57 citations as recorded by crossref.

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5. Carbon Cycling, Climate Regulation, and Disturbances in Canadian Forests: Scientific Principles for Management J. Landry & N. Ramankutty 10.3390/land4010083
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10. Aquatic DOC export from subarctic Atlantic blanket bog in Norway is controlled by seasalt deposition, temperature and precipitation H. de Wit et al. 10.1007/s10533-016-0182-z
11. Prediction of Potential and Actual Evapotranspiration Fluxes Using Six Meteorological Data-Based Approaches for a Range of Climate and Land Cover Types M. Mobilia & A. Longobardi 10.3390/ijgi10030192
12. Holocene regional climate change and formation of southern Ontario's largest swamp inferred from a kettle-lake pollen record E. Byun et al. 10.1017/qua.2021.54
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15. Improved Estimation of the Gross Primary Production of Europe by Considering the Spatial and Temporal Changes in Photosynthetic Capacity from 2001 to 2016 Q. Wu et al. 10.3390/rs15051172
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22. Incorporating Spatial Variations in Parameters for Improvements of an Evapotranspiration Model G. Wu et al. 10.1029/2019JG005504
23. Response of greenhouse gas fluxes to simulated water level management under contrasting climate scenarios in a peatland mesocosm study S. Salimi et al. 10.1016/j.jenvman.2025.127064
24. Long-term effect of fertilization on the greenhouse gas exchange of low-productive peatland forests P. Ojanen et al. 10.1016/j.foreco.2018.10.015
25. Calculating carbon changes in peat soils drained for forestry with four different profile-based methods J. Krüger et al. 10.1016/j.foreco.2016.09.006
26. How does management affect soil C sequestration and greenhouse gas fluxes in boreal and temperate forests? – A review R. Mäkipää et al. 10.1016/j.foreco.2022.120637
27. Comparing chamber and eddy covariance based net ecosystem CO2 exchange of fen soils A. Poyda et al. 10.1002/jpln.201600447
28. Carbon and water balance of an afforested shallow drained peatland in Iceland B. Bjarnadottir et al. 10.1016/j.foreco.2020.118861
29. Field-scale CH4 emission at a subarctic mire with heterogeneous permafrost thaw status P. Łakomiec et al. 10.5194/bg-18-5811-2021
30. Impacts of drainage, restoration and warming on boreal wetland greenhouse gas fluxes A. Laine et al. 10.1016/j.scitotenv.2018.07.390
31. Water table fluctuations control CO2 exchange in wet and dry bogs through different mechanisms J. Ratcliffe et al. 10.1016/j.scitotenv.2018.11.151
32. Ecosystem scale methane fluxes in a natural temperate bog-pine forest in southern Germany J. Hommeltenberg et al. 10.1016/j.agrformet.2014.08.017
33. Effects of microtopography and water table on Sphagnum palustre L. in subtropical high mountains and implications for peatland restoration T. Li et al. 10.1080/03736687.2019.1601446
34. Effects of water level alteration on carbon cycling in peatlands Y. Zhong et al. 10.1080/20964129.2020.1806113
35. Greenhouse gas and energy fluxes in a boreal peatland forest after clear-cutting M. Korkiakoski et al. 10.5194/bg-16-3703-2019
36. Future methane fluxes of peatlands are controlled by management practices and fluctuations in hydrological conditions due to climatic variability V. Tyystjärvi et al. 10.5194/bg-21-5745-2024
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38. Interannual variability in the ecosystem CO2 fluxes at a paludified spruce forest and ombrotrophic bog in the southern taiga V. Mamkin et al. 10.5194/acp-23-2273-2023
39. Implications of structural diversity for seasonal and annual carbon dioxide fluxes in two temperate deciduous forests R. Tamrakar et al. 10.1016/j.agrformet.2018.08.027
40. Surface flux estimates derived from UAS-based mole fraction measurements by means of a nocturnal boundary layer budget approach M. Kunz et al. 10.5194/amt-13-1671-2020
41. Detection and evaluation of anthropogenic impacts on natural forest ecosystems from long-term tree-ring observations M. Bogachev et al. 10.1016/j.foreco.2024.121784
42. Synchronous Growth Releases in Peatland Pine Chronologies as an Indicator for Regional Climate Dynamics—A Multi-Site Study Including Estonia, Belarus and Sweden A. Potapov et al. 10.3390/f10121097
43. Partial cutting of a boreal nutrient-rich peatland forest causes radically less short-term on-site CO2 emissions than clear-cutting M. Korkiakoski et al. 10.1016/j.agrformet.2023.109361
44. Peat loss collocates with a threshold in plant–mycorrhizal associations in drained peatlands encroached by trees C. Defrenne et al. 10.1111/nph.18954
45. Detecting Spatial Patterns of Peatland Greenhouse Gas Sinks and Sources with Geospatial Environmental and Remote Sensing Data P. Christiani et al. 10.1007/s00267-024-01965-7
46. Rewetting Offers Rapid Climate Benefits for Tropical and Agricultural Peatlands But Not for Forestry‐Drained Peatlands P. Ojanen & K. Minkkinen 10.1029/2019GB006503
47. Retrieval of daily gross primary production over Europe and Africa from an ensemble of SEVIRI/MSG products B. Martínez et al. 10.1016/j.jag.2017.10.011
48. Assessing methane emissions for northern peatlands in ORCHIDEE-PEAT revision 7020 E. Salmon et al. 10.5194/gmd-15-2813-2022
49. Deriving Effective Soil Water Retention Characteristics from Shallow Water Table Fluctuations in Peatlands U. Dettmann & M. Bechtold 10.2136/vzj2016.04.0029
50. A new methodology for organic soils in national greenhouse gas inventories: Data synthesis, derivation and application B. Tiemeyer et al. 10.1016/j.ecolind.2019.105838
51. Short-term forecasting of regional biospheric CO2 fluxes in Europe using a light-use-efficiency model (VPRM, MPI-BGC version 1.2) J. Chen et al. 10.5194/gmd-13-4091-2020
52. On the exchange of sensible and latent heat between the atmosphere and melting snow P. Stoy et al. 10.1016/j.agrformet.2018.01.028
53. Organic soils can be CO2 sinks in both drained and undrained hemiboreal peatland forests A. Butlers et al. 10.5194/bg-22-4627-2025
54. A multi-scale comparison of modeled and observed seasonal methane emissions in northern wetlands X. Xu et al. 10.5194/bg-13-5043-2016
55. Tamm Review: Influence of forest management activities on soil organic carbon stocks: A knowledge synthesis M. Mayer et al. 10.1016/j.foreco.2020.118127
56. Sphagnum-dominated bog systems are highly effective yet variable sources of bio-available iron to marine waters R. Krachler et al. 10.1016/j.scitotenv.2016.03.012
57. Ecological and environmental transition across the forested-to-open bog ecotone in a west Siberian peatland J. Ratcliffe et al. 10.1016/j.scitotenv.2017.06.276