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contributor authorStevens, Bjorn
contributor authorAment, Felix
contributor authorBony, Sandrine
contributor authorCrewell, Susanne
contributor authorEwald, Florian
contributor authorGross, Silke
contributor authorHansen, Akio
contributor authorHirsch, Lutz
contributor authorJacob, Marek
contributor authorKölling, Tobias
contributor authorKonow, Heike
contributor authorMayer, Bernhard
contributor authorWendisch, Manfred
contributor authorWirth, Martin
contributor authorWolf, Kevin
contributor authorBakan, Stephan
contributor authorBauer-Pf
date accessioned2019-10-05T06:53:28Z
date available2019-10-05T06:53:28Z
date copyright1/18/2019 12:00:00 AM
date issued2019
identifier otherBAMS-D-18-0198.1.pdf
identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4263748
description abstractAbstractA configuration of the High-Altitude Long-Range Research Aircraft (HALO) as a remote sensing cloud observatory is described, and its use is illustrated with results from the first and second Next-Generation Aircraft Remote Sensing for Validation (NARVAL) field studies. Measurements from the second NARVAL (NARVAL2) are used to highlight the ability of HALO, when configured in this fashion, to characterize not only the distribution of water condensate in the atmosphere, but also its impact on radiant energy transfer and the covarying large-scale meteorological conditions?including the large-scale velocity field and its vertical component. The NARVAL campaigns with HALO demonstrate the potential of airborne cloud observatories to address long-standing riddles in studies of the coupling between clouds and circulation and are helping to motivate a new generation of field studies.
publisherAmerican Meteorological Society
titleA High-Altitude Long-Range Aircraft Configured as a Cloud Observatory: The NARVAL Expeditions
typeJournal Paper
journal volume100
journal issue6
journal titleBulletin of the American Meteorological Society
identifier doi10.1175/BAMS-D-18-0198.1
journal fristpage1061
journal lastpage1077
treeBulletin of the American Meteorological Society:;2019:;volume 100:;issue 006
contenttypeFulltext


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