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contributor authorKahn, Ralph A.
contributor authorOgren, John A.
contributor authorAckerman, Thomas P.
contributor authorBösenberg, Jens
contributor authorCharlson, Robert J.
contributor authorDiner, David J.
contributor authorHolben, Brent N.
contributor authorMenzies, Robert T.
contributor authorMiller, Mark A.
contributor authorSeinfeld, John H.
date accessioned2017-06-09T16:42:22Z
date available2017-06-09T16:42:22Z
date copyright2004/10/01
date issued2004
identifier issn0003-0007
identifier otherams-72638.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4214663
description abstractWe briefly but systematically review major sources of aerosol data, emphasizing suites of measurements that seem most likely to contribute to assessments of global aerosol climate forcing. The strengths and limitations of existing satellite, surface, and aircraft remote sensing systems are described, along with those of direct sampling networks and ship-based stations. It is evident that an enormous number of aerosol-related observations have been made, on a wide range of spatial and temporal sampling scales, and that many of the key gaps in this collection of data could be filled by technologies that either exist or are expected to be available in the near future. Emphasis must be given to combining remote sensing and in situ active and passive observations and integrating them with aerosol chemical transport models, in order to create a more complete environmental picture, having sufficient detail to address current climate forcing questions. The Progressive Aerosol Retrieval and Assimilation Global Observing Network (PARAGON) initiative would provide an organizational framework to meet this goal.
publisherAmerican Meteorological Society
titleAerosol Data Sources and Their Roles within PARAGON
typeJournal Paper
journal volume85
journal issue10
journal titleBulletin of the American Meteorological Society
identifier doi10.1175/BAMS-85-10-1511
journal fristpage1511
journal lastpage1522
treeBulletin of the American Meteorological Society:;2004:;volume( 085 ):;issue: 010
contenttypeFulltext


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