Modeling long-term changes in tundra carbon balance following wildfire, climate change and potential nutrient addition. Ecological Applications. 2017 ;27(1):105–117 ..
C–N–P interactions control climate driven changes in regional patterns of C storage on the North Slope of Alaska. Landscape Ecology. 2016 ;31(1):195 - 213..
Contrasting soil thermal responses to fire in Alaskan tundra and boreal forest. Journal of Geophysical Research: Earth Surface. 2015 ;120(2):363-378..
Modeling carbon–nutrient interactions during the early recovery of tundra after fire. Ecological Applications. 2015 ;25(6):1640 - 1652..
Assessing the spatial variability in peak season CO2 exchange characteristics across the Arctic tundra using a light response curve parameterization. Biogeosciences. 2014 ;11:4897-4912.
Change in surface energy balance in Alaska due to fire and spring warming, based on upscaling eddy covariance measurements. Journal of Geophysical Research: Biogeosciences. 2014 ;119(10):1947-1969..
Disturbance legacies and climate jointly drive tree growth and mortality in an intensively studied boreal forest. Global Change Biology. 2014 ;20:216-227..
Effect of vegetation phenology and stomatal coupling on carbon and water fluxes in arctic tundra. Environmental Change Initiative Postdoc Symposium and Reception. 2014 ..
Latent heat exchange in the boreal and arctic biomes. Global Change Biology. 2014 ;20(11):3439–3456.
Macrosystems ecology: understanding ecological patterns and processes at continental scales. Frontiers in Ecology and the Environment. 2014 ;12(1):5-14.
Ecosystem resilience and climate feedbacks in an arctic with fire (Invited Speaker). Grand Valley State University. 2013 ..
Identification of unrecognized tundra fire events on the north slope of Alaska. Journal of Geophysical Research: Biogeosciences. 2013 ;118:1334-1344..
Panarctic modeling of net ecosystem exchange of CO2. Philosophical Transactions of Royal Society: Biology. 2013 ;368(1624):20120485..
Phenological responses of tundra plants to background climate warming tested using the International Tundra Experiment. Philosophical Transactions of Royal Society: Biology. 2013 ;368(1624):2012481.
The footprint of Alaskan tundra fires during the past half-century: implications for surface properties and radiative forcing. Environmental Research Letters [Internet]. 2012 ;7(4):044039. Available from: http://stacks.iop.org/1748-9326/7/i=4/a=044039.
Vegetation shifts observed in arctic tundra 17 years after fire. Remote Sensing Letters [Internet]. 2012 ;3(8):729-736. Available from: http://dx.doi.org/10.1080/2150704X.2012.676741.
Burn severity influences postfire CO2 exchange in arctic tundra. Ecological Applications [Internet]. 2011 ;21(2):477-89. Available from: http://www.ncbi.nlm.nih.gov/pubmed/21563578.
Cross-system comparisons elucidate disturbance complexities and generalities. Ecosphere. 2011 ;2(7):3-26..
Postfire energy exchange in arctic tundra: the importance and climatic implications of burn severity. Global Change Biology [Internet]. 2011 ;17(9):2831-2841. Available from: <Go to ISI>://WOS:000293399000005.
Scaling an instantaneous model of tundra NEE to the Arctic landscape. Ecosystems. 2011 ;14(1):76-93..
Understanding burn severity sensing in Arctic tundra: exploring vegetation indices, suboptimal assessment timing and the impact of increasing pixel size. International Journal of Remote Sensing. 2011 ;32(2):7033-7056..
Drought legacies influence the long-term carbon balance of a freshwater marsh. Journal of Geophysical Research: Biogeosciences. 2010 ;115(G3):9 pp..
Advantages of a two band EVI calculated from solar and photosynthetically active radiation fluxes. Agricultural and Forest Meteorology [Internet]. 2009 ;149(9):1560-1563. Available from: http://dx.doi.org/10.1016/j.agrformet.2009.03.016.
Albedo vs. energy budget partitioning: effects on climate. Notre Dame, IN: University of Notre Dame.