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Showing 1–10 of 10 results
Advanced filters: Author: Edward J. Dlugokencky Clear advanced filters
  • The net balance of terrestrial biogenic greenhouse gases produced as a result of human activities and the climatic impact of this balance are uncertain; here the net cumulative impact of the three greenhouse gases, methane, nitrous oxide and carbon dioxide, on the planetary energy budget from 2001 to 2010 is a warming of the planet.

    • Hanqin Tian
    • Chaoqun Lu
    • Steven C. Wofsy
    Research
    Nature
    Volume: 531, P: 225-228
  • Bottom-up and top-down approaches are used to quantify global nitrous oxide sources and sinks resulting from both natural and anthropogenic sources, revealing a 30% increase in global human-induced emissions between 1980 and 2016.

    • Hanqin Tian
    • Rongting Xu
    • Yuanzhi Yao
    Research
    Nature
    Volume: 586, P: 248-256
  • A late-autumn shoulder is consistently observed in the seasonal cycles of atmospheric methane at high latitude sites, but the sources responsible remain uncertain. This study reports methane flux measurements from a high Arctic setting during the onset of soil freezing. The integral of the emissions during this freeze-in period amount to approximately the same amount of methane emitted during the entire summer season. It is found that the observed early winter emission burst improves the agreement between the simulated seasonal cycle and atmospheric data from latitudes north of 60°N. The results suggest that permafrost associated freeze-in bursts of methane emissions from tundra regions could be an important component of the seasonal distribution of methane emissions from high latitudes.

    • Mikhail Mastepanov
    • Charlotte Sigsgaard
    • Torben R. Christensen
    Research
    Nature
    Volume: 456, P: 628-630
  • Methane is an important greenhouse gas, responsible for about 20% of the warming induced by long-lived greenhouse gases since pre-industrial times. A compilation of observations and results from chemical transport, ecosystem and climate chemistry models suggests that a rise in wetland and fossil fuel emissions probably accounts for the renewed increase in global methane levels after 2006.

    • Stefanie Kirschke
    • Philippe Bousquet
    • Guang Zeng
    Reviews
    Nature Geoscience
    Volume: 6, P: 813-823
  • Models overestimate Arctic methane emissions compared to observations. Incorporating microbial dynamics into biogeochemistry models helps reconcile this discrepancy; high-affinity methanotrophs are an important part of the Arctic methane budget and double previous estimates of methane sinks.

    • Youmi Oh
    • Qianlai Zhuang
    • Bo Elberling
    Research
    Nature Climate Change
    Volume: 10, P: 317-321
  • A process-based carbon isotope biogeochemistry model substantially reduces uncertainty in regional and global estimates of the stable carbon isotopic composition of methane emissions from wetlands and suggests rising atmospheric concentrations are due to increased microbial emissions.

    • Youmi Oh
    • Qianlai Zhuang
    • Jeffrey P. Chanton
    ResearchOpen Access
    Communications Earth & Environment
    Volume: 3, P: 1-12