, J. A. O'Donnell
Recent acceleration of biomass burning and carbon losses in Alaskan forests and peatlands Recent acceleration of biomass burning and carbon losses in Alaskan forests and peatlands
Climate change has increased the area affected by forest fires each year in boreal North America. Increases in burned area and fire frequency are expected to stimulate boreal carbon losses. However, the impact of wildfires on carbon emissions is also affected by the severity of burning. How climate change influences the severity of biomass burning has proved difficult to assess. Here, we...
Authors
M.R. Turetsky, E.S. Kane, J.W. Harden, R.D. Ottmar, K.L. Manies, E. Hoy, E.S. Kasischke
Science and Products
Filter Total Items: 144
Soil physical, chemical, and gas-flux characterization from Picea mariana stands near Erickson Creek, Alaska Soil physical, chemical, and gas-flux characterization from Picea mariana stands near Erickson Creek, Alaska
Fire is a particularly important control on the carbon (C) balance of the boreal forest, and fire-return intervals and fire severity appear to have increased since the late 1900s in North America. In addition to the immediate release of stored C to the atmosphere through organic-matter combustion, fire also modifies soil conditions, possibly affecting C exchange between terrestrial and...
Authors
Jonathan A. O’Donnell, Jennifer W. Harden, Kristen L. Manies
Soil data from different-age Picea mariana stands near Delta Junction, Alaska Soil data from different-age Picea mariana stands near Delta Junction, Alaska
One objective of the U.S. Geological Survey\'s Fate of Carbon in Alaskan Landscapes (FOCAL) project is to study the effects of fire and soil drainage on soil carbon storage in boreal forests. For this purpose, the project has measured the soil carbon content in several chronosequences (time since disturbance) of various soil-drainage types. One such chronosequence near Delta Junction...
Authors
Kristen L. Manies, Jennifer W. Harden
Patterns of NPP, GPP, respiration, and NEP during boreal forest succession Patterns of NPP, GPP, respiration, and NEP during boreal forest succession
We combined year‐round eddy covariance with biometry and biomass harvests along a chronosequence of boreal forest stands that were 1, 6, 15, 23, 40, ∼74, and ∼154 years old to understand how ecosystem production and carbon stocks change during recovery from stand‐replacing crown fire. Live biomass (Clive) was low in the 1‐ and 6‐year‐old stands, and increased following a logistic pattern...
Authors
M. L. Goulden, A.M.S. Mcmillan, G.C. Winston, A.V. Rocha, K.L. Manies, J.W. Harden, B. P. Bond-Lamberty
The effect of fire and permafrost interactions on soil carbon accumulation in an upland black spruce ecosystem of interior Alaska: Implications for post-thaw carbon loss The effect of fire and permafrost interactions on soil carbon accumulation in an upland black spruce ecosystem of interior Alaska: Implications for post-thaw carbon loss
High‐latitude regions store large amounts of organic carbon (OC) in active‐layer soils and permafrost, accounting for nearly half of the global belowground OC pool. In the boreal region, recent warming has promoted changes in the fire regime, which may exacerbate rates of permafrost thaw and alter soil OC dynamics in both organic and mineral soil. We examined how interactions between...
Authors
J. A. O'Donnell, J.W. Harden, A. D. McGuire, M.Z. Kanevskiy, M.T. Jorgenson, X. Xu
Water and heat transport in boreal soils: Implications for soil response to climate change Water and heat transport in boreal soils: Implications for soil response to climate change
Soil water content strongly affects permafrost dynamics by changing the soil thermal properties. However, the movement of liquid water, which plays an important role in the heat transport of temperate soils, has been under-represented in boreal studies. Two different heat transport models with and without convective heat transport were compared to measurements of soil temperatures in...
Authors
Z. Fan, J. C. Neff, J.W. Harden, T. Zhang, H. Veldhuis, C.I. Czimczik, G.C. Winston, J. A. O'Donnell
Recent acceleration of biomass burning and carbon losses in Alaskan forests and peatlands Recent acceleration of biomass burning and carbon losses in Alaskan forests and peatlands
Climate change has increased the area affected by forest fires each year in boreal North America. Increases in burned area and fire frequency are expected to stimulate boreal carbon losses. However, the impact of wildfires on carbon emissions is also affected by the severity of burning. How climate change influences the severity of biomass burning has proved difficult to assess. Here, we...
Authors
M.R. Turetsky, E.S. Kane, J.W. Harden, R.D. Ottmar, K.L. Manies, E. Hoy, E.S. Kasischke
*Disclaimer: Listing outside positions with professional scientific organizations on this Staff Profile are for informational purposes only and do not constitute an endorsement of those professional scientific organizations or their activities by the USGS, Department of the Interior, or U.S. Government