Satellite based detection of Volcanic SO2 over PakistanView Crossref metadata(active tab) <div id="edit-xml" class="form-item form-type-item"> <?xml version="1.0"?> <doi_batch version="4.4.1" xmlns="http://www.crossref.org/schema/4.4.1" xmlns:jats="http://www.ncbi.nlm.nih.gov/JATS1" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.crossref.org/schema/4.4.1 http://www.crossref.org/schemas/crossref4.4.1.xsd"><head><doi_batch_id>000699</doi_batch_id><timestamp>1714895166</timestamp><depositor><depositor_name>University of the Aegean</depositor_name><email_address>uoa@university.com</email_address></depositor><registrant>Global NEST Journal</registrant></head><body><journal><journal_metadata><full_title>Global NEST Journal</full_title><full_title>Global NEST: the international Journal</full_title><issn media_type="print">1790-7632</issn><issn media_type="electronic">2241-777X</issn></journal_metadata><journal_issue><titles><title>Issue 3</title></titles><publication_date><month>09</month><year>2024</year></publication_date><journal_volume><volume>18</volume></journal_volume><issue>3</issue></journal_issue><journal_article><titles><title>Satellite based detection of Volcanic SO2 over Pakistan</title></titles><abstract xmlns="http://www.ncbi.nlm.nih.gov/JATS1"><p><div> <p>The present study is carried out to explain the presence of large concentrations of SO<sub>2</sub> in atmosphere of Pakistan during June, 2011. Large volcanic eruptions are a major source of greenhouse and trace gases. The eruption of Mount Nabro in June, 2011 injected large amount of SO<sub>2 </sub>into stratosphere. Nabro volcanic eruption generated a layer of sulfate aerosols, which resided in stratosphere for months. The total amount of SO<sub>2 </sub>that was injected into the atmosphere was estimated to be 1.3-2.0 Tg. Data products of Global Ozone Monitoring Experiment (GOME-2), Ozone Monitoring Instrument (OMI) and Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) were used to study SO<sub>2</sub> concentrations and plume movement over Pakistan. HYSPLIT backward trajectory model is utilized to study the origin of SO<sub>2</sub> plume. The study confirms that SO<sub>2</sub> plume originated from Nabro volcanic eruption and caused significant atmospheric perturbations and affected the air quality of Pakistan. SO<sub>2</sub> emissions from volcanic eruptions can pose serious hazard to population as well as global climate.</p> </div> <p> </p> </p></abstract><publication_date><month>06</month><day>24</day><year>2016</year></publication_date><pages><first_page>591</first_page><last_page>598</last_page></pages><publisher_item><identifier id_type="pii">gnest_01910</identifier></publisher_item><doi_data><doi>10.30955/gnj.001910</doi><timestamp>1714895166</timestamp><resource>https://journal.gnest.org/publication/gnest_01910</resource></doi_data></journal_article></journal></body></doi_batch> </div>
