Jennifer Harden, PhD (Former Employee)
Science and Products
Filter Total Items: 144
A new data set for estimating organic carbon storage to 3 m depth in soils of the northern circumpolar permafrost region A new data set for estimating organic carbon storage to 3 m depth in soils of the northern circumpolar permafrost region
High-latitude terrestrial ecosystems are key components in the global carbon cycle. The Northern Circumpolar Soil Carbon Database (NCSCD) was developed to quantify stocks of soil organic carbon (SOC) in the northern circumpolar permafrost region (a total area of 18.7 × 106 km2). The NCSCD is a geographical information system (GIS) data set that has been constructed using harmonized...
Authors
G. Hugelius, James G. Bockheim, P. Camill, B. Elberling, G. Grosse, J.W. Harden, Kevin Johnson, T. Jorgenson, C.D. Koven, P. Kuhry, G. Michaelson, U. Mishra, J. Palmtag, C.-L. Ping, J. O'Donnell, L. Schirrmeister, E.A.G. Schuur, Y. Sheng, L.C. Smith, J. Strauss, Z. Yu
Soil data from fire and permafrost-thaw chronosequences in upland Picea mariana stands near Hess Creek and Tok, interior Alaska Soil data from fire and permafrost-thaw chronosequences in upland Picea mariana stands near Hess Creek and Tok, interior Alaska
Soils of the Northern Circumpolar Permafrost region harbor 1,672 petagrams (Pg) (1 Pg = 1,000,000,000 kilograms) of organic carbon (OC), nearly 50 percent of the global belowground OC pool (Tarnocai and others, 2009). Of that soil OC, nearly 88 percent is presently stored in perennially frozen ground. Recent climate warming at northern latitudes has resulted in warming and thawing of...
Authors
Jonathan A. O’Donnell, Jennifer W. Harden, Kristen L. Manies, M. Torre Jorgenson, Mikhail Kanevskiy, Xiaomei Xu
The response of soil organic carbon of a rich fen peatland in interior Alaska to projected climate change The response of soil organic carbon of a rich fen peatland in interior Alaska to projected climate change
It is important to understand the fate of carbon in boreal peatland soils in response to climate change because a substantial change in release of this carbon as CO2 and CH4 could influence the climate system. The goal of this research was to synthesize the results of a field water table manipulation experiment conducted in a boreal rich fen into a process-based model to understand how...
Authors
Zhaosheng Fan, Anthony David McGuire, Merritt R. Turetsky, Jennifer W. Harden, James Michael Waddington, Evan S. Kane
Response of anaerobic carbon cycling to water table manipulation in an Alaskan rich fen Response of anaerobic carbon cycling to water table manipulation in an Alaskan rich fen
To test the effects of altered hydrology on organic soil decomposition, we investigated CO2 and CH4 production potential of rich-fen peat (mean surface pH = 6.3) collected from a field water table manipulation experiment including control, raised and lowered water table treatments. Mean anaerobic CO2 production potential at 10 cm depth (14.1 ± 0.9 μmol C g−1 d−1) was as high as aerobic...
Authors
E.S. Kane, M.R. Chivers, M.R. Turetsky, Claire C. Treat, D.G. Petersen, M. Waldrop, J.W. Harden, A. D. McGuire
Empirical estimates to reduce modeling uncertainties of soil organic carbon in permafrost regions: a review of recent progress and remaining challenges Empirical estimates to reduce modeling uncertainties of soil organic carbon in permafrost regions: a review of recent progress and remaining challenges
The vast amount of organic carbon (OC) stored in soils of the northern circumpolar permafrost region is a potentially vulnerable component of the global carbon cycle. However, estimates of the quantity, decomposability, and combustibility of OC contained in permafrost-region soils remain highly uncertain, thereby limiting our ability to predict the release of greenhouse gases due to...
Authors
U. Mishra, J.D. Jastrow, R. Matamala, G. Hugelius, C.D. Koven, Jennifer W. Harden, S.L. Ping, G.J. Michaelson, Z. Fan, R.M. Miller, A. D. McGuire, C. Tarnocai, P. Kuhry, W.J. Riley, K. Schaefer, E.A.G. Schuur, M.T. Jorgenson, L. D. Hinzman
Reorganization of vegetation, hydrology and soil carbon after permafrost degradation across heterogeneous boreal landscapes Reorganization of vegetation, hydrology and soil carbon after permafrost degradation across heterogeneous boreal landscapes
The diversity of ecosystems across boreal landscapes, successional changes after disturbance and complicated permafrost histories, present enormous challenges for assessing how vegetation, water and soil carbon may respond to climate change in boreal regions. To address this complexity, we used a chronosequence approach to assess changes in vegetation composition, water storage and soil...
Authors
M. Torre Jorgenson, Jennifer Harden, Mikhail Kanevskiy, Jonathan O'Donnell, Kim Wickland, Stephanie Ewing, Kristen Manies, Qianlai Zhuang, Yuri Shur, Robert G. Striegl, Joshua C. Koch
Science and Products
Filter Total Items: 144
A new data set for estimating organic carbon storage to 3 m depth in soils of the northern circumpolar permafrost region A new data set for estimating organic carbon storage to 3 m depth in soils of the northern circumpolar permafrost region
High-latitude terrestrial ecosystems are key components in the global carbon cycle. The Northern Circumpolar Soil Carbon Database (NCSCD) was developed to quantify stocks of soil organic carbon (SOC) in the northern circumpolar permafrost region (a total area of 18.7 × 106 km2). The NCSCD is a geographical information system (GIS) data set that has been constructed using harmonized...
Authors
G. Hugelius, James G. Bockheim, P. Camill, B. Elberling, G. Grosse, J.W. Harden, Kevin Johnson, T. Jorgenson, C.D. Koven, P. Kuhry, G. Michaelson, U. Mishra, J. Palmtag, C.-L. Ping, J. O'Donnell, L. Schirrmeister, E.A.G. Schuur, Y. Sheng, L.C. Smith, J. Strauss, Z. Yu
Soil data from fire and permafrost-thaw chronosequences in upland Picea mariana stands near Hess Creek and Tok, interior Alaska Soil data from fire and permafrost-thaw chronosequences in upland Picea mariana stands near Hess Creek and Tok, interior Alaska
Soils of the Northern Circumpolar Permafrost region harbor 1,672 petagrams (Pg) (1 Pg = 1,000,000,000 kilograms) of organic carbon (OC), nearly 50 percent of the global belowground OC pool (Tarnocai and others, 2009). Of that soil OC, nearly 88 percent is presently stored in perennially frozen ground. Recent climate warming at northern latitudes has resulted in warming and thawing of...
Authors
Jonathan A. O’Donnell, Jennifer W. Harden, Kristen L. Manies, M. Torre Jorgenson, Mikhail Kanevskiy, Xiaomei Xu
The response of soil organic carbon of a rich fen peatland in interior Alaska to projected climate change The response of soil organic carbon of a rich fen peatland in interior Alaska to projected climate change
It is important to understand the fate of carbon in boreal peatland soils in response to climate change because a substantial change in release of this carbon as CO2 and CH4 could influence the climate system. The goal of this research was to synthesize the results of a field water table manipulation experiment conducted in a boreal rich fen into a process-based model to understand how...
Authors
Zhaosheng Fan, Anthony David McGuire, Merritt R. Turetsky, Jennifer W. Harden, James Michael Waddington, Evan S. Kane
Response of anaerobic carbon cycling to water table manipulation in an Alaskan rich fen Response of anaerobic carbon cycling to water table manipulation in an Alaskan rich fen
To test the effects of altered hydrology on organic soil decomposition, we investigated CO2 and CH4 production potential of rich-fen peat (mean surface pH = 6.3) collected from a field water table manipulation experiment including control, raised and lowered water table treatments. Mean anaerobic CO2 production potential at 10 cm depth (14.1 ± 0.9 μmol C g−1 d−1) was as high as aerobic...
Authors
E.S. Kane, M.R. Chivers, M.R. Turetsky, Claire C. Treat, D.G. Petersen, M. Waldrop, J.W. Harden, A. D. McGuire
Empirical estimates to reduce modeling uncertainties of soil organic carbon in permafrost regions: a review of recent progress and remaining challenges Empirical estimates to reduce modeling uncertainties of soil organic carbon in permafrost regions: a review of recent progress and remaining challenges
The vast amount of organic carbon (OC) stored in soils of the northern circumpolar permafrost region is a potentially vulnerable component of the global carbon cycle. However, estimates of the quantity, decomposability, and combustibility of OC contained in permafrost-region soils remain highly uncertain, thereby limiting our ability to predict the release of greenhouse gases due to...
Authors
U. Mishra, J.D. Jastrow, R. Matamala, G. Hugelius, C.D. Koven, Jennifer W. Harden, S.L. Ping, G.J. Michaelson, Z. Fan, R.M. Miller, A. D. McGuire, C. Tarnocai, P. Kuhry, W.J. Riley, K. Schaefer, E.A.G. Schuur, M.T. Jorgenson, L. D. Hinzman
Reorganization of vegetation, hydrology and soil carbon after permafrost degradation across heterogeneous boreal landscapes Reorganization of vegetation, hydrology and soil carbon after permafrost degradation across heterogeneous boreal landscapes
The diversity of ecosystems across boreal landscapes, successional changes after disturbance and complicated permafrost histories, present enormous challenges for assessing how vegetation, water and soil carbon may respond to climate change in boreal regions. To address this complexity, we used a chronosequence approach to assess changes in vegetation composition, water storage and soil...
Authors
M. Torre Jorgenson, Jennifer Harden, Mikhail Kanevskiy, Jonathan O'Donnell, Kim Wickland, Stephanie Ewing, Kristen Manies, Qianlai Zhuang, Yuri Shur, Robert G. Striegl, Joshua C. Koch
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