| human | Q5 |
| P496 | ORCID iD | 0000-0002-8096-1594 |
| P3829 | Publons author ID | 2798365 |
| P1053 | ResearcherID | C-9759-2011 |
| P735 | given name | Gustaf | Q15646212 |
| Gustaf | Q15646212 | ||
| P106 | occupation | researcher | Q1650915 |
| P21 | sex or gender | male | Q6581097 |
| Q57263669 | A new data set for estimating organic carbon storage to 3 m depth in soils of the northern circumpolar permafrost region |
| Q101165850 | A spatial emergent constraint on the sensitivity of soil carbon turnover to global warming |
| Q115742089 | Aboveground biomass patterns across treeless northern landscapes |
| Q57202059 | Amino acid production exceeds plant nitrogen demand in Siberian tundra |
| Q57059418 | Amorphous silica pools in permafrost soils of the Central Canadian Arctic and the potential impact of climate change |
| Q58403141 | An observation-based constraint on permafrost loss as a function of global warming |
| Q64069881 | Approaching the potential of model-data comparisons of global land carbon storage |
| Q57202717 | Biomass offsets little or none of permafrost carbon release from soils, streams, and wildfire: an expert assessment |
| Q57890540 | Can C-band synthetic aperture radar be used to estimate soil organic carbon storage in tundra? |
| Q117611335 | Carbon loss from northern circumpolar permafrost soils amplified by rhizosphere priming |
| Q89109872 | Carbon release through abrupt permafrost thaw |
| Q57196272 | Carbon stocks and fluxes in the high latitudes: using site-level data to evaluate Earth system models |
| Q58317999 | Characterisation of the Permafrost Carbon Pool |
| Q31135981 | Circumpolar distribution and carbon storage of thermokarst landscapes |
| Q57202078 | Controls on the storage of organic carbon in permafrost soil in northern Siberia |
| Q57027793 | Decadal soil carbon accumulation across Tibetan permafrost regions |
| Q58388770 | Deep Yedoma permafrost: A synthesis of depositional characteristics and carbon vulnerability |
| Q106622065 | Definitions and methods to estimate regional land carbon fluxes for the second phase of the REgional Carbon Cycle Assessment and Processes Project (RECCAP-2) |
| Q112764450 | Definitions and methods to estimate regional land carbon fluxes for the second phase of the REgional Carbon Cycle Assessment and Processes Project (RECCAP-2) |
| Q57879487 | Distinguishing between old and modern permafrost sources in the northeast Siberian land–shelf system with compound-specific δ2H analysis |
| Q57914964 | Effects of permafrost aggradation on peat properties as determined from a pan-Arctic synthesis of plant macrofossils |
| Q58318002 | Empirical estimates to reduce modeling uncertainties of soil organic carbon in permafrost regions: a review of recent progress and remaining challenges |
| Q57263661 | Estimated stocks of circumpolar permafrost carbon with quantified uncertainty ranges and identified data gaps |
| Q57059388 | Estimated storage of amorphous silica in soils of the circum-Arctic tundra region |
| Q64451023 | Evaluation of terrestrial pan-Arctic carbon cycling using a data-assimilation system |
| Q64459498 | Evaluation of terrestrial pan-Arctic carbon cycling using a data-assimilation system |
| Q58078600 | Expert assessment of vulnerability of permafrost carbon to climate change |
| Q120345781 | Extensive global wetland loss over the past three centuries |
| Q59095940 | Extensive loss of past permafrost carbon but a net accumulation into present-day soils |
| Q58318007 | Field information links permafrost carbon to physical vulnerabilities of thawing |
| Q125408546 | Floral resources in Swedish grasslands remain relatively stable under an experimental drought and are enhanced by soil amendments if regularly mown |
| Q58317970 | Higher climatological temperature sensitivity of soil carbon in cold than warm climates |
| Q57889719 | Ideas and perspectives: Holocene thermokarst sediments of the Yedoma permafrost region do not increase the northern peatland carbon pool |
| Q117611398 | Land cover and landform-based upscaling of soil organic carbon stocks on the Brøgger Peninsula, Svalbard |
| Q58683376 | Landscape controls and vertical variability of soil organic carbon storage in permafrost-affected soils of the Lena River Delta |
| Q98302620 | Large stocks of peatland carbon and nitrogen are vulnerable to permafrost thaw |
| Q126066094 | Long‐term soil organic carbon changes after cropland conversion to grazed grassland in Southern Sweden |
| Q57878698 | Low below-ground organic carbon storage in a subarctic Alpine permafrost environment |
| Q117611279 | Mapping the Vulnerability of Arctic Wetlands to Global Warming |
| Q58084222 | Mapping the degree of decomposition and thaw remobilization potential of soil organic matter in discontinuous permafrost terrain |
| Q109317386 | Modeled Microbial Dynamics Explain the Apparent Temperature Sensitivity of Wetland Methane Emissions |
| Q58084192 | Multi-proxy study of soil organic matter dynamics in permafrost peat deposits reveal vulnerability to climate change in the European Russian Arctic |
| Q42695027 | Networking our science to characterize the state, vulnerabilities, and management opportunities of soil organic matter |
| Q117611252 | No support for carbon storage of >1,000 GtC in northern peatlands |
| Q117611220 | Only halving emissions by 2030 can minimize risks of crossing cryosphere thresholds |
| Q104245407 | PeRL: A Circum-Arctic Permafrost Region Pond and Lake Database |
| Q57649282 | PeRL: a circum-Arctic Permafrost Region Pond and Lake database |
| Q114167357 | Permafrost Causes Unique Fine‐Scale Spatial Variability Across Tundra Soils |
| Q55951027 | Permafrost Stores a Globally Significant Amount of Mercury |
| Q28603074 | Plant-derived compounds stimulate the decomposition of organic matter in arctic permafrost soils |
| Q117611309 | Reconstructing Past Global Vegetation With Random Forest Machine Learning, Sacrificing the Dynamic Response for Robust Results |
| Q106533435 | Reduced net methane emissions due to microbial methane oxidation in a warmer Arctic |
| Q57263618 | Short and Long-Term Controls on Active Layer and Permafrost Carbon Turnover Across the Arctic |
| Q57263676 | Short communication: a new dataset for estimating organic carbon storage to 3 m depth in soils of the northern circumpolar permafrost region |
| Q57202066 | Significance of dark CO2 fixation in arctic soils |
| Q110192814 | Spatial heterogeneity and environmental predictors of permafrost region soil organic carbon stocks |
| Q60493216 | Stable isotopes in Sphagnum fuscum peat as late-Holocene climate proxies in northeastern European Russia |
| Q57250259 | Storage and transformation of organic matter fractions in cryoturbated permafrost soils across the Siberian Arctic |
| Q57250260 | Storage and transformation of organic matter fractions in cryoturbated permafrost soils across the Siberian Arctic |
| Q57202089 | Storage, Landscape Distribution, and Burial History of Soil Organic Matter in Contrasting Areas of Continuous Permafrost |
| Q106622130 | Supplementary material to "The Global Methane Budget 2000–2017" |
| Q117611243 | Temperature effects on carbon storage are controlled by soil stabilisation capacities |
| Q106622086 | The Global Methane Budget 2000–2017 |
| Q106622144 | The Global Methane Budget 2000–2017 |
| Q57017457 | The Northern Circumpolar Soil Carbon Database: spatially distributed datasets of soil coverage and soil carbon storage in the northern permafrost regions |
| Q57202090 | The effect of warming on the vulnerability of subducted organic carbon in arctic soils |
| Q57263642 | Thermokarst dynamics and soil organic matter characteristics controlling initial carbon release from permafrost soils in the Siberian Yedoma region |
| Q58271695 | Tundra landscape heterogeneity, not interannual variability, controls the decadal regional carbon balance in the Western Russian Arctic |
| Q117611233 | Water Availability and Land Management Control Catchment‐Scale Agricultural Nitrogen and Phosphorous Use Efficiencies |
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