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Articles by Dan Kou
Progressive decline in soil nitrogen stocks with warming in a Tibetan permafrost ecosystem - Nature Geoscience
Abstract Permafrost regions contain a substantial fraction of Earth’s soil nitrogen, which is vulnerable to climate change. The response of this crucial N stock to warming could impact the permafrost–climate feedback by altering plant productivity, microbial decomposition and nitrous oxide emissions. However, the long-term trajectory of soil N stocks in response to warming remains unclear.
Spatiotemporal patterns of methane fluxes across alpine permafrost region on the Tibetan Plateau - Nature Communications
Abstract Methane (CH4) emissions from thawing permafrost could amplify climate warming. However, long-term trajectory of net CH4 balance in permafrost regions, particularly high-altitude permafrost regions, remains unknown. Based on literature synthesis and CLM5.0 model, we evaluate the contemporary and future CH4 fluxes across the Tibetan alpine permafrost region from 1989−2100.
Individual risk attitudes and expectations to support online hotel decisions: a UGC-driven intelligent decision-making approach
Advanced search Asia Pacific Journal of Tourism Research Latest Articles Submit an article Journal homepage Full Article Figures & data References Citations Metrics Reprints & Permissions Read this article /doi/full/10.1080/10941665.2025.2474017?needAccess=true ABSTRACT This paper proposes an adjustable intelligent decision-making method for online hotel booking platforms, aiming to reveal the differences in hotel selection results for different types of travelers.
Arctic soil methane sink increases with drier conditions and higher ecosystem respiration - Nature Climate Change
Abstract Arctic wetlands are known methane (CH4) emitters but recent studies suggest that the Arctic CH4 sink strength may be underestimated. Here we explore the capacity of well-drained Arctic soils to consume atmospheric CH4 using >40,000 hourly flux observations and spatially distributed flux measurements from 4 sites and 14 surface types.
A globally relevant stock of soil nitrogen in the Yedoma permafrost domain - Nature Communications
Material We included 1092 samples from late Pleistocene deposits and 1121 samples from Late Glacial to Holocene deposits. The thermokarst processes started during the Late Glacial warming (ca, 14,670 to ca. 12,890 years BP) and intensified during the Holocene thereafter. As the majority of the samples from thermokarst is from the Holocene, we referred to this sample category as Holocene.
Magnitude and Drivers of Potential Methane Oxidation and Production across the Tibetan Alpine Permafrost Region
Methane (CH4) dynamics across permafrost regions is critical in determining the magnitude and direction of permafrost carbon (C)-climate feedback. However, current studies are mainly derived from the Arctic area, with limited evidence from other permafrost regions.
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