Publication Index | NGEE Arctic

1. 21st century tundra shrubification could enhance net carbon uptake of North America Arctic tundra under an RCP8.5 climate trajectory
2. A best-practice guide to predicting plant traits from leaf-level hyperspectral data using partial least squares regression
3. A distributed temperature profiling method for assessing spatial variability in ground temperatures in a discontinuous permafrost region of Alaska
4. A distributed temperature profiling system for vertically and laterally dense acquisition of soil and snow temperature
5. A global scale mechanistic model of photosynthetic capacity (LUNA V1.0)
6. A global trait-based approach to estimate leaf nitrogen functional allocation from observations
7. A hybrid reduced-order model of fine-resolution hydrologic simulations at a polygonal tundra site
8. A method for experimental heating of intact soil profiles for application to climate change experiments
9. A microbial functional group-based module for simulating methane production and consumption: Application to an incubated permafrost soil
10. A Model of Ice Wedge Polygon Drainage in Changing Arctic Terrain
11. A modeling toolbox for permafrost landscapes
12. A multi-scale comparison of modeled and observed seasonal methane emissions in northern wetlands
13. A Multi-Sensor Unoccupied Aerial System Improves Characterization of Vegetation Composition and Canopy Properties in the Arctic Tundra
14. A new theory of plant-microbe nutrient competition resolves inconsistencies between observations and model predictions
15. A pan-Arctic synthesis of CH 4 and CO 2 production from anoxic soil incubations
16. A reduced-order modeling approach to represent subgrid-scale hydrological dynamics for land-surface simulations: application in a polygonal tundra landscape
17. A reporting format for leaf-level gas exchange data and metadata
18. A roadmap for improving the representation of photosynthesis in Earth system models
19. A rock-physics investigation of unconsolidated saline permafrost: P-wave properties from laboratory ultrasonic measurements
20. A simplified, data-constrained approach to estimate the permafrost carbon–climate feedback
21. A subgrid approach for modeling microtopography effects on overland flow
22. A synthesis dataset of permafrost-affected soil thermal conditions for Alaska, USA
23. A test of the ‘one-point method’ for estimating maximum carboxylation capacity from field-measured, light-saturated photosynthesis
24. A theory of effective microbial substrate affinity parameters in variably saturated soils and an example application to aerobic soil heterotrophic respiration
25. A total quasi-steady-state formulation of substrate uptake kinetics in complex networks and an example application to microbial litter decomposition
26. A zero-power warming chamber for investigating plant responses to rising temperature
27. Accelerated nutrient cycling and increased light competition will lead to 21st century shrub expansion in North American Arctic tundra
28. Acclimation and adaptation components of the temperature dependence of plant photosynthesis at the global scale
29. Active layer hydrology in an arctic tundra ecosystem: quantifying water sources and cycling using water stable isotopes
30. Active layer thickness as a function of soil water content
31. Active-Layer soil moisture content regional variations in Alaska and Russia by ground-based and satellite-based methods, 2002 through 2014
32. Addressing numerical challenges in introducing a reactive transport code into a land surface model: a biogeochemical modeling proof-of-concept with CLM–PFLOTRAN 1.0
33. Age and chemistry of dissolved organic carbon reveal enhanced leaching of ancient labile carbon at the permafrost thaw zone
34. Alaskan carbon-climate feedbacks will be weaker than inferred from short-term experiments
35. Alaskan carbon-climate feedbacks will be weaker than inferred from short-term manipulations
36. Alder distribution and expansion across a tundra hillslope: Implications for local N cycling
37. An assessment of the carbon balance of Arctic tundra: comparisons among observations, process models, and atmospheric inversions
38. An effective-medium model for P-wave velocities of saturated, unconsolidated saline permafrost
39. An intermediate-scale model for thermal hydrology in low-relief permafrost-affected landscapes
40. Anaerobic respiration pathways and response to increased substrate availability of Arctic wetland soils
41. Applicability of the ecosystem type approach to model permafrost dynamics across the Alaska North Slope
42. Arctic Hydrology, Permafrost and EcosystemsResponses of Boreal Forest Ecosystems and Permafrost to Climate Change and Disturbances: A Modeling Perspective
43. Arctic landscapes in transition: Responses to thawing permafrost
44. Arctic soil governs whether climate change drives global losses or gains in soil carbon
45. Arctic soil patterns analogous to fluid instabilitiesSignificance
46. Arctic tundra ice-wedge landscape characterization by active contours without edges and structural analysis using high-resolution satellite imagery
47. Arctic tundra shrubification: a review of mechanisms and impacts on ecosystem carbon balance
48. Arctic vegetation mapping using unsupervised training datasets and convolutional neural networks
49. Assessing dynamic vegetation model parameter uncertainty across Alaskan arctic tundra plant communities
50. Assessing impacts of plant stoichiometric traits on terrestrial ecosystem carbon accumulation using the E3SM land model
51. Beyond ecosystem modeling: A roadmap to community cyberinfrastructure for ecological data‐model integration
52. Biogeochemical model of CO2 and CH4 production in anoxic Arctic soil microcosms
53. Brief communication: Rapid machine-learning-based extraction and measurement of ice wedge polygons in high-resolution digital elevation models
54. Building a Culture of Safety and Trust in Team Science
55. Changes in precipitation and air temperature contribute comparably to permafrost degradation in a warmer climate
56. Characterization of iron oxide nanoparticle films at the air–water interface in Arctic tundra waters
57. Characterizing coarse-resolution watershed soil moisture heterogeneity using fine-scale simulations and reduced-order models
58. Chemostatic concentration–discharge behaviour observed in a headwater catchment underlain with discontinuous permafrost
59. Circumpolar distribution and carbon storage of thermokarst landscapes
60. Climate change and the permafrost carbon feedback
61. Climate change: A controlled experiment
62. Climate policy implications of nonlinear decline of Arctic land permafrost and other cryosphere elements
63. Coincident aboveground and belowground autonomous monitoring to quantify covariability in permafrost, soil, and vegetation properties in Arctic tundra
64. Competitor and substrate sizes and diffusion together define enzymatic depolymerization and microbial substrate uptake rates
65. Conceptualizing Biogeochemical Reactions With an Ohm's Law Analogy
66. Consequences of changes in vegetation and snow cover for climate feedbacks in Alaska and northwest Canada
67. Consequences of permafrost degradation for Arctic infrastructure – bridging the model gap between regional and engineering scales
68. Constitutive model for unfrozen water content in subfreezing unsaturated soils
69. Continuously amplified warming in the Alaskan Arctic: Implications for estimating global warming hiatus
70. Controls on fine-scale spatial and temporal variability of plant-available inorganic nitrogen in a polygonal tundra landscape
71. Convolutional Neural Network Approach for Mapping Arctic Vegetation Using Multi-Sensor Remote Sensing Fusion
72. Convolutional neural network approach for mapping Arctic vegetation using multi-sensor remote sensing fusion
73. Coupled land surface-subsurface hydrogeophysical inverse modeling to estimate soil organic content and explore associated hydrological and thermal dynamics in an Arctic tundra
74. Coupling surface flow and subsurface flow in complex soil structures using mimetic finite differences
75. Co‐producing knowledge: the Integrated Ecosystem Model for resource management in Arctic Alaska
76. Deep Yedoma permafrost: A synthesis of depositional characteristics and carbon vulnerability
77. Dependence of the evolution of carbon dynamics in the northern permafrost region on the trajectory of climate change
78. Depth-resolved physicochemical characteristics of active layer and permafrost soils in an Arctic polygonal tundra region
79. Detecting regional patterns of changing CO 2 flux in Alaska
80. Detecting the permafrost carbon feedback: Talik formation and increased cold-seasonrespiration as precursors to sink-to-source transitions
81. Disentangling the complexity of permafrost soil by using high resolution profiling of microbial community composition, key functions and respiration rates
82. Drainage subsidence associated with Arctic permafrost degradation
83. Effect of soil property uncertainties on permafrost thaw projections: a calibration-constrained analysis
84. Effects of warming on the degradation and production of low-molecular-weight labile organic carbon in an Arctic tundra soil
85. Electrical and seismic response of saline permafrost soil during freeze - Thaw transition
86. Electrical conductivity imaging of active layer and permafrost in an arctic ecosystem, through advanced inversion of electromagnetic induction data
87. Enhancing global change experiments through integration of remote‐sensing techniques
88. Enhancing terrestrial ecosystem sciences by integrating empirical modeling approaches
89. Estimation of subsurface porosities and thermal conductivities of polygonal tundra by coupled inversion of electrical resistivity, temperature, and moisture content data
90. Evaluating integrated surface/subsurface permafrost thermal hydrology models in ATS (v0.88) against observations from a polygonal tundra site
91. Evaluating temporal controls on greenhouse gas (GHG) fluxes in an Arctic tundra environment: An entropy-based approach
92. Evaluation of an untargeted nano-liquid chromatography-mass spectrometry approach to expand coverage of low molecular weight dissolved organic matter in Arctic soil
93. Evaporation dominates evapotranspiration on Alaska’s Arctic Coastal Plain
94. Evapotranspiration across plant types and geomorphological units in polygonal Arctic tundra
95. Expansion of high-latitude deciduous forests driven by interactions between climate warming and fire
96. Exploring the Role of Cryptic Nitrogen Fixers in Terrestrial Ecosystems: A Frontier in Nitrogen Cycling Research
97. Extrapolating active layer thickness measurements across Arctic polygonal terrain using LiDAR and NDVI data sets
98. From documentation to prediction: How remote sensing and mechanistic modeling are raising the bar for thermokarst research.
99. From the Arctic to the tropics: Multibiome prediction of leaf mass per area using leaf reflectance
100. Full-wavefield inversion of surface waves for mapping embedded low-velocity zones in permafrost
101. Future increases in Arctic lightning and fire risk for permafrost carbon
102. Genomics in a changing arctic: critical questions await the molecular ecologist
103. Geochemical drivers of organic matter decomposition in arctic tundra soils
104. Geomorphological and geochemistry changes in permafrost after the 2002 tundra wildfire in Kougarok, Seward Peninsula, Alaska
105. Geophysical estimation of shallow permafrost distribution and properties in an ice-wedge polygon-dominated Arctic tundra region
106. Geophysical Monitoring Shows that Spatial Heterogeneity in Thermohydrological Dynamics Reshapes a Transitional Permafrost System
107. Global pattern and controls of soil microbial metabolic quotient
108. Global photosynthetic capacity is optimized to the environment
109. Global-scale environmental control of plant photosynthetic capacity
110. Groundwater flow and heat transport for systems undergoing freeze-thaw: Intercomparison of numerical simulators for 2D test cases
111. High temporal and spatial variability of nitrate on an Alaskan hillslope dominated by alder shrubs
112. High-resolution mapping of spatial heterogeneity in ice wedge polygon geomorphology near Prudhoe Bay, Alaska
113. High-Resolution Spatio-Temporal Estimation of Net Ecosystem Exchange in Ice-Wedge Polygon Tundra Using In Situ Sensors and Remote Sensing Data
114. Hybrid-energy module for remote environmental observations, instruments, and communications
115. Hysteretic temperature sensitivity of wetland CH4 fluxes explained by substrate availability and microbial activity
116. ICESat GLAS elevation changes and ALOS PALSAR InSAR line-of-sight changes on the continuous permafrost zone of the North Slope, Alaska
117. Identifying multiscale zonation and assessing the relative importance of polygon geomorphology on carbon fluxes in an Arctic tundra ecosystem
118. Impacts of microtopographic snow redistribution and lateral subsurface processes on hydrologic and thermal states in an Arctic polygonal ground ecosystem: A case study using ELM-3D v1.0
119. Impacts of temperature and soil characteristics on methane production and oxidation in Arctic polygonal tundra
120. Importance of feedback loops between soil inorganic nitrogen and microbial communities in the heterotrophic soil respiration response to global warming
121. Improved global-scale predictions of soil carbon stocks with Millennial Version 2
122. Improving representation of photosynthesis in Earth System Models
123. Increased Arctic NO3− Availability as a Hydrogeomorphic Consequence of Permafrost Degradation and Landscape Drying
124. Indexing permafrost soil organic matter degradation using high-resolution mass spectrometry
125. Influence of iron redox cycling on organo-mineral associations in Arctic tundra soil
126. Influence of Tundra Polygon Type and Climate Variability on CO2 and CH4 Fluxes Near Utqiagvik, Alaska
127. Influences and interactions of inundation, peat, and snow on active layer thickness
128. Influences of Hillslope Biogeochemistry on Anaerobic Soil Organic Matter Decomposition in a Tundra Watershed
129. InSAR detection and field evidence for thermokarst after a tundra wildfire, using ALOS-PALSAR
130. Integrated surface/subsurface permafrost thermal hydrology: Model formulation and proof-of-concept simulations
131. Integrating Arctic Plant Functional Types in a Land Surface Model Using Above‐ and Belowground Field Observations
132. Integrating empirical-modeling approaches to improve understanding of terrestrial ecology processes
133. Ion concentrations in ice wedges: An innovative approach to reconstruct past climate variability
134. Iron (oxyhydr)oxides serve as phosphate traps in tundra and boreal peat soils
135. Iron and iron-bound phosphate accumulate in surface soils of ice-wedge polygons in arctic tundra
136. Isotopic identification of soil and permafrost nitrate sources in an Arctic tundra ecosystem
137. Isotopic insights into methane production, oxidation, and emissions in Arctic polygon tundra
138. Land cover classification in multispectral imagery using clustering of sparse approximations over learned feature dictionaries
139. Land Use and Land Cover Affect the Depth Distribution of Soil Carbon: Insights From a Large Database of Soil ProfilesImage_1.PDFTable_1.docx
140. Landscape topography structures the soil microbiome in Arctic polygonal tundra
141. Landscape-scale characterization of Arctic tundra vegetation composition, structure, and function with a multi-sensor unoccupied aerial system
142. Large CO2 and CH4 emissions from polygonal tundra during spring thaw in northern Alaska
143. Large loss of CO2 in winter observed across the northern permafrost region
144. Large uncertainty in permafrost carbon stocks due to hillslope soil deposits
145. Large-Eddy simulations of air flow and turbulence within and around low-aspect-ratio cylindrical open-top chambers
146. Leaf respiration (GlobResp) - global trait database supports Earth System Models
147. Local-scale Arctic tundra heterogeneity affects regional-scale carbon dynamics
148. Long residence times of rapidly decomposable soil organic matter: Application of a multi-phase, multi-component, and vertically resolved model (BAMS1) to soil carbon dynamics
149. Low-Power, Flexible Sensor Arrays with Solderless Board-to-Board Connectors for Monitoring Soil Deformation and Temperature
150. Managing complexity in simulations of land surface and near-surface processes
151. Mapping Arctic plant functional type distributions in the Barrow Environmental Observatory using WorldView-2 and LiDAR datasets
152. Mapping snow depth within a tundra ecosystem using multiscale observations and Bayesian methods
153. Mathematical modeling of Arctic polygonal tundra with Ecosys: 1. Microtopography determines how active layer depths responds to changes in temperature and precipitation
154. Mathematical modeling of Arctic polygonal tundra with Ecosys: 2. Microtopography determines how CO3 and CH4 exchange responds to changes in temperature and precipitation
155. Measuring diurnal cycles of evapotranspiration in the Arctic with an automated chamber system
156. Mechanistic modeling of microtopographic impacts on CO2 and CH4 fluxes in an Alaskan tundra ecosystem using the CLM‐Microbe model
157. Meta-analysis of high-latitude nitrogen-addition and warming studies implies ecological mechanisms overlooked by land models
158. Microbes in thawing permafrost: the unknown variable in the climate change equation
159. Microbial community and functional gene changes in Arctic tundra soils in a microcosm warming experiment
160. Microbial contribution to post-fire tundra ecosystem recovery over the 21st century
161. Microtopographic and depth controls on active layer chemistry in Arctic polygonal ground
162. Microtopographic control on the ground thermal regime in ice wedge polygons
163. Mineral properties, microbes, transport, and plant-input profiles control vertical distribution and age of soil carbon stocks
164. Missing pieces to modeling the Arctic-Boreal puzzle
165. Modeling anaerobic soil organic carbon decomposition in Arctic polygon tundra: Insights into soil geochemical influences on carbon mineralization
166. Modeling challenges for predicting hydrologic response to degrading permafrost
167. Modeling climate change impacts on an Arctic Polygonal Tundra: 1. Rates of permafrost thaw depend on changes in vegetation and drainage
168. Modeling climate change impacts on an Arctic Polygonal Tundra: 2. Changes in CO2 and CH4 exchange depend on rates of permafrost thaw as affected by changes in vegetation and drainage
169. Modeling long-term permafrost degradation
170. Modeling Present and Future Permafrost Distribution at the Seward Peninsula, Alaska
171. Modeling the role of preferential snow accumulation in through talik development and hillslope groundwater flow in a transitional permafrost landscape
172. Modeling the spatiotemporal variability in subsurface thermal regimes across a low-relief polygonal tundra landscape
173. Modelling impacts of recent warming on seasonal carbon exchange in higher latitudes of North America
174. Molecular insights into Arctic soil organic matter degradation under warming
175. NASA's surface biology and geology designated observable: A perspective on surface imaging algorithms
176. Near activation and differential activation in enzymatic reactions
177. New calculations for photosynthesis measurement systems: what's the impact for physiologists and modelers?
178. New insights into the drainage of inundated ice-wedge polygons using fundamental hydrologic principles
179. No evidence for triose phosphate limitation of light‐saturated leaf photosynthesis under current atmospheric CO2 concentration
180. Non-growing season plant nutrient uptake controls Arctic tundra vegetation composition under future climate
181. Non-isothermal, three-phase simulations of near-surface flows in a model permafrost system under seasonal variability and climate change
182. Nonlinear CO2 flux response to 7 years of experimentally induced permafrost thaw
183. Numerical modeling of two-dimensional temperature field dynamics across non-deforming ice-wedge polygons
184. On the relationships between the Michaelis–Menten kinetics, reverse Michaelis–Menten kinetics, equilibrium chemistry approximation kinetics, and quadratic kinetics
185. Open Science principles for accelerating trait-based science across the Tree of Life
186. Optimal stomatal behaviour around the world
187. Pan-Arctic ice-wedge degradation in warming permafrost and its influence on tundra hydrology
188. Pathways and transformations of dissolved methane and dissolved inorganic carbon in Arctic tundra watersheds: Evidence from analysis of stable isotopes
189. Pathways of anaerobic organic matter decomposition in tundra soils from Barrow, Alaska
190. PeRL: A Circum-Arctic permafrost region pond and lake database
191. PeRL: a circum-Arctic permafrost region pond and lake database
192. Permafrost carbon-climate feedbacks accelerate global warming
193. Permafrost carbon−climate feedback is sensitive to deep soil carbon decomposability but not deep soil nitrogen dynamics
194. Permafrost degradation and subsurface-flow changes caused by surface warming trends
195. Permafrost Meta-Omics and climate change
196. Permafrost Promotes Shallow Groundwater Flow and Warmer Headwater Streams
197. Permafrost thaw and resulting soil moisture changes regulate projected high-latitude CO2 and CH4 emissions
198. Permafrost thermal conditions are sensitive to shifts in snow timing
199. Persistence of soil organic carbon caused by functional complexity
200. Planning the Next Generation of Arctic Ecosystem Experiments
201. Plant functional types in Earth system models: past experiences and future directions for application of dynamic vegetation models in high-latitude ecosystems
202. Polygonal tundra geomorphological change in response to warming alters future CO2 and CH4 flux on the Barrow Peninsula
203. Polygonal tundra geomorphological change in response to warming alters future CO2 and CH4 flux on the Barrow Peninsula
204. Potential carbon emissions dominated by carbon dioxide from thawed permafrost soils
205. Potential impacts of mercury released from thawing permafrost
206. Preface: Hydrogeology of cold regions
207. Profile: Stan D. Wullschleger
208. Quantification of Arctic soil and permafrost properties using ground penetrating radar
209. Quantification of Arctic soil and permafrost properties using ground-penetrating radar and electrical resistivity tomography datasets
210. Quantifying and relating land-surface and subsurface variability in permafrost environments using LiDAR and surface geophysical datasets
211. Quantifying pH buffering capacity in acidic, organic-rich Arctic soils: Measurable proxies and implications for soil carbon degradation
212. Range shifts in a foundation sedge potentially induce large Arctic ecosystem carbon losses and gains
213. Rapidly changing high-latitude seasonality: implications for the 21st century carbon cycle in Alaska
214. Reduced arctic tundra productivity linked with landform and climate change interactions
215. Reducing model uncertainty of climate change impacts on high latitude carbon assimilation
216. Remote monitoring of freeze–thaw transitions in Arctic soils using the complex resistivity method
217. Representativeness assessment of the pan-Arctic eddy covariance site network and optimized future enhancements
218. Representativeness-based sampling network design for the State of Alaska
219. Representing leaf and root physiological traits in CLM improves global carbon and nitrogen cycling predictions
220. Reviews and syntheses: Four decades of modeling methane cycling in terrestrial ecosystems
221. Rising plant-mediated methane emissions from Arctic wetlands
222. Root structural and functional dynamics in terrestrial biosphere models - evaluation and recommendations
223. Root traits explain observed tundra vegetation nitrogen uptake patterns: Implications for trait-based land models
224. Root traits explain observed tundra vegetation nitrogen uptake patterns: Implications for trait‐based land models
225. Saturated N2O emission rates occur above the nitrogen deposition level predicted for the semi-arid grasslands of Inner Mongolia, China
226. Scaling-up permafrost thermal measurements in western Alaska using an ecotype approach
227. Second-order accurate finite volume schemes with the discrete maximum principle for solving Richards’ equation on unstructured meshes
228. Sensitivity evaluation of the Kudryavtsev permafrost model
229. Shallow soils are warmer under trees and tall shrubs across Arctic and Boreal ecosystems
230. Size distributions of Arctic waterbodies reveal consistent relations in their statistical moments in space and time
231. Soil moisture and hydrology projections of the permafrost region – a model intercomparison
232. Soil respiration strongly offsets carbon uptake in Alaska and Northwest Canada
233. Spatial and temporal variations of thaw layer thickness and its controlling factors identified using time-lapse electrical resistivity tomography and hydro-thermal modeling
234. Spatial distribution of thermokarst terrain in Arctic Alaska
235. Spatial patterns of snow distribution for improved Earth system modelling in the Arctic
236. Sphagnum physiology in the context of changing climate: emergent influences of genomics, modelling and host-microbiome interactions on understanding ecosystem function
237. Statistical upscaling of ecosystem CO 2 fluxes across the terrestrial tundra and boreal domain: Regional patterns and uncertainties
238. Stoichiometry and temperature sensitivity of methanogenesis and CO2 production from saturated polygonal tundra in Barrow, Alaska
239. Sub-aerial talik formation observed across the discontinuous permafrost zone of Alaska
240. SUPECA kinetics for scaling redox reactions in networks of mixed substrates and consumers and an example application to aerobic soil respiration
241. Technical Note: A generic law-of-the-minimum flux limiter for simulating substrate limitation in biogeochemical models
242. Technical Note: Simple formulations and solutions of the dual-phase diffusive transport for biogeochemical modeling
243. Temperature sensitivity of mineral-enzyme interactions on the hydrolysis of cellobiose and indican by β-glucosidase
244. Temporal, Spatial, and Temperature Controls on Organic Carbon Mineralization and Methanogenesis in Arctic High-Centered Polygon SoilsData_Sheet_1.docx
245. Terrestrial biosphere models may overestimate Arctic
246. Terrestrial biosphere models underestimate photosynthetic capacity and CO2 assimilation in the Arctic
247. The Alaska Arctic vegetation archive (AVA-AK)
248. The effect of temperature on the rate, affinity, and 15N fractionation of NO3 − during biological denitrification in soils
249. The fungal collaboration gradient dominates the root economics space in plants
250. The impacts of recent permafrost thaw on land–atmosphere greenhouse gas exchange
251. The integrated hydrologic model intercomparison project, IH-MIP2: A second set of benchmark results to diagnose integrated hydrology and feedbacks
252. The microbial ecology of permafrost
253. The role of advective heat transport in talik development beneath lakes and ponds in discontinuous permafrost
254. The State of the Climate in 2019: The Arctic
255. The unseen iceberg: plant roots in arctic tundra
256. The use and misuse of Vc,max in Earth System Models
257. The “one‐point method” for estimating maximum carboxylation capacity of photosynthesis: A cautionary tale
258. Thermal effects of groundwater flow through subarctic fens: A case study based on field observations and numerical modeling
259. Three-phase numerical model for subsurface hydrology in permafrost-affected regions (PFLOTRAN-ICE v1.0)
260. Timing and duration of hydrological transitions in Arctic polygonal ground from stable isotopes
261. Timing and duration of hydrological transitions in Arctic polygonal ground from stable isotopes
262. Topographical Controls on Hillslope‐Scale Hydrology Drive Shrub Distributions on the Seward Peninsula, Alaska
263. Toward a mechanistic modeling of nitrogen limitation on vegetation dynamics
264. Trait covariance: the functional warp of plant diversity?
265. Trait-Based representation of biological nitrification: Model development, testing, and predicted community composition
266. Trajectory of the Arctic as an integrated system
267. Triose phosphate limitation in photosynthesis models reduces leaf photosynthesis and global terrestrial carbon storage
268. Triose phosphate utilization limitation: an unnecessary complexity in terrestrial biosphere model representation of photosynthesis
269. TRY plant trait database – Enhanced coverage and open access
270. Tundra landform and vegetation productivity trend maps for the Arctic Coastal Plain of northern Alaska
271. Understanding the relative importance of vertical and horizontal flow in ice-wedge polygons
272. Unravelling biogeochemical drivers of methylmercury production in an Arctic fen soil and a bog soil
273. Untargeted Exometabolomics Provides a Powerful Approach to Investigate Biogeochemical Hotspots with Vegetation and Polygon Type in Arctic Tundra Soils
274. Use of a metadata documentation and search tool for large data volumes: The NGEE arctic example
275. Using field observations to inform thermal hydrology models of permafrost dynamics with ATS (v0.83)
276. Using model reduction to predict the soil-surface C18OO flux: an example of representing complex biogeochemical dynamics in a computationally efficient manner
277. Using MODIS estimates of fractional snow cover area to improve streamflow forecasts in interior Alaska
278. Variability in the sensitivity among model simulations of permafrost and carbon dynamics in the permafrost region between 1960 and 2009
279. Variations of soil microbial community structures beneath broadleaved forest trees in temperate and subtropical climate zones
280. Warming increases methylmercury production in an Arctic soil
281. Water balance response of permafrost-affected watersheds to changes in air temperatures
282. Weaker soil carbon–climate feedbacks resulting from microbial and abiotic interactions
283. WETCHIMP-WSL: Intercomparison of wetland methane emissions models over West Siberia