1. Fine-scale landscape characteristics, vegetation composition, and snowmelt timing control phenological heterogeneity across low-Arctic tundra landscapes in Western Alaska
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 model parameter sensitivity approach to understand soil thermal and hydrological linkages and their influence on ecosystem carbon dynamics
12. A modeling toolbox for permafrost landscapes
13. A multi-scale comparison of modeled and observed seasonal methane emissions in northern wetlands
14. A Multi-Sensor Unoccupied Aerial System Improves Characterization of Vegetation Composition and Canopy Properties in the Arctic Tundra
15. A new theory of plant-microbe nutrient competition resolves inconsistencies between observations and model predictions
16. A pan-Arctic synthesis of methane and carbon dioxide production from anoxic soil incubations
17. A reduced-order modeling approach to represent subgrid-scale hydrological dynamics for land-surface simulations: application in a polygonal tundra landscape
18. A reporting format for leaf-level gas exchange data and metadata
19. A roadmap for improving the representation of photosynthesis in Earth system models
20. A rock-physics investigation of unconsolidated saline permafrost: P-wave properties from laboratory ultrasonic measurements
21. A simplified, data-constrained approach to estimate the permafrost carbon–climate feedback
22. A subgrid approach for modeling microtopography effects on overland flow
23. A synthesis dataset of permafrost-affected soil thermal conditions for Alaska, USA
24. A test of the ‘one-point method’ for estimating maximum carboxylation capacity from field-measured, light-saturated photosynthesis
25. A theory of effective microbial substrate affinity parameters in variably saturated soils and an example application to aerobic soil heterotrophic respiration
26. A total quasi-steady-state formulation of substrate uptake kinetics in complex networks and an example application to microbial litter decomposition
27. A zero-power warming chamber for investigating plant responses to rising temperature
28. Abiotic and Biotic Controls on Soil Organo–Mineral Interactions: Developing Model Structures to Analyze Why Soil Organic Matter Persists
29. Accelerated nutrient cycling and increased light competition will lead to 21st century shrub expansion in North American Arctic tundra
30. Acclimation and adaptation components of the temperature dependence of plant photosynthesis at the global scale
31. Active layer hydrology in an arctic tundra ecosystem: quantifying water sources and cycling using water stable isotopes
32. Active layer thickness as a function of soil water content
33. Active-Layer soil moisture content regional variations in Alaska and Russia by ground-based and satellite-based methods, 2002 through 2014
34. 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
35. Age and chemistry of dissolved organic carbon reveal enhanced leaching of ancient labile carbon at the permafrost thaw zone
36. Alaskan carbon-climate feedbacks will be weaker than inferred from short-term experiments
37. Alaskan carbon-climate feedbacks will be weaker than inferred from short-term manipulations
38. Alder distribution and expansion across a tundra hillslope: Implications for local N cycling
39. An assessment of the carbon balance of Arctic tundra: comparisons among observations, process models, and atmospheric inversions
40. An effective-medium model for P-wave velocities of saturated, unconsolidated saline permafrost
41. An intermediate-scale model for thermal hydrology in low-relief permafrost-affected landscapes
42. An ultrahigh-resolution E3SM land model simulation framework and its first application to the Seward Peninsula in Alaska
43. Anaerobic respiration pathways and response to increased substrate availability of Arctic wetland soils
44. Applicability of the ecosystem type approach to model permafrost dynamics across the Alaska North Slope
45. Arctic landscapes in transition: Responses to thawing permafrost
46. Arctic permafrost
47. Arctic soil governs whether climate change drives global losses or gains in soil carbon
48. Arctic soil patterns analogous to fluid instabilities
49. Arctic tundra ice-wedge landscape characterization by active contours without edges and structural analysis using high-resolution satellite imagery
50. Arctic tundra shrubification: a review of mechanisms and impacts on ecosystem carbon balance
51. Arctic vegetation mapping using unsupervised training datasets and convolutional neural networks
52. Assessing dynamic vegetation model parameter uncertainty across Alaskan arctic tundra plant communities
53. Assessing dynamic vegetation model parameter uncertainty across Alaskan arctic tundra plant communities
54. Assessing dynamic vegetation model parameter uncertainty across Alaskan arctic tundra plant communities
55. Assessing impacts of plant stoichiometric traits on terrestrial ecosystem carbon accumulation using the E3SM land model
56. Beyond ecosystem modeling: A roadmap to community cyberinfrastructure for ecological data‐model integration
57. Biogeochemical model of carbon dioxide and methane production in anoxic Arctic soil microcosms
58. Bridging gaps in permafrost-shrub understanding
59. Brief communication: Monitoring snow depth using small, cheap, and easy-to-deploy snow–ground interface temperature sensors
60. Brief communication: Rapid machine-learning-based extraction and measurement of ice wedge polygons in high-resolution digital elevation models
61. Building a Culture of Safety and Trust in Team Science
62. Canopy cover and microtopography control precipitation-enhanced thaw of ecosystem-protected permafrost
63. Changes in precipitation and air temperature contribute comparably to permafrost degradation in a warmer climate
64. Changing characteristics of runoff and freshwater export from watersheds draining northern Alaska
65. Characterization of iron oxide nanoparticle films at the air–water interface in Arctic tundra waters
66. Characterizing coarse-resolution watershed soil moisture heterogeneity using fine-scale simulations and reduced-order models
67. Chemostatic concentration–discharge behaviour observed in a headwater catchment underlain with discontinuous permafrost
68. Circumpolar distribution and carbon storage of thermokarst landscapes
69. Climate change and the permafrost carbon feedback
70. Climate change: A controlled experiment
71. Climate policy implications of nonlinear decline of Arctic land permafrost and other cryosphere elements
72. Coincident aboveground and belowground autonomous monitoring to quantify covariability in permafrost, soil, and vegetation properties in Arctic tundra
73. Competitor and substrate sizes and diffusion together define enzymatic depolymerization and microbial substrate uptake rates
74. Conceptualizing Biogeochemical Reactions With an Ohm's Law Analogy
75. Consequences of changes in vegetation and snow cover for climate feedbacks in Alaska and northwest Canada
76. Consequences of permafrost degradation for Arctic infrastructure – bridging the model gap between regional and engineering scales
77. Constitutive model for unfrozen water content in subfreezing unsaturated soils
78. Continuously amplified warming in the Alaskan Arctic: Implications for estimating global warming hiatus
79. Controls on fine-scale spatial and temporal variability of plant-available inorganic nitrogen in a polygonal tundra landscape
80. Convolutional Neural Network Approach for Mapping Arctic Vegetation Using Multi-Sensor Remote Sensing Fusion
81. Convolutional neural network approach for mapping Arctic vegetation using multi-sensor remote sensing fusion
82. Coupled land surface-subsurface hydrogeophysical inverse modeling to estimate soil organic content and explore associated hydrological and thermal dynamics in an Arctic tundra
83. Coupling surface flow and subsurface flow in complex soil structures using mimetic finite differences
84. Co‐producing knowledge: the Integrated Ecosystem Model for resource management in Arctic Alaska
85. Deep Yedoma permafrost: A synthesis of depositional characteristics and carbon vulnerability
86. Dependence of the evolution of carbon dynamics in the northern permafrost region on the trajectory of climate change
87. Depth-resolved physicochemical characteristics of active layer and permafrost soils in an Arctic polygonal tundra region
88. Detecting regional patterns of changing CO <sub>2</sub> flux in Alaska
89. Detecting the permafrost carbon feedback: Talik formation and increased cold-seasonrespiration as precursors to sink-to-source transitions
90. Determination of ground subsidence around snow fences in the Arctic region
91. Disentangling the complexity of permafrost soil by using high resolution profiling of microbial community composition, key functions and respiration rates
92. Dispersal and fire limit Arctic shrub expansion
93. Does fire always accelerate shrub expansion in Arctic tundra? Examining a novel grass-dominated successional trajectory on the Seward Peninsula
94. Drainage network response to Arctic warming
95. Drainage subsidence associated with Arctic permafrost degradation
96. Drying of tundra landscapes will limit subsidence-induced acceleration of permafrost thaw
97. Dynamic soil columns simulate Arctic redox biogeochemistry and carbon release during changes in water saturation
98. Effect of soil property uncertainties on permafrost thaw projections: a calibration-constrained analysis
99. Effects of warming on the degradation and production of low-molecular-weight labile organic carbon in an Arctic tundra soil
100. Electrical and seismic response of saline permafrost soil during freeze - Thaw transition
101. Electrical conductivity imaging of active layer and permafrost in an arctic ecosystem, through advanced inversion of electromagnetic induction data
102. Enabling FAIR data in Earth and environmental science with community-centric (meta)data reporting formats
103. Enhancing global change experiments through integration of remote‐sensing techniques
104. Enhancing terrestrial ecosystem sciences by integrating empirical modeling approaches
105. Environmental controls on observed spatial variability of soil pore water geochemistry in small headwater catchments underlain with permafrost
106. Estimating Permafrost Distribution Using Co-Located Temperature and Electrical Resistivity Measurements
107. Estimating snow cover from high-resolution satellite imagery by thresholding blue wavelengths
108. Estimation of subsurface porosities and thermal conductivities of polygonal tundra by coupled inversion of electrical resistivity, temperature, and moisture content data
109. Evaluating integrated surface/subsurface permafrost thermal hydrology models in ATS (v0.88) against observations from a polygonal tundra site
110. Evaluating temporal controls on greenhouse gas (GHG) fluxes in an Arctic tundra environment: An entropy-based approach
111. Evaluating the impact of peat soils and snow schemes on simulated active layer thickness at pan-Arctic permafrost sites
112. Evaluation of an untargeted nano-liquid chromatography-mass spectrometry approach to expand coverage of low molecular weight dissolved organic matter in Arctic soil
113. Evaporation dominates evapotranspiration on Alaska’s Arctic Coastal Plain
114. Evapotranspiration across plant types and geomorphological units in polygonal Arctic tundra
115. Expansion of high-latitude deciduous forests driven by interactions between climate warming and fire
116. Exploring the Role of Cryptic Nitrogen Fixers in Terrestrial Ecosystems: A Frontier in Nitrogen Cycling Research
117. Extrapolating active layer thickness measurements across Arctic polygonal terrain using LiDAR and NDVI data sets
118. Factors Controlling a Synthetic Aperture Radar (SAR) Derived Root-Zone Soil Moisture Product over The Seward Peninsula of Alaska
119. Feedbacks Between Surface Deformation and Permafrost Degradation in Ice Wedge Polygons, Arctic Coastal Plain, Alaska
120. FLUXNET-Methane Synthesis Activity: Objectives, Observations, and Future Directions
121. From documentation to prediction: How remote sensing and mechanistic modeling are raising the bar for thermokarst research.
122. From the Arctic to the tropics: Multibiome prediction of leaf mass per area using leaf reflectance
123. Full-wavefield inversion of surface waves for mapping embedded low-velocity zones in permafrost
124. Future increases in Arctic lightning and fire risk for permafrost carbon
125. Genomic insights into redox-driven microbial processes for carbon decomposition in thawing arctic soils and permafrost
126. Genomics in a changing arctic: critical questions await the molecular ecologist
127. Geochemical drivers of organic matter decomposition in arctic tundra soils
128. Geomorphological and geochemistry changes in permafrost after the 2002 tundra wildfire in Kougarok, Seward Peninsula, Alaska
129. Geophysical estimation of shallow permafrost distribution and properties in an ice-wedge polygon-dominated Arctic tundra region
130. Geophysical Monitoring Shows that Spatial Heterogeneity in Thermohydrological Dynamics Reshapes a Transitional Permafrost System
131. Global pattern and controls of soil microbial metabolic quotient
132. Global photosynthetic capacity is optimized to the environment
133. Global-scale environmental control of plant photosynthetic capacity
134. Groundwater flow and heat transport for systems undergoing freeze-thaw: Intercomparison of numerical simulators for 2D test cases
135. High temporal and spatial variability of nitrate on an Alaskan hillslope dominated by alder shrubs
136. High-resolution mapping of spatial heterogeneity in ice wedge polygon geomorphology near Prudhoe Bay, Alaska
137. High-Resolution Maps of Near-Surface Permafrost for Three Watersheds on the Seward Peninsula, Alaska Derived From Machine Learning
138. High-Resolution Spatio-Temporal Estimation of Net Ecosystem Exchange in Ice-Wedge Polygon Tundra Using In Situ Sensors and Remote Sensing Data
139. Hillslope-channel transitions and the role of water tracks in a changing permafrost landscape
140. How deep should we go to understand roots at the top of the world?
141. How does humidity data impact the land surface modeling of hydrothermal regimes at a permafrost site in Utqiaġvik, Alaska?
142. Hybrid-energy module for remote environmental observations, instruments, and communications
143. Hysteretic temperature sensitivity of wetland methane fluxes explained by substrate availability and microbial activity
144. ICESat GLAS elevation changes and ALOS PALSAR InSAR line-of-sight changes on the continuous permafrost zone of the North Slope, Alaska
145. Identifying multiscale zonation and assessing the relative importance of polygon geomorphology on carbon fluxes in an Arctic tundra ecosystem
146. 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
147. Impacts of temperature and soil characteristics on methane production and oxidation in Arctic polygonal tundra
148. Importance of feedback loops between soil inorganic nitrogen and microbial communities in the heterotrophic soil respiration response to global warming
149. Improved global-scale predictions of soil carbon stocks with Millennial Version 2
150. Improving representation of photosynthesis in Earth System Models
151. Increased Arctic NO3− Availability as a Hydrogeomorphic Consequence of Permafrost Degradation and Landscape Drying
152. Indexing permafrost soil organic matter degradation using high-resolution mass spectrometry
153. Influence of iron redox cycling on organo-mineral associations in Arctic tundra soil
154. Influence of tundra polygon type and climate variability on carbon dioxide and methane fluxes near Utqiagvik, Alaska
155. Influences and interactions of inundation, peat, and snow on active layer thickness
156. Influences of Hillslope Biogeochemistry on Anaerobic Soil Organic Matter Decomposition in a Tundra Watershed
157. Inhibition of Methylmercury and Methane Formation by Nitrous Oxide in Arctic Tundra Soil Microcosms
158. InSAR detection and field evidence for thermokarst after a tundra wildfire, using ALOS-PALSAR
159. Insights on seasonal solifluction processes in warm permafrost Arctic landscape using a dense monitoring approach across adjacent hillslopes
160. Integrated surface/subsurface permafrost thermal hydrology: Model formulation and proof-of-concept simulations
161. Integrating Arctic Plant Functional Types in a Land Surface Model Using Above‐ and Belowground Field Observations
162. Integrating empirical-modeling approaches to improve understanding of terrestrial ecology processes
163. Integrating State Data Assimilation and Innovative Model Parameterization Reduces Simulated Carbon Uptake in the Arctic and Boreal Region
164. Integrating very-high-resolution UAS data and airborne imaging spectroscopy to map the fractional composition of Arctic plant functional types in Western Alaska
165. Ion concentrations in ice wedges: An innovative approach to reconstruct past climate variability
166. Iron (oxyhydr)oxides serve as phosphate traps in tundra and boreal peat soils
167. Iron and iron-bound phosphate accumulate in surface soils of ice-wedge polygons in arctic tundra
168. Isotopic identification of soil and permafrost nitrate sources in an Arctic tundra ecosystem
169. Isotopic insights into methane production, oxidation, and emissions in Arctic polygon tundra
170. Land cover classification in multispectral imagery using clustering of sparse approximations over learned feature dictionaries
171. Land Use and Land Cover Affect the Depth Distribution of Soil Carbon: Insights From a Large Database of Soil Profiles
172. Landscape topography structures the soil microbiome in Arctic polygonal tundra
173. Landscape-scale characterization of Arctic tundra vegetation composition, structure, and function with a multi-sensor unoccupied aerial system
174. Large carbon dioxide and methane emissions from polygonal tundra during spring thaw in northern Alaska
175. Large Divergence of Projected High Latitude Vegetation Composition and Productivity Due To Functional Trait Uncertainty
176. Large emissions of CO2 and CH4 due to active-layer warming in Arctic tundra
177. Large loss of carbon dioxide in winter observed across the northern permafrost region
178. Large uncertainty in permafrost carbon stocks due to hillslope soil deposits
179. Large-Eddy simulations of air flow and turbulence within and around low-aspect-ratio cylindrical open-top chambers
180. Leaf respiration (GlobResp) - global trait database supports Earth System Models
181. Local-scale Arctic tundra heterogeneity affects regional-scale carbon dynamics
182. Local-scale heterogeneity of soil thermal dynamics and controlling factors in a discontinuous permafrost region
183. 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
184. Low-Power, Flexible Sensor Arrays with Solderless Board-to-Board Connectors for Monitoring Soil Deformation and Temperature
185. Machine learning models inaccurately predict current and future high-latitude C balances
186. Managing complexity in simulations of land surface and near-surface processes
187. Mapping Arctic plant functional type distributions in the Barrow Environmental Observatory using WorldView-2 and LiDAR datasets
188. Mapping canopy traits over Québec using airborne and spaceborne imaging spectroscopy
189. Mapping snow depth within a tundra ecosystem using multiscale observations and Bayesian methods
190. Mathematical modeling of Arctic polygonal tundra with Ecosys: 1. Microtopography determines how active layer depths respond to changes in temperature and precipitation
191. Mathematical modeling of Arctic polygonal tundra with Ecosys: 2. Microtopography determines how carbon dioxide and methane exchange responds to changes in temperature and precipitation
192. Measuring diurnal cycles of evapotranspiration in the Arctic with an automated chamber system
193. Mechanistic modeling of microtopographic impacts on carbon dioxide and methane fluxes in an Alaskan tundra ecosystem using the CLM‐Microbe model
194. Meta-analysis of high-latitude nitrogen-addition and warming studies implies ecological mechanisms overlooked by land models
195. Metagenomes from Arctic Soil Microbial Communities from the Barrow Environmental Observatory, Utqiaġvik, AK, USA
196. Microbes in thawing permafrost: the unknown variable in the climate change equation
197. Microbial community and functional gene changes in Arctic tundra soils in a microcosm warming experiment
198. Microbial contribution to post-fire tundra ecosystem recovery over the 21st century
199. Microtopographic and depth controls on active layer chemistry in Arctic polygonal ground
200. Microtopographic control on the ground thermal regime in ice wedge polygons
201. Mineral properties, microbes, transport, and plant-input profiles control vertical distribution and age of soil carbon stocks
202. Missing pieces to modeling the Arctic-Boreal puzzle
203. Modeling anaerobic soil organic carbon decomposition in Arctic polygon tundra: Insights into soil geochemical influences on carbon mineralization
204. Modeling challenges for predicting hydrologic response to degrading permafrost
205. Modeling climate change impacts on an Arctic Polygonal Tundra: 1. Rates of permafrost thaw depend on changes in vegetation and drainage
206. Modeling climate change impacts on an Arctic Polygonal Tundra: 2. Changes in carbon dioxide and methane exchange depend on rates of permafrost thaw as affected by changes in vegetation and drainage
207. Modeling long-term permafrost degradation
208. Modeling Present and Future Permafrost Distribution at the Seward Peninsula, Alaska
209. Modeling the role of preferential snow accumulation in through talik development and hillslope groundwater flow in a transitional permafrost landscape
210. Modeling the spatiotemporal variability in subsurface thermal regimes across a low-relief polygonal tundra landscape
211. Modelling impacts of recent warming on seasonal carbon exchange in higher latitudes of North America
212. Molecular insights into Arctic soil organic matter degradation under warming
213. NASA's surface biology and geology designated observable: A perspective on surface imaging algorithms
214. Near activation and differential activation in enzymatic reactions
215. Near‐Surface Hydrology and Soil Properties Drive Heterogeneity in Permafrost Distribution, Vegetation Dynamics, and Carbon Cycling in a Sub‐Arctic Watershed
216. New calculations for photosynthesis measurement systems: what's the impact for physiologists and modelers?
217. New insights into the drainage of inundated ice-wedge polygons using fundamental hydrologic principles
218. Next generation Arctic vegetation maps: Aboveground plant biomass and woody dominance mapped at 30 m resolution across the tundra biome
219. Nitrogen fixing shrubs advance the pace of tall-shrub expansion in low-Arctic tundra
220. No evidence for triose phosphate limitation of light‐saturated leaf photosynthesis under current atmospheric carbon dioxide concentration
221. Non-growing season plant nutrient uptake controls Arctic tundra vegetation composition under future climate
222. Non-isothermal, three-phase simulations of near-surface flows in a model permafrost system under seasonal variability and climate change
223. Nonlinear carbon dioxide flux response to 7 years of experimentally induced permafrost thaw
224. Numerical modeling of two-dimensional temperature field dynamics across non-deforming ice-wedge polygons
225. Observational constraints reduce model spread but not uncertainty in global wetland methane emission estimates
226. On the relationships between the Michaelis–Menten kinetics, reverse Michaelis–Menten kinetics, equilibrium chemistry approximation kinetics, and quadratic kinetics
227. Open Science principles for accelerating trait-based science across the Tree of Life
228. Optimal stomatal behaviour around the world
229. Pan-Arctic ice-wedge degradation in warming permafrost and its influence on tundra hydrology
230. Pathways and transformations of dissolved methane and dissolved inorganic carbon in Arctic tundra watersheds: Evidence from analysis of stable isotopes
231. Pathways of anaerobic organic matter decomposition in tundra soils from Barrow, Alaska
232. Patterns and rates of soil movement and shallow failures across several small watersheds on the Seward Peninsula, Alaska
233. PeRL: A Circum-Arctic permafrost region pond and lake database
234. PeRL: a circum-Arctic permafrost region pond and lake database
235. Permafrost carbon-climate feedbacks accelerate global warming
236. Permafrost carbon−climate feedback is sensitive to deep soil carbon decomposability but not deep soil nitrogen dynamics
237. Permafrost degradation and subsurface-flow changes caused by surface warming trends
238. Permafrost Meta-Omics and climate change
239. Permafrost Promotes Shallow Groundwater Flow and Warmer Headwater Streams
240. Permafrost thaw and resulting soil moisture changes regulate projected high-latitude carbon dioxide and methane emissions
241. Permafrost thermal conditions are sensitive to shifts in snow timing
242. Persistence of soil organic carbon caused by functional complexity
243. PiCAM: a Raspberry Pi-based open-source, low-power camera system for monitoring plant phenology in arctic environments
244. Planning the Next Generation of Arctic Ecosystem Experiments
245. Plant functional trait change across a warming tundra biome
246. Plant functional types in Earth system models: past experiences and future directions for application of dynamic vegetation models in high-latitude ecosystems
247. Polygonal tundra geomorphological change in response to warming alters future carbon dioxide and methane flux on the Barrow Peninsula
248. Polygonal tundra geomorphological change in response to warming alters future CO2 and CH4 flux on the Barrow Peninsula
249. Potential carbon emissions dominated by carbon dioxide from thawed permafrost soils
250. Potential impacts of mercury released from thawing permafrost
251. Preface: Hydrogeology of cold regions
252. Probabilistic estimation of depth-resolved profiles of soil thermal diffusivity from temperature time series
253. Profile: Stan D. Wullschleger
254. Quantification of Arctic soil and permafrost properties using ground penetrating radar
255. Quantification of Arctic soil and permafrost properties using ground-penetrating radar and electrical resistivity tomography datasets
256. Quantifying and relating land-surface and subsurface variability in permafrost environments using LiDAR and surface geophysical datasets
257. Quantifying pH buffering capacity in acidic, organic-rich Arctic soils: Measurable proxies and implications for soil carbon degradation
258. Radiocarbon evidence that millennial and fast-cycling soil carbon are equally sensitive to warming
259. Radiocarbon measurements of ecosystem respiration and soil pore-space carbon dioxide in Utqiaġvik (Barrow), Alaska
260. Range shifts in a foundation sedge potentially induce large Arctic ecosystem carbon losses and gains
261. Rapidly changing high-latitude seasonality: implications for the 21st century carbon cycle in Alaska
262. Reduced arctic tundra productivity linked with landform and climate change interactions
263. Reducing model uncertainty of climate change impacts on high latitude carbon assimilation
264. Reducing uncertainty of high-latitude ecosystem models through identification of key parameters
265. Remote monitoring of freeze–thaw transitions in Arctic soils using the complex resistivity method
266. Remote sensing from unoccupied aerial systems: Opportunities to enhance Arctic plant ecology in a changing climate
267. Remote Sensing of Tundra Ecosystems Using High Spectral Resolution Reflectance: Opportunities and Challenges
268. Representativeness assessment of the pan-Arctic eddy covariance site network and optimized future enhancements
269. Representativeness-based sampling network design for the State of Alaska
270. Representing leaf and root physiological traits in CLM improves global carbon and nitrogen cycling predictions
271. Responses of Boreal Forest Ecosystems and Permafrost to Climate Change and Disturbances: A Modeling Perspective
272. Reviews and syntheses: Four decades of modeling methane cycling in terrestrial ecosystems
273. Revising the dynamic energy budget theory with a new reserve mobilization rule and three example applications to bacterial growth
274. Rising plant-mediated methane emissions from Arctic wetlands
275. Root structural and functional dynamics in terrestrial biosphere models - evaluation and recommendations
276. Root traits explain observed tundra vegetation nitrogen uptake patterns: Implications for trait-based land models
277. Root traits explain observed tundra vegetation nitrogen uptake patterns: Implications for trait‐based land models
278. Saturated nitrous oxide emission rates occur above the nitrogen deposition level predicted for the semi-arid grasslands of Inner Mongolia, China
279. Scaling Arctic landscape and permafrost features improves active layer depth modeling
280. Scaling-up permafrost thermal measurements in western Alaska using an ecotype approach
281. Second-order accurate finite volume schemes with the discrete maximum principle for solving Richards’ equation on unstructured meshes
282. Sensitivity evaluation of the Kudryavtsev permafrost model
283. Shallow soils are warmer under trees and tall shrubs across Arctic and Boreal ecosystems
284. Shrubs Strongly Influence Snow Properties in Two Subarctic Watersheds
285. Simulated Hydrological Dynamics and Coupled Iron Redox Cycling Impact Methane Production in an Arctic Soil
286. Size distributions of Arctic waterbodies reveal consistent relations in their statistical moments in space and time
287. Snow distribution patterns revisited: A physics-based and machine learning hybrid approach to snow distribution mapping in the sub-Arctic
288. Soil moisture and hydrology projections of the permafrost region – a model intercomparison
289. Soil respiration strongly offsets carbon uptake in Alaska and Northwest Canada
290. Spatial and temporal variations of thaw layer thickness and its controlling factors identified using time-lapse electrical resistivity tomography and hydro-thermal modeling
291. Spatial distribution of thermokarst terrain in Arctic Alaska
292. Spatial patterns of snow distribution for improved Earth system modelling in the Arctic
293. Sphagnum physiology in the context of changing climate: emergent influences of genomics, modelling and host-microbiome interactions on understanding ecosystem function
294. Statistical upscaling of ecosystem carbon dioxide fluxes across the terrestrial tundra and boreal domain: Regional patterns and uncertainties
295. Stoichiometry and temperature sensitivity of methanogenesis and CO<sub>2</sub> production from saturated polygonal tundra in Barrow, Alaska
296. Sub-aerial talik formation observed across the discontinuous permafrost zone of Alaska
297. Substantial and overlooked greenhouse gas emissions from deep Arctic lake sediment
298. SUPECA kinetics for scaling redox reactions in networks of mixed substrates and consumers and an example application to aerobic soil respiration
299. TDD LoRa and Delta Encoding in Low-Power Networks of Environmental Sensor Arrays for Temperature and Deformation Monitoring
300. Technical Note: A generic law-of-the-minimum flux limiter for simulating substrate limitation in biogeochemical models
301. Technical Note: Simple formulations and solutions of the dual-phase diffusive transport for biogeochemical modeling
302. Temperature sensitivity of mineral-enzyme interactions on the hydrolysis of cellobiose and indican by beta-glucosidase
303. Temporal, Spatial, and Temperature Controls on Organic Carbon Mineralization and Methanogenesis in Arctic High-Centered Polygon SoilsData_Sheet_1.docx
304. Terrestrial biosphere models may overestimate Arctic carbon dioxide assimilation if they do not account for decreased quantum yield and convexity at low temperature
305. Terrestrial biosphere models underestimate photosynthetic capacity and carbon dioxide assimilation in the Arctic
306. The ABCflux database: Arctic–boreal CO2 flux observations and ancillary information aggregated to monthly time steps across terrestrial ecosystems
307. The Alaska Arctic vegetation archive (AVA-AK)
308. The Arctic
309. The arctic plant aboveground biomass synthesis dataset
310. The eco-evolutionary role of fire in shaping terrestrial ecosystems
311. The effect of temperature on the rate, affinity, and 15N fractionation of NO3 − during biological denitrification in soils
312. The fungal collaboration gradient dominates the root economics space in plants
313. The impacts of recent permafrost thaw on land–atmosphere greenhouse gas exchange
314. The importance of freeze–thaw cycles for lateral tracer transport in ice-wedge polygons
315. The integrated hydrologic model intercomparison project, IH-MIP2: A second set of benchmark results to diagnose integrated hydrology and feedbacks
316. The microbial ecology of permafrost
317. The Next-Generation Ecosystem Experiment Arctic Rainfall Simulator: a tool to understand the effects of changing rainfall patterns in the Arctic
318. The role of advective heat transport in talik development beneath lakes and ponds in discontinuous permafrost
319. The State of the Climate in 2019: The Arctic
320. The unseen iceberg: plant roots in arctic tundra
321. The use and misuse of Vc,max in Earth System Models
322. The “one‐point method” for estimating maximum carboxylation capacity of photosynthesis: A cautionary tale
323. Thermal effects of groundwater flow through subarctic fens: A case study based on field observations and numerical modeling
324. Three-phase numerical model for subsurface hydrology in permafrost-affected regions (PFLOTRAN-ICE v1.0)
325. Timing and duration of hydrological transitions in Arctic polygonal ground from stable isotopes
326. Timing and duration of hydrological transitions in Arctic polygonal ground from stable isotopes
327. Topographical Controls on Hillslope‐Scale Hydrology Drive Shrub Distributions on the Seward Peninsula, Alaska
328. Topography controls variability in circumpolar permafrost thaw pond expansion
329. Toward a mechanistic modeling of nitrogen limitation on vegetation dynamics
330. Traditional plant functional groups explain variation in economic but not size‐related traits across the tundra biome
331. Trait covariance: the functional warp of plant diversity?
332. Trait-Based representation of biological nitrification: Model development, testing, and predicted community composition
333. Trajectory of the Arctic as an integrated system
334. Triose phosphate limitation in photosynthesis models reduces leaf photosynthesis and global terrestrial carbon storage
335. Triose phosphate utilization limitation: an unnecessary complexity in terrestrial biosphere model representation of photosynthesis
336. TRY plant trait database – Enhanced coverage and open access
337. Tundra Greenness
338. Tundra landform and vegetation productivity trend maps for the Arctic Coastal Plain of northern Alaska
339. Tundra vegetation community, not microclimate, controls asynchrony of above and belowground phenology
340. Tundra water budget and implications of precipitation underestimation
341. Twenty-first century tundra shrubification could enhance net carbon uptake of North America Arctic tundra under an RCP_8.5 climate trajectory
342. UAS LIDAR MAPPING OF AN ARCTIC TUNDRA WATERSHED: CHALLENGES AND OPPORTUNITIES
343. Understanding spatial variability of methane fluxes in Arctic wetlands through footprint modelling
344. Understanding the relative importance of vertical and horizontal flow in ice-wedge polygons
345. Unravelling biogeochemical drivers of methylmercury production in an Arctic fen soil and a bog soil
346. Untargeted Exometabolomics Provides a Powerful Approach to Investigate Biogeochemical Hotspots with Vegetation and Polygon Type in Arctic Tundra Soils
347. Use of a metadata documentation and search tool for large data volumes: The NGEE arctic example
348. Using field observations to inform thermal hydrology models of permafrost dynamics with ATS (v0.83)
349. Using model reduction to predict the soil-surface C<sup>18</sup> carbon dioxide flux: an example of representing complex biogeochemical dynamics in a computationally efficient manner
350. Using MODIS estimates of fractional snow cover area to improve streamflow forecasts in interior Alaska
351. Variability in the sensitivity among model simulations of permafrost and carbon dynamics in the permafrost region between 1960 and 2009
352. Variations of soil microbial community structures beneath broadleaved forest trees in temperate and subtropical climate zones
353. Warming increases methylmercury production in an Arctic soil
354. Water balance response of permafrost-affected watersheds to changes in air temperatures
355. We Must Stop Fossil Fuel Emissions to Protect Permafrost Ecosystems
356. Weaker soil carbon–climate feedbacks resulting from microbial and abiotic interactions
357. WETCHIMP-WSL: Intercomparison of wetland methane emissions models over West Siberia
358. Wildfire exacerbates high-latitude soil carbon losses from climate warming
359. Wildfire Mapping in Interior Alaska Using Deep Neural Networks on Imbalanced Datasets
