Features of aerosol optical depth observed at Barrow, March 10-20, 1983
Total vertical aerosol optical depth over Barrow, Alaska, during March 1983 was up to four times greater than the average for recent years, with part of the excess being due to stratospheric debris from El Chichon. The variability in optical depth during a 10‐day period spanning the aircraft flights...
Gespeichert in:
Veröffentlicht in: | Geophys. Res. Lett.; (United States) 1984-05, Vol.11 (5), p.385-388 |
---|---|
Hauptverfasser: | , , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | 388 |
---|---|
container_issue | 5 |
container_start_page | 385 |
container_title | Geophys. Res. Lett.; (United States) |
container_volume | 11 |
creator | Dutton, Ellsworth G. DeLuisi, John J. Bodhaine, Barry A. |
description | Total vertical aerosol optical depth over Barrow, Alaska, during March 1983 was up to four times greater than the average for recent years, with part of the excess being due to stratospheric debris from El Chichon. The variability in optical depth during a 10‐day period spanning the aircraft flights of the Arctic Gas and Aerosol Sampling Program (AGASP) suggests a major tropospheric aerosol event on March 12 and 13, which accounts for the maximum observed optical depths. Occurrence of the tropospheric event is substantiated with independent aerosol data from aircraft, surface sampling, and synoptic scale meteorological data. Analysis of the Barrow optical depth data yields information on the climatic effects of both the stratospheric aerosol from El Chichon and the tropospheric aerosol commonly called Arctic haze. |
doi_str_mv | 10.1029/GL011i005p00385 |
format | Article |
fullrecord | <record><control><sourceid>proquest_osti_</sourceid><recordid>TN_cdi_proquest_miscellaneous_24213631</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>18335616</sourcerecordid><originalsourceid>FETCH-LOGICAL-c5680-1686839ab65b68ce3d6e063577f3c18c9b44994475594300a6e7084d4dbff5493</originalsourceid><addsrcrecordid>eNqNks9rFDEcxYNYcF09ew0i4qFjv_mdHLXYqbBtQZSCl5DJZNjR6WaazNr2v2-WKT146Pb0zeHzXr7Jewi9I_CZADVH9QoI6QHECMC0eIEWxHBeaQD1Ei0ATDlTJV-h1zn_gcIAIwtUnwQ3bVPIOHbYhRRzHHAcp967AbdhnNY4Njmkf6HFbsJfXUrx5hCfueTXmEBF4RATo9kbdNC5IYe3D3OJfp18-3l8Wq0u6u_HX1aVF1JDRaSWmhnXSNFI7QNrZQDJhFId80R703BuytpKCMMZgJNBgeYtb5uuE9ywJXo_-8Y89Tb7fgp-7eNmE_xkJaWCaFGgjzM0pni9DXmyV332YRjcJsRttpRTwiQjzwM53w8SzZiQRBbw09Og5JRqygTsRwXlrHyGeMb1nACnJYYlOppBX5LMKXR2TP2VS3eWgN3VxP5Xk6L48GDtcsm8S27j-_woM4oyonbGfMZu-iHc7XO19Y8VlbB7YzXL-jyF20eZS3-tVEwJe3le21PDgF7-PrOK3QMTedRI</addsrcrecordid><sourcetype>Open Access Repository</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>14104298</pqid></control><display><type>article</type><title>Features of aerosol optical depth observed at Barrow, March 10-20, 1983</title><source>Wiley Online Library All Journals</source><creator>Dutton, Ellsworth G. ; DeLuisi, John J. ; Bodhaine, Barry A.</creator><creatorcontrib>Dutton, Ellsworth G. ; DeLuisi, John J. ; Bodhaine, Barry A. ; Geophysical Monitoring for Climatic Change, Air Resources Laboratory, NOAA, Boulder, Colorado 80303</creatorcontrib><description>Total vertical aerosol optical depth over Barrow, Alaska, during March 1983 was up to four times greater than the average for recent years, with part of the excess being due to stratospheric debris from El Chichon. The variability in optical depth during a 10‐day period spanning the aircraft flights of the Arctic Gas and Aerosol Sampling Program (AGASP) suggests a major tropospheric aerosol event on March 12 and 13, which accounts for the maximum observed optical depths. Occurrence of the tropospheric event is substantiated with independent aerosol data from aircraft, surface sampling, and synoptic scale meteorological data. Analysis of the Barrow optical depth data yields information on the climatic effects of both the stratospheric aerosol from El Chichon and the tropospheric aerosol commonly called Arctic haze.</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/GL011i005p00385</identifier><identifier>CODEN: GPRLAJ</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>500200 - Environment, Atmospheric- Chemicals Monitoring & Transport- (-1989) ; AEROSOLS ; AIR POLLUTION ; Aircraft ; Aircraft components ; ALASKA ; ARCTIC REGIONS ; COLLOIDS ; Debris ; DISPERSIONS ; Earth, ocean, space ; ENVIRONMENTAL SCIENCES ; ERUPTION ; Exact sciences and technology ; External geophysics ; FEDERAL REGION X ; Geophysics ; Haze ; Meteorology ; NORTH AMERICA ; OPACITY ; OPTICAL PROPERTIES ; PARTICLES ; Particles and aerosols ; PARTICULATES ; PHYSICAL PROPERTIES ; POLAR REGIONS ; POLLUTION ; Sampling ; SOLS ; USA ; VOLCANOES</subject><ispartof>Geophys. Res. Lett.; (United States), 1984-05, Vol.11 (5), p.385-388</ispartof><rights>This paper is not subject to U.S. copyright.</rights><rights>1984 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c5680-1686839ab65b68ce3d6e063577f3c18c9b44994475594300a6e7084d4dbff5493</citedby><cites>FETCH-LOGICAL-c5680-1686839ab65b68ce3d6e063577f3c18c9b44994475594300a6e7084d4dbff5493</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2FGL011i005p00385$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2FGL011i005p00385$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,885,1416,27923,27924,45573,45574</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=9723178$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://www.osti.gov/biblio/6225185$$D View this record in Osti.gov$$Hfree_for_read</backlink></links><search><creatorcontrib>Dutton, Ellsworth G.</creatorcontrib><creatorcontrib>DeLuisi, John J.</creatorcontrib><creatorcontrib>Bodhaine, Barry A.</creatorcontrib><creatorcontrib>Geophysical Monitoring for Climatic Change, Air Resources Laboratory, NOAA, Boulder, Colorado 80303</creatorcontrib><title>Features of aerosol optical depth observed at Barrow, March 10-20, 1983</title><title>Geophys. Res. Lett.; (United States)</title><addtitle>Geophys. Res. Lett</addtitle><description>Total vertical aerosol optical depth over Barrow, Alaska, during March 1983 was up to four times greater than the average for recent years, with part of the excess being due to stratospheric debris from El Chichon. The variability in optical depth during a 10‐day period spanning the aircraft flights of the Arctic Gas and Aerosol Sampling Program (AGASP) suggests a major tropospheric aerosol event on March 12 and 13, which accounts for the maximum observed optical depths. Occurrence of the tropospheric event is substantiated with independent aerosol data from aircraft, surface sampling, and synoptic scale meteorological data. Analysis of the Barrow optical depth data yields information on the climatic effects of both the stratospheric aerosol from El Chichon and the tropospheric aerosol commonly called Arctic haze.</description><subject>500200 - Environment, Atmospheric- Chemicals Monitoring & Transport- (-1989)</subject><subject>AEROSOLS</subject><subject>AIR POLLUTION</subject><subject>Aircraft</subject><subject>Aircraft components</subject><subject>ALASKA</subject><subject>ARCTIC REGIONS</subject><subject>COLLOIDS</subject><subject>Debris</subject><subject>DISPERSIONS</subject><subject>Earth, ocean, space</subject><subject>ENVIRONMENTAL SCIENCES</subject><subject>ERUPTION</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>FEDERAL REGION X</subject><subject>Geophysics</subject><subject>Haze</subject><subject>Meteorology</subject><subject>NORTH AMERICA</subject><subject>OPACITY</subject><subject>OPTICAL PROPERTIES</subject><subject>PARTICLES</subject><subject>Particles and aerosols</subject><subject>PARTICULATES</subject><subject>PHYSICAL PROPERTIES</subject><subject>POLAR REGIONS</subject><subject>POLLUTION</subject><subject>Sampling</subject><subject>SOLS</subject><subject>USA</subject><subject>VOLCANOES</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1984</creationdate><recordtype>article</recordtype><recordid>eNqNks9rFDEcxYNYcF09ew0i4qFjv_mdHLXYqbBtQZSCl5DJZNjR6WaazNr2v2-WKT146Pb0zeHzXr7Jewi9I_CZADVH9QoI6QHECMC0eIEWxHBeaQD1Ei0ATDlTJV-h1zn_gcIAIwtUnwQ3bVPIOHbYhRRzHHAcp967AbdhnNY4Njmkf6HFbsJfXUrx5hCfueTXmEBF4RATo9kbdNC5IYe3D3OJfp18-3l8Wq0u6u_HX1aVF1JDRaSWmhnXSNFI7QNrZQDJhFId80R703BuytpKCMMZgJNBgeYtb5uuE9ywJXo_-8Y89Tb7fgp-7eNmE_xkJaWCaFGgjzM0pni9DXmyV332YRjcJsRttpRTwiQjzwM53w8SzZiQRBbw09Og5JRqygTsRwXlrHyGeMb1nACnJYYlOppBX5LMKXR2TP2VS3eWgN3VxP5Xk6L48GDtcsm8S27j-_woM4oyonbGfMZu-iHc7XO19Y8VlbB7YzXL-jyF20eZS3-tVEwJe3le21PDgF7-PrOK3QMTedRI</recordid><startdate>198405</startdate><enddate>198405</enddate><creator>Dutton, Ellsworth G.</creator><creator>DeLuisi, John J.</creator><creator>Bodhaine, Barry A.</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TV</scope><scope>C1K</scope><scope>7TG</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KR7</scope><scope>L7M</scope><scope>7TB</scope><scope>OTOTI</scope></search><sort><creationdate>198405</creationdate><title>Features of aerosol optical depth observed at Barrow, March 10-20, 1983</title><author>Dutton, Ellsworth G. ; DeLuisi, John J. ; Bodhaine, Barry A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c5680-1686839ab65b68ce3d6e063577f3c18c9b44994475594300a6e7084d4dbff5493</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1984</creationdate><topic>500200 - Environment, Atmospheric- Chemicals Monitoring & Transport- (-1989)</topic><topic>AEROSOLS</topic><topic>AIR POLLUTION</topic><topic>Aircraft</topic><topic>Aircraft components</topic><topic>ALASKA</topic><topic>ARCTIC REGIONS</topic><topic>COLLOIDS</topic><topic>Debris</topic><topic>DISPERSIONS</topic><topic>Earth, ocean, space</topic><topic>ENVIRONMENTAL SCIENCES</topic><topic>ERUPTION</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>FEDERAL REGION X</topic><topic>Geophysics</topic><topic>Haze</topic><topic>Meteorology</topic><topic>NORTH AMERICA</topic><topic>OPACITY</topic><topic>OPTICAL PROPERTIES</topic><topic>PARTICLES</topic><topic>Particles and aerosols</topic><topic>PARTICULATES</topic><topic>PHYSICAL PROPERTIES</topic><topic>POLAR REGIONS</topic><topic>POLLUTION</topic><topic>Sampling</topic><topic>SOLS</topic><topic>USA</topic><topic>VOLCANOES</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Dutton, Ellsworth G.</creatorcontrib><creatorcontrib>DeLuisi, John J.</creatorcontrib><creatorcontrib>Bodhaine, Barry A.</creatorcontrib><creatorcontrib>Geophysical Monitoring for Climatic Change, Air Resources Laboratory, NOAA, Boulder, Colorado 80303</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Pollution Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Mechanical & Transportation Engineering Abstracts</collection><collection>OSTI.GOV</collection><jtitle>Geophys. Res. Lett.; (United States)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Dutton, Ellsworth G.</au><au>DeLuisi, John J.</au><au>Bodhaine, Barry A.</au><aucorp>Geophysical Monitoring for Climatic Change, Air Resources Laboratory, NOAA, Boulder, Colorado 80303</aucorp><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Features of aerosol optical depth observed at Barrow, March 10-20, 1983</atitle><jtitle>Geophys. Res. Lett.; (United States)</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>1984-05</date><risdate>1984</risdate><volume>11</volume><issue>5</issue><spage>385</spage><epage>388</epage><pages>385-388</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>Total vertical aerosol optical depth over Barrow, Alaska, during March 1983 was up to four times greater than the average for recent years, with part of the excess being due to stratospheric debris from El Chichon. The variability in optical depth during a 10‐day period spanning the aircraft flights of the Arctic Gas and Aerosol Sampling Program (AGASP) suggests a major tropospheric aerosol event on March 12 and 13, which accounts for the maximum observed optical depths. Occurrence of the tropospheric event is substantiated with independent aerosol data from aircraft, surface sampling, and synoptic scale meteorological data. Analysis of the Barrow optical depth data yields information on the climatic effects of both the stratospheric aerosol from El Chichon and the tropospheric aerosol commonly called Arctic haze.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/GL011i005p00385</doi><tpages>4</tpages></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0094-8276 |
ispartof | Geophys. Res. Lett.; (United States), 1984-05, Vol.11 (5), p.385-388 |
issn | 0094-8276 1944-8007 |
language | eng |
recordid | cdi_proquest_miscellaneous_24213631 |
source | Wiley Online Library All Journals |
subjects | 500200 - Environment, Atmospheric- Chemicals Monitoring & Transport- (-1989) AEROSOLS AIR POLLUTION Aircraft Aircraft components ALASKA ARCTIC REGIONS COLLOIDS Debris DISPERSIONS Earth, ocean, space ENVIRONMENTAL SCIENCES ERUPTION Exact sciences and technology External geophysics FEDERAL REGION X Geophysics Haze Meteorology NORTH AMERICA OPACITY OPTICAL PROPERTIES PARTICLES Particles and aerosols PARTICULATES PHYSICAL PROPERTIES POLAR REGIONS POLLUTION Sampling SOLS USA VOLCANOES |
title | Features of aerosol optical depth observed at Barrow, March 10-20, 1983 |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-12T05%3A14%3A44IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_osti_&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Features%20of%20aerosol%20optical%20depth%20observed%20at%20Barrow,%20March%2010-20,%201983&rft.jtitle=Geophys.%20Res.%20Lett.;%20(United%20States)&rft.au=Dutton,%20Ellsworth%20G.&rft.aucorp=Geophysical%20Monitoring%20for%20Climatic%20Change,%20Air%20Resources%20Laboratory,%20NOAA,%20Boulder,%20Colorado%2080303&rft.date=1984-05&rft.volume=11&rft.issue=5&rft.spage=385&rft.epage=388&rft.pages=385-388&rft.issn=0094-8276&rft.eissn=1944-8007&rft.coden=GPRLAJ&rft_id=info:doi/10.1029/GL011i005p00385&rft_dat=%3Cproquest_osti_%3E18335616%3C/proquest_osti_%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=14104298&rft_id=info:pmid/&rfr_iscdi=true |