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In situ measurements of tropospheric volcanic plumes in Ecuador and Colombia during TC^sup 4
A NASA DC-8 research aircraft penetrated tropospheric gas and aerosol plumes sourced from active volcanoes in Ecuador and Colombia during the Tropical Composition, Cloud and Climate Coupling (TC^sub 4^) mission in July-August 2007. The likely source volcanoes were Tungurahua (Ecuador) and Nevado del...
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Published in: | Journal of geophysical research. Atmospheres 2011-05, Vol.116 (10), p.1B |
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creator | Carn, S A Froyd, K D Anderson, B E Wennberg, P Crounse, J Spencer, K Dibb, J E Krotkov, N A Browell, E V Hair, J W Diskin, G Sachse, G Vay, S A |
description | A NASA DC-8 research aircraft penetrated tropospheric gas and aerosol plumes sourced from active volcanoes in Ecuador and Colombia during the Tropical Composition, Cloud and Climate Coupling (TC^sub 4^) mission in July-August 2007. The likely source volcanoes were Tungurahua (Ecuador) and Nevado del Huila (Colombia). The TC^sub 4^ data provide rare insight into the chemistry of volcanic plumes in the tropical troposphere, and permit a comparison of SO2 column amounts measured by the Ozone Monitoring Instrument on the Aura satellite with in situ SO2 measurements. Elevated concentrations of SO2, sulfate aerosol, and particles were measured by DC-8 instrumentation in volcanic outflow at altitudes of 3-6 km. Estimated plume ages range from ∼2 h at Huila to ∼22-48 h downwind of Ecuador. The plumes contained sulfate-rich accumulation mode particles that were variably neutralized and often highly acidic. A significant fraction of supermicron volcanic ash was evident in one plume. The TC^sub 4^ data set provides further evidence of the impact of volcanic emissions on tropospheric acidity and oxidizing capacity. |
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The likely source volcanoes were Tungurahua (Ecuador) and Nevado del Huila (Colombia). The TC^sub 4^ data provide rare insight into the chemistry of volcanic plumes in the tropical troposphere, and permit a comparison of SO2 column amounts measured by the Ozone Monitoring Instrument on the Aura satellite with in situ SO2 measurements. Elevated concentrations of SO2, sulfate aerosol, and particles were measured by DC-8 instrumentation in volcanic outflow at altitudes of 3-6 km. Estimated plume ages range from ∼2 h at Huila to ∼22-48 h downwind of Ecuador. The plumes contained sulfate-rich accumulation mode particles that were variably neutralized and often highly acidic. A significant fraction of supermicron volcanic ash was evident in one plume. The TC^sub 4^ data set provides further evidence of the impact of volcanic emissions on tropospheric acidity and oxidizing capacity.</description><identifier>ISSN: 2169-897X</identifier><identifier>EISSN: 2169-8996</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Acidity ; Aerosols ; Atmospheric chemistry ; Emission measurements ; Geophysics ; In situ measurement ; Instrumentation ; Monitoring instruments ; Plumes ; Sulfates ; Sulfur dioxide ; Troposphere ; Volcanoes</subject><ispartof>Journal of geophysical research. 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Atmospheres</title><description>A NASA DC-8 research aircraft penetrated tropospheric gas and aerosol plumes sourced from active volcanoes in Ecuador and Colombia during the Tropical Composition, Cloud and Climate Coupling (TC^sub 4^) mission in July-August 2007. The likely source volcanoes were Tungurahua (Ecuador) and Nevado del Huila (Colombia). The TC^sub 4^ data provide rare insight into the chemistry of volcanic plumes in the tropical troposphere, and permit a comparison of SO2 column amounts measured by the Ozone Monitoring Instrument on the Aura satellite with in situ SO2 measurements. Elevated concentrations of SO2, sulfate aerosol, and particles were measured by DC-8 instrumentation in volcanic outflow at altitudes of 3-6 km. Estimated plume ages range from ∼2 h at Huila to ∼22-48 h downwind of Ecuador. The plumes contained sulfate-rich accumulation mode particles that were variably neutralized and often highly acidic. A significant fraction of supermicron volcanic ash was evident in one plume. The TC^sub 4^ data set provides further evidence of the impact of volcanic emissions on tropospheric acidity and oxidizing capacity.</description><subject>Acidity</subject><subject>Aerosols</subject><subject>Atmospheric chemistry</subject><subject>Emission measurements</subject><subject>Geophysics</subject><subject>In situ measurement</subject><subject>Instrumentation</subject><subject>Monitoring instruments</subject><subject>Plumes</subject><subject>Sulfates</subject><subject>Sulfur dioxide</subject><subject>Troposphere</subject><subject>Volcanoes</subject><issn>2169-897X</issn><issn>2169-8996</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><recordid>eNqNijsLwjAURoMoWLT_4YJzoe_HXCq6d3AQS2xTTWlzY27j77eDOHuW78B3VswJg7Tw8qJI1z_PLlvmEg3-Qu5HcRI77HpWQHK2MAlO1ohJqJkAe5gNaiT9FEa28Max5WoRPdpJEEgFVWt5hwa46qDEEae75NBZI9UD6vJGVkO8Z5uejyTc7-7Y4VjV5cnTBl9W0NwMaI1ariZIwyTKs9Avov-qD6KWRWQ</recordid><startdate>20110515</startdate><enddate>20110515</enddate><creator>Carn, S A</creator><creator>Froyd, K D</creator><creator>Anderson, B E</creator><creator>Wennberg, P</creator><creator>Crounse, J</creator><creator>Spencer, K</creator><creator>Dibb, J E</creator><creator>Krotkov, N A</creator><creator>Browell, E V</creator><creator>Hair, J W</creator><creator>Diskin, G</creator><creator>Sachse, G</creator><creator>Vay, S A</creator><general>Blackwell Publishing Ltd</general><scope>3V.</scope><scope>7TG</scope><scope>7UA</scope><scope>7XB</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>L7M</scope><scope>M2O</scope><scope>M7S</scope><scope>MBDVC</scope><scope>P5Z</scope><scope>P62</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope></search><sort><creationdate>20110515</creationdate><title>In situ measurements of tropospheric volcanic plumes in Ecuador and Colombia during TC^sup 4</title><author>Carn, S A ; 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Atmospheres</jtitle><date>2011-05-15</date><risdate>2011</risdate><volume>116</volume><issue>10</issue><spage>1B</spage><pages>1B-</pages><issn>2169-897X</issn><eissn>2169-8996</eissn><abstract>A NASA DC-8 research aircraft penetrated tropospheric gas and aerosol plumes sourced from active volcanoes in Ecuador and Colombia during the Tropical Composition, Cloud and Climate Coupling (TC^sub 4^) mission in July-August 2007. The likely source volcanoes were Tungurahua (Ecuador) and Nevado del Huila (Colombia). The TC^sub 4^ data provide rare insight into the chemistry of volcanic plumes in the tropical troposphere, and permit a comparison of SO2 column amounts measured by the Ozone Monitoring Instrument on the Aura satellite with in situ SO2 measurements. Elevated concentrations of SO2, sulfate aerosol, and particles were measured by DC-8 instrumentation in volcanic outflow at altitudes of 3-6 km. Estimated plume ages range from ∼2 h at Huila to ∼22-48 h downwind of Ecuador. The plumes contained sulfate-rich accumulation mode particles that were variably neutralized and often highly acidic. A significant fraction of supermicron volcanic ash was evident in one plume. The TC^sub 4^ data set provides further evidence of the impact of volcanic emissions on tropospheric acidity and oxidizing capacity.</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub></addata></record> |
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subjects | Acidity Aerosols Atmospheric chemistry Emission measurements Geophysics In situ measurement Instrumentation Monitoring instruments Plumes Sulfates Sulfur dioxide Troposphere Volcanoes |
title | In situ measurements of tropospheric volcanic plumes in Ecuador and Colombia during TC^sup 4 |
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