Long-term decline of global atmospheric ethane concentrations and implications for methane

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Long-term decline of global atmospheric ethane concentrations and implications for methane. / Simpson, Isobel J; Andersen, Mads Peter Sulbæk; Meinardi, Simone; Bruhwiler, Lori; Blake, Nicola J; Helmig, Detlev; Rowland, F Sherwood; Blake, Donald R.

I: Nature, Bind 488, Nr. 7412, 23.08.2012, s. 490-4.

Publikation: Bidrag til tidsskriftTidsskriftartikelForskningfagfællebedømt

Harvard

Simpson, IJ, Andersen, MPS, Meinardi, S, Bruhwiler, L, Blake, NJ, Helmig, D, Rowland, FS & Blake, DR 2012, 'Long-term decline of global atmospheric ethane concentrations and implications for methane', Nature, bind 488, nr. 7412, s. 490-4. https://doi.org/10.1038/nature11342

APA

Simpson, I. J., Andersen, M. P. S., Meinardi, S., Bruhwiler, L., Blake, N. J., Helmig, D., Rowland, F. S., & Blake, D. R. (2012). Long-term decline of global atmospheric ethane concentrations and implications for methane. Nature, 488(7412), 490-4. https://doi.org/10.1038/nature11342

Vancouver

Simpson IJ, Andersen MPS, Meinardi S, Bruhwiler L, Blake NJ, Helmig D o.a. Long-term decline of global atmospheric ethane concentrations and implications for methane. Nature. 2012 aug. 23;488(7412):490-4. https://doi.org/10.1038/nature11342

Author

Simpson, Isobel J ; Andersen, Mads Peter Sulbæk ; Meinardi, Simone ; Bruhwiler, Lori ; Blake, Nicola J ; Helmig, Detlev ; Rowland, F Sherwood ; Blake, Donald R. / Long-term decline of global atmospheric ethane concentrations and implications for methane. I: Nature. 2012 ; Bind 488, Nr. 7412. s. 490-4.

Bibtex

@article{477f1f6c0e554e518539a8656978be3b,
title = "Long-term decline of global atmospheric ethane concentrations and implications for methane",
abstract = "After methane, ethane is the most abundant hydrocarbon in the remote atmosphere. It is a precursor to tropospheric ozone and it influences the atmosphere's oxidative capacity through its reaction with the hydroxyl radical, ethane's primary atmospheric sink. Here we present the longest continuous record of global atmospheric ethane levels. We show that global ethane emission rates decreased from 14.3 to 11.3 teragrams per year, or by 21 per cent, from 1984 to 2010. We attribute this to decreasing fugitive emissions from ethane's fossil fuel source--most probably decreased venting and flaring of natural gas in oil fields--rather than a decline in its other major sources, biofuel use and biomass burning. Ethane's major emission sources are shared with methane, and recent studies have disagreed on whether reduced fossil fuel or microbial emissions have caused methane's atmospheric growth rate to slow. Our findings suggest that reduced fugitive fossil fuel emissions account for at least 10-21 teragrams per year (30-70 per cent) of the decrease in methane's global emissions, significantly contributing to methane's slowing atmospheric growth rate since the mid-1980s.",
author = "Simpson, {Isobel J} and Andersen, {Mads Peter Sulb{\ae}k} and Simone Meinardi and Lori Bruhwiler and Blake, {Nicola J} and Detlev Helmig and Rowland, {F Sherwood} and Blake, {Donald R}",
year = "2012",
month = aug,
day = "23",
doi = "10.1038/nature11342",
language = "English",
volume = "488",
pages = "490--4",
journal = "Nature",
issn = "0028-0836",
publisher = "nature publishing group",
number = "7412",

}

RIS

TY - JOUR

T1 - Long-term decline of global atmospheric ethane concentrations and implications for methane

AU - Simpson, Isobel J

AU - Andersen, Mads Peter Sulbæk

AU - Meinardi, Simone

AU - Bruhwiler, Lori

AU - Blake, Nicola J

AU - Helmig, Detlev

AU - Rowland, F Sherwood

AU - Blake, Donald R

PY - 2012/8/23

Y1 - 2012/8/23

N2 - After methane, ethane is the most abundant hydrocarbon in the remote atmosphere. It is a precursor to tropospheric ozone and it influences the atmosphere's oxidative capacity through its reaction with the hydroxyl radical, ethane's primary atmospheric sink. Here we present the longest continuous record of global atmospheric ethane levels. We show that global ethane emission rates decreased from 14.3 to 11.3 teragrams per year, or by 21 per cent, from 1984 to 2010. We attribute this to decreasing fugitive emissions from ethane's fossil fuel source--most probably decreased venting and flaring of natural gas in oil fields--rather than a decline in its other major sources, biofuel use and biomass burning. Ethane's major emission sources are shared with methane, and recent studies have disagreed on whether reduced fossil fuel or microbial emissions have caused methane's atmospheric growth rate to slow. Our findings suggest that reduced fugitive fossil fuel emissions account for at least 10-21 teragrams per year (30-70 per cent) of the decrease in methane's global emissions, significantly contributing to methane's slowing atmospheric growth rate since the mid-1980s.

AB - After methane, ethane is the most abundant hydrocarbon in the remote atmosphere. It is a precursor to tropospheric ozone and it influences the atmosphere's oxidative capacity through its reaction with the hydroxyl radical, ethane's primary atmospheric sink. Here we present the longest continuous record of global atmospheric ethane levels. We show that global ethane emission rates decreased from 14.3 to 11.3 teragrams per year, or by 21 per cent, from 1984 to 2010. We attribute this to decreasing fugitive emissions from ethane's fossil fuel source--most probably decreased venting and flaring of natural gas in oil fields--rather than a decline in its other major sources, biofuel use and biomass burning. Ethane's major emission sources are shared with methane, and recent studies have disagreed on whether reduced fossil fuel or microbial emissions have caused methane's atmospheric growth rate to slow. Our findings suggest that reduced fugitive fossil fuel emissions account for at least 10-21 teragrams per year (30-70 per cent) of the decrease in methane's global emissions, significantly contributing to methane's slowing atmospheric growth rate since the mid-1980s.

U2 - 10.1038/nature11342

DO - 10.1038/nature11342

M3 - Journal article

C2 - 22914166

VL - 488

SP - 490

EP - 494

JO - Nature

JF - Nature

SN - 0028-0836

IS - 7412

ER -

ID: 44565274