Articles | Volume 14, issue 2
https://doi.org/10.5194/hess-14-301-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/hess-14-301-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Forest decline caused by high soil water conditions in a permafrost region
H. Iwasaki
Graduate School of Agriculture, Hokkaido University. North 9, West 9, Kita-ku, Sapporo, 060-8589, Japan
H. Saito
Graduate School of Agriculture, Hokkaido University. North 9, West 9, Kita-ku, Sapporo, 060-8589, Japan
K. Kuwao
Graduate School of Agriculture, Hokkaido University. North 9, West 9, Kita-ku, Sapporo, 060-8589, Japan
T. C. Maximov
Institute for Biological Problems of Cryolithozone, Siberian Division of Russian Academy of Sciences, 41, Lenin ave. Yakutsk, 678891, Russia
S. Hasegawa
Graduate School of Agriculture, Hokkaido University. North 9, West 9, Kita-ku, Sapporo, 060-8589, Japan
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37 citations as recorded by crossref.
- Environmental factors controlling forest evapotranspiration and surface conductance on a multi-temporal scale in growing seasons of a Siberian larch forest M. Yoshida et al. 10.1016/j.jhydrol.2010.10.023
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- Decadal variation in CO<sub>2</sub> fluxes and its budget in a wheat and maize rotation cropland over the North China Plain Q. Zhang et al. 10.5194/bg-17-2245-2020
- Importance of soil moisture and N availability to larch growth and distribution in the Arctic taiga-tundra boundary ecosystem, northeastern Siberia M. Liang et al. 10.1016/j.polar.2014.07.008
- Topography Controls the Abundance of Siberian Larch Forest H. Sato & H. Kobayashi 10.1002/2017JG004096
- Asymmetric responses of EVI and tree ring growth to extreme climate on the northeastern margin of the Tibetan Plateau M. Wei et al. 10.1007/s00484-024-02786-3
- An independent framework-based evapotranspiration model (IFEM) for dual-source: From field to regional scale S. Wang et al. 10.1016/j.rse.2023.113792
- Effects of waterlogging on water and carbon dioxide fluxes and environmental variables in a Siberian larch forest, 1998–2011 T. Ohta et al. 10.1016/j.agrformet.2013.12.012
- Effects of snow manipulation on larch trees in the taiga forest ecosystem in northeastern Siberia R. Shakhmatov et al. 10.1186/s40645-021-00460-5
- The History of Tree and Shrub Taxa on Bol'shoy Lyakhovsky Island (New Siberian Archipelago) since the Last Interglacial Uncovered by Sedimentary Ancient DNA and Pollen Data H. Zimmermann et al. 10.3390/genes8100273
- Evaluation of Daytime Evaporative Fraction from MODIS TOA Radiances Using FLUXNET Observations J. Peng & A. Loew 10.3390/rs6075959
- Changes in Forest Conditions in a Siberian Larch Forest Induced by an Extreme Wet Event A. Nogovitcyn et al. 10.3390/f13081331
- Effect of waterlogging on carbon isotope discrimination during photosynthesis in Larix gmelinii F. Li & A. Sugimoto 10.1080/10256016.2017.1340886
- Spatial variation in vegetation productivity trends, fire disturbance, and soil carbon across arctic-boreal permafrost ecosystems M. Loranty et al. 10.1088/1748-9326/11/9/095008
- Satellite-Derived Spatiotemporal Variations in Evapotranspiration over Northeast China during 1982–2010 L. Zhang et al. 10.3390/rs9111140
- Stochastic representation of spatial variability in thaw depth in permafrost boreal forests T. Nakai et al. 10.1002/ppp.2204
- Response of larch root development to annual changes of water conditions in eastern Siberia C. Takenaka et al. 10.1016/j.polar.2016.04.012
- Strong and stable relationships between tree-ring parameters and forest-level carbon fluxes in a Siberian larch forest S. Tei et al. 10.1016/j.polar.2019.02.001
- Assessment and projection of ground freezing–thawing responses to climate change in the Upper Heihe River Basin, Northwest China J. Hu et al. 10.1016/j.ejrh.2022.101137
- Spatial heterogeneity of greening and browning between and within bioclimatic zones in northern West Siberia V. Miles & I. Esau 10.1088/1748-9326/11/11/115002
- Fine-root growth in a forested bog is seasonally dynamic, but shallowly distributed in nutrient-poor peat C. Iversen et al. 10.1007/s11104-017-3231-z
- Impact of unusually wet permafrost soil on understory vegetation and CO2 exchange in a larch forest in eastern Siberia A. Kotani et al. 10.1016/j.agrformet.2018.11.025
- Water, Energy, and Carbon Dioxide Circulation in Eastern Siberian Larch Forests: GAME, CREST and RIHN Results T. OHTA et al. 10.3178/jjshwr.29.294
- Too wet for oaks? Inter-tree competition and recent persistent wetness predispose oaks to rainfall-induced dieback in Atlantic rainy forest V. Rozas & I. García-González 10.1016/j.gloplacha.2012.07.004
- Greening vs browning? Surface water cover mediates how tundra and boreal ecosystems respond to climate warming J. Li et al. 10.1088/1748-9326/ac2376
- Growth and physiological responses of larch trees to climate changes deduced from tree-ring widths and δ13C at two forest sites in eastern Siberia S. Tei et al. 10.1016/j.polar.2013.12.002
- Contribution of transpiration to the atmospheric moisture in eastern Siberia estimated with isotopic composition of water vapour A. Ueta et al. 10.1002/eco.1403
- Arctic Plant Responses to Summer Climates and Flooding Events: A Study of Carbon and Nitrogen‐Related Larch Growth and Ecosystem Parameters in Northeastern Siberia M. Liang et al. 10.1029/2022JG007135
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- Sap flow changes in relation to permafrost degradation under increasing precipitation in an eastern Siberian larch forest Y. Iijima et al. 10.1002/eco.1366
- Reconstruction of summer Palmer Drought Severity Index from δ13C of larch tree rings in East Siberia S. Tei et al. 10.1016/j.quaint.2012.06.040
- Temporal variations in the linkage between the net ecosystem exchange of water vapour and CO2over boreal forests in eastern Siberia A. Kotani et al. 10.1002/eco.1449
- Effects of Two-Year Variation in Soil Moisture Condition on the Development of Larch Root System in Eastern Siberia C. Takenaka et al. 10.4236/ajcc.2016.52015
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