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Simulating the effects of soil organic nitrogen and grazing on arctic tundra vegetation dynamics on the Yamal Peninsula, Russia

Datos Bibliográficos

ID15547499
AutoresQin Yu (0000-0002-4342-9398, University of Virginia, autor de correspondencia), Howard E Epstein (0000-0003-2817-4486, University of Virginia), Howard Epstein, Donald A Walker (0000-0001-9581-7811, University of Alaska Fairbanks), Donald Walker
Año2009
Volumen4
Número4
Páginas045027-045027
Fecha de publicación2009-10-01
Open AccessSí
TipoARTICLE
RevistaEnvironmental Research Letters (JOURNAL)
Identificadores de la revistaISSN: 1748-9326 • E-ISSN: 1748-9326
EditorialIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/4/4/045027
OpenAlexW2113117963
IdiomaEN
Citas recibidas3
Referencias citadas55

Sustainability of tundra vegetation under changing climate on the Yamal Peninsula, northwestern Siberia, home to the world’s largest area of reindeer husbandry, is of crucial importance to the local native community. An integrated investigation is needed for better understanding of the effects of soils, climate change and grazing on tundra vegetation in the Yamal region. In this study we applied a nutrient-based plant community model—ArcVeg—to evaluate how two factors (soil organic nitrogen (SON) levels and grazing) interact to affect tundra responses to climate warming across a latitudinal climatic gradient on the Yamal Peninsula. Model simulations were driven by field-collected soil data and expected grazing patterns along the Yamal Arctic Transect (YAT), within bioclimate subzones C (high arctic), D (northern low arctic) and E (southern low arctic). Plant biomass and NPP (net primary productivity) were significantly increased with warmer bioclimate subzones, greater soil nutrient levels and temporal climate warming, while they declined with higher grazing frequency. Temporal climate warming of 2 ◦ C caused an increase of 665 g m −2 in total biomass at the high SON site in subzone E, but only 298 g m −2 at the low SON site. When grazing frequency was also increased, total biomass increased by only 369 g m −2 at the high SON site in contrast to 184 g m −2 at the low SON site in subzone E. Our results suggest that high SON can support greater plant biomass and plant responses to climate warming, while low SON and grazing may limit plant response to climate change. In addition to the first order factors (SON, bioclimate subzones, grazing and temporal climate warming), interactions among these significantly affect plant biomass and productivity in the arctic tundra and should not be ignored in regional scale studies

Arctic · Arctic vegetation · Biology · Geography · Grazing · Nitrogen · Peninsula · Physical geography · Tundra · Vegetation (pathology · Chemistry · Climate change and permafrost · Cryospheric studies and observations · Environmental Science · Geology and Paleoclimatology Research · Ecology

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Citas por año0,2
Intervalo de citas2011 - 2018 (8)
Altamente citadoNo
Abrir DOISci-HubOpen Access
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