Arctic methane sources: Isotopic evidence for atmospheric inputs
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δ(13)C-CH4 reveals CH4 variations over oceans from mid-latitudes to the ArcticWidespread methane seepage along the continental margin off Svalbard - from Bjørnøya to Kongsfjorden.Subterranean atmospheres may act as daily methane sinks.Assessing Connectivity Between an Overlying Aquifer and a Coal Seam Gas Resource Using Methane Isotopes, Dissolved Organic Carbon and TritiumGlacial/interglacial wetland, biomass burning, and geologic methane emissions constrained by dual stable isotopic CH4 ice core records.Constraints on oceanic methane emissions west of Svalbard from atmospheric in situ measurements and Lagrangian transport modeling.Automated simultaneous measurement of the δ(13) C and δ(2) H values of methane and the δ(13) C and δ(18) O values of carbon dioxide in flask air samples using a new multi cryo-trap/gas chromatography/isotope ratio mass spectrometry system.Gas hydrate dissociation off Svalbard induced by isostatic rebound rather than global warming.Atmospheric observations of Arctic Ocean methane emissions up to 82° northGas hydrate distribution and hydrocarbon maturation north of the Knipovich Ridge, western Svalbard marginSeismic evidence for shallow gas-escape features associated with a retreating gas hydrate zone offshore west SvalbardThe interaction of climate change and methane hydratesA joint electromagnetic and seismic study of an active pockmark within the hydrate stability field at the Vestnesa Ridge, West Svalbard marginPaleo-methane emissions recorded in foraminifera near the landward limit of the gas hydrate stability zone offshore western SvalbardBivalve shell horizons in seafloor pockmarks of the last glacial-interglacial transition: a thousand years of methane emissions in the Arctic OceanMeasurement of the 13 C isotopic signature of methane emissions from northern European wetlandsMeasurements of δ13C in CH4and using particle dispersion modeling to characterize sources of Arctic methane within an air massExtensive release of methane from Arctic seabed west of Svalbard during summer 2014 does not influence the atmosphereFluxes and fate of dissolved methane released at the seafloor at the landward limit of the gas hydrate stability zone offshore western SvalbardCarbon isotope ratios suggest no additional methane from boreal wetlands during the rapid Greenland Interstadial 21.2
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Arctic methane sources: Isotopic evidence for atmospheric inputs
description
article
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im November 2011 veröffentlichter wissenschaftlicher Artikel
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wetenschappelijk artikel
@nl
наукова стаття, опублікована в листопаді 2011
@uk
name
Arctic methane sources: Isotopic evidence for atmospheric inputs
@en
Arctic methane sources: Isotopic evidence for atmospheric inputs
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type
label
Arctic methane sources: Isotopic evidence for atmospheric inputs
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Arctic methane sources: Isotopic evidence for atmospheric inputs
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prefLabel
Arctic methane sources: Isotopic evidence for atmospheric inputs
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Arctic methane sources: Isotopic evidence for atmospheric inputs
@nl
P2093
P2860
P356
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Arctic methane sources: Isotopic evidence for atmospheric inputs
@en
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C. Lund Myhre
C. M. R. Fowler
E. G. Nisbet
J. Mienert
M. Lanoisellé
O. Hermansen
P. B. R. Nisbet-Jones
R. E. Fisher
R. H. James
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P356
10.1029/2011GL049319
P407
P577
2011-11-01T00:00:00Z