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A 30-Year Record of the Isotopic Composition of Atmospheric Methane

<p> Methane (CH<sub>4</sub>) is one of the most important greenhouse gases after water vapor and carbon dioxide due to its high concentration and global warming potential 25 times than that of CO<sub>2</sub>(based on a 100 year time horizon). Its atmospheric concentration has more than doubled from the preindustrial era due to anthropogenic activities such as rice cultivation, biomass burning, and fossil fuel production. However, the rate of increase of atmospheric CH<sub>4</sub> (or the growth rate) slowed from 1980 until present. The main reason for this trend is a slowdown in the trend of CH<sub> 4</sub>sources. Measuring stable isotopes of atmospheric CH<sub>4</sub> can constrain changes of CH<sub>4</sub>sources. The main goal of this work is to interpret the CH<sub>4</sub> trend from 1978-2010 in terms of its sources using measurements of CH<sub>4</sub> mixing ratio and its isotopes. </p><p> The current work presents the measurements and analysis of CH<sub>4</sub> and its isotopes (&delta;<sup>13</sup>C and &delta;D) of four air archive sample sets collected by the Oregon Graduate Institute (OGI). CH<sub>4</sub> isotope ratios (&delta;<sup>13</sup>C and &delta;D) were measured by a continuous flow isotope ratio mass spectrometer technique developed at PSU. The first set is for Cape Meares, Oregon which is the oldest and longest set and spans 1977-1999. The integrity of this sample set was evaluated by comparing between our measured CH<sub>4</sub> mixing ratio values with those measured values by OGI and was found to be stable. Resulting CH<sub>4</sub> seasonal cycle was evaluated from the Cape Meares data. The CH<sub>4</sub> seasonal cycle shows a broad maximum during October-April and a minimum between July and August. The seasonal cycles of &delta;<sup>13</sup>C and &delta;D have maximum values in May for &delta;<sup>13</sup>C and in July for &delta;D and minimum values between September-October for &delta;<sup>13</sup>C and in October for &delta;D. These results indicate a CH<sub>4</sub> source that is more enriched January-May (e.g. biomass burning) and a source that is more depleted August-October (e.g. microbial). In addition to Cape Meares, air archive sets were analyzed from: South Pole (SPO), Samoa (SMO), Mauna Loa (MLO) 1992-1996. The presented &delta;D measurements are unique measured values during these time periods at these stations. </p><p> To obtain the long-term in isotopic CH<sub>4</sub> from 1978-2010, other datasets of Northern Hemisphere mid-latitude sites are included with Cape Meares. These sites are Olympic Peninsula, Washington; Monta&ntilde;a de Oro, California; and Niwot Ridge, Colorado. The seasonal cycles of CH<sub>4</sub> and its isotopes from the composite dataset have the same phase and amplitudes as the Cape Meares site. CH<sub>4</sub> growth rate shows a decrease over time 1978-2010 with three main spikes in 1992, 1998, and 2003 consistent with the literature from the global trend. CH<sub>4</sub> lifetime is estimated to 9.7 yrs. The &delta;<sup>13</sup>C trend in the composite data shows a slow increase from 1978-1987, a more rapid rate of change 1987-2005, and a gradual depletion during 2005-2010. The &delta;D trend in the composite data shows a gradual increase during 1978-2001 and decrease from 2001-2005. From these results, the global CH<sub>4</sub> emissions are estimated and show a leveling off sources 1982-2010 with two large peak anomalies in 1998 and 2003. The global average &delta;<sup>13</sup>C and &delta;D of CH<sub> 4</sub> sources are estimated from measured values. The results of these calculations indicate that there is more than one source which controls the decrease in the global CH4 trend. From 1982-2001, &delta;<sup>13</sup>C and &delta;D of CH<sub>4</sub> sources becomes more depleted due to a decrease in fossil and/or biomass burning sources relative to microbial sources. From 2005-2010, &delta;<sup> 13</sup>C of CH<sub>4</sub> sources returns to its 1981 value. There are two significant peaks in &delta;<sup>13</sup>C and &delta;D of CH<sub> 4</sub> sources in 1998 and 2003 due to the wildfire emissions in boreal areas and in Europe.</p>

Identiferoai:union.ndltd.org:PROQUEST/oai:pqdtoai.proquest.com:3557627
Date04 May 2013
CreatorsTeama, Doaa Galal
PublisherPortland State University
Source SetsProQuest.com
LanguageEnglish
Detected LanguageEnglish
Typethesis

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