Measurement report: Regional characteristics of seasonal and long-term variations in greenhouse gases at Nainital, India, and Comilla, Bangladesh
<p>Emissions of greenhouse gases (GHGs) from the Indian subcontinent have increased during the last 20 years along with rapid economic growth; however, there remains a paucity of GHG measurements for policy-relevant research. In northern India and Bangladesh, agricultural activities are consid...
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| Autores principales: | , , , , , , , |
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| Formato: | article |
| Lenguaje: | EN |
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Copernicus Publications
2021
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| Materias: | |
| Acceso en línea: | https://doaj.org/article/51d2b2de7c9c419cb7f12e31e97bc8cd |
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| Sumario: | <p>Emissions of greenhouse gases (GHGs) from the Indian subcontinent have increased during the last 20 years along with rapid economic growth; however, there remains a paucity of GHG measurements for policy-relevant research. In northern India and Bangladesh, agricultural activities are
considered to play an important role in GHG concentrations in the atmosphere. We performed weekly air sampling at Nainital (NTL) in northern India and Comilla (CLA) in Bangladesh from 2006 and 2012, respectively. Air
samples were analyzed for dry-air gas mole fractions of <span class="inline-formula">CO<sub>2</sub></span>, <span class="inline-formula">CH<sub>4</sub></span>, <span class="inline-formula">CO</span>, <span class="inline-formula">H<sub>2</sub></span>, N<span class="inline-formula"><sub>2</sub></span>O, and SF<span class="inline-formula"><sub>6</sub></span> and carbon and oxygen isotopic ratios of CO<span class="inline-formula"><sub>2</sub></span> (<span class="inline-formula"><i>δ</i><sup>13</sup></span>C-CO<span class="inline-formula"><sub>2</sub></span> and <span class="inline-formula"><i>δ</i><sup>18</sup></span>O-CO<span class="inline-formula"><sub>2</sub></span>). Regional characteristics of these components over the Indo-Gangetic Plain
are discussed compared to data from other Indian sites and Mauna Loa, Hawaii (MLO), which is representative of marine background air.</p>
<p>We found that the CO<span class="inline-formula"><sub>2</sub></span> mole fraction at CLA had two seasonal minima in
February–March and September, corresponding to crop cultivation activities
that depend on regional climatic conditions. Although NTL had only one clear
minimum in September, the carbon isotopic signature suggested that photosynthetic CO<span class="inline-formula"><sub>2</sub></span> absorption by crops cultivated in each season
contributes differently to lower CO<span class="inline-formula"><sub>2</sub></span> mole fractions at both sites. The
CH<span class="inline-formula"><sub>4</sub></span> mole fraction of NTL and CLA in August–October showed high values (i.e., sometimes over 4000 ppb at CLA), mainly due to the influence of CH<span class="inline-formula"><sub>4</sub></span> emissions from the paddy fields. High CH<span class="inline-formula"><sub>4</sub></span> mole fractions
sustained over months at CLA were a characteristic feature on the Indo-Gangetic Plain, which were affected by both the local emission and air mass transport. The CO mole fractions at NTL were also high and showed peaks
in May and October, while CLA had much higher peaks in October–March due to the influence of human activities such as emissions from biomass burning and
brick production. The N<span class="inline-formula"><sub>2</sub></span>O mole fractions at NTL and CLA increased in
June–August and November–February, which coincided with the application of
nitrogen fertilizer and the burning of biomass such as the harvest residues
and dung for domestic cooking. Based on H<span class="inline-formula"><sub>2</sub></span> seasonal variation at both
sites, it appeared that the emissions in this region were related to biomass
burning in addition to production from the reaction of OH and CH<span class="inline-formula"><sub>4</sub></span>. The
SF<span class="inline-formula"><sub>6</sub></span> mole fraction was similar to that at MLO, suggesting that there
were few anthropogenic SF<span class="inline-formula"><sub>6</sub></span> emission sources in the district.</p>
<p>The variability of the CO<span class="inline-formula"><sub>2</sub></span> growth rate at NTL was different from the variability in the CO<span class="inline-formula"><sub>2</sub></span> growth rate at MLO, which is more closely linked
to the El Niño–Southern Oscillation (ENSO). In addition, the growth rates of the CH<span class="inline-formula"><sub>4</sub></span> and SF<span class="inline-formula"><sub>6</sub></span> mole fractions at NTL showed an anticorrelation with those at MLO, indicating that the frequency of
southerly air masses strongly influenced these mole fractions. These findings showed that rather large regional<span id="page16428"/> climatic conditions considerably
controlled interannual variations in GHGs, <span class="inline-formula"><i>δ</i><sup>13</sup></span>C-CO<span class="inline-formula"><sub>2</sub></span>, and
<span class="inline-formula"><i>δ</i><sup>18</sup></span>O-CO<span class="inline-formula"><sub>2</sub></span> through changes in precipitation and air mass.</p> |
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