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    Atmospheric Climate Change Detection by Radio Occultation Data Using a Fingerprinting Method

    Source: Journal of Climate:;2011:;volume( 024 ):;issue: 020::page 5275
    Author:
    Lackner, Bettina C.
    ,
    Steiner, Andrea K.
    ,
    Hegerl, Gabriele C.
    ,
    Kirchengast, Gottfried
    DOI: 10.1175/2011JCLI3966.1
    Publisher: American Meteorological Society
    Abstract: he detection of climate change signals in rather short satellite datasets is a challenging task in climate research and requires high-quality data with good error characterization. Global Navigation Satellite System (GNSS) radio occultation (RO) provides a novel record of high-quality measurements of atmospheric parameters of the upper-troposphere?lower-stratosphere (UTLS) region. Because of characteristics such as long-term stability, self calibration, and a very good height resolution, RO data are well suited to investigate atmospheric climate change. This study describes the signals of ENSO and the quasi-biennial oscillation (QBO) in the data and investigates whether the data already show evidence of a forced climate change signal, using an optimal-fingerprint technique. RO refractivity, geopotential height, and temperature within two trend periods (1995?2010 intermittently and 2001?10 continuously) are investigated. The data show that an emerging climate change signal consistent with the projections of three global climate models from the Coupled Model Intercomparison Project cycle 3 (CMIP3) archive is detected for geopotential height of pressure levels at a 90% confidence level both for the intermittent and continuous period, for the latter so far in a broad 50°S?50°N band only. Such UTLS geopotential height changes reflect an overall tropospheric warming. 90% confidence is not achieved for the temperature record when only large-scale aspects of the pattern are resolved. When resolving smaller-scale aspects, RO temperature trends appear stronger than GCM-projected trends, the difference stemming mainly from the tropical lower stratosphere, allowing for climate change detection at a 95% confidence level. Overall, an emerging trend signal is thus detected in the RO climate record, which is expected to increase further in significance as the record grows over the coming years. Small natural changes during the period suggest that the detected change is mainly caused by anthropogenic influence on climate.
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      Atmospheric Climate Change Detection by Radio Occultation Data Using a Fingerprinting Method

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4213774
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    contributor authorLackner, Bettina C.
    contributor authorSteiner, Andrea K.
    contributor authorHegerl, Gabriele C.
    contributor authorKirchengast, Gottfried
    date accessioned2017-06-09T16:39:58Z
    date available2017-06-09T16:39:58Z
    date copyright2011/10/01
    date issued2011
    identifier issn0894-8755
    identifier otherams-71838.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4213774
    description abstracthe detection of climate change signals in rather short satellite datasets is a challenging task in climate research and requires high-quality data with good error characterization. Global Navigation Satellite System (GNSS) radio occultation (RO) provides a novel record of high-quality measurements of atmospheric parameters of the upper-troposphere?lower-stratosphere (UTLS) region. Because of characteristics such as long-term stability, self calibration, and a very good height resolution, RO data are well suited to investigate atmospheric climate change. This study describes the signals of ENSO and the quasi-biennial oscillation (QBO) in the data and investigates whether the data already show evidence of a forced climate change signal, using an optimal-fingerprint technique. RO refractivity, geopotential height, and temperature within two trend periods (1995?2010 intermittently and 2001?10 continuously) are investigated. The data show that an emerging climate change signal consistent with the projections of three global climate models from the Coupled Model Intercomparison Project cycle 3 (CMIP3) archive is detected for geopotential height of pressure levels at a 90% confidence level both for the intermittent and continuous period, for the latter so far in a broad 50°S?50°N band only. Such UTLS geopotential height changes reflect an overall tropospheric warming. 90% confidence is not achieved for the temperature record when only large-scale aspects of the pattern are resolved. When resolving smaller-scale aspects, RO temperature trends appear stronger than GCM-projected trends, the difference stemming mainly from the tropical lower stratosphere, allowing for climate change detection at a 95% confidence level. Overall, an emerging trend signal is thus detected in the RO climate record, which is expected to increase further in significance as the record grows over the coming years. Small natural changes during the period suggest that the detected change is mainly caused by anthropogenic influence on climate.
    publisherAmerican Meteorological Society
    titleAtmospheric Climate Change Detection by Radio Occultation Data Using a Fingerprinting Method
    typeJournal Paper
    journal volume24
    journal issue20
    journal titleJournal of Climate
    identifier doi10.1175/2011JCLI3966.1
    journal fristpage5275
    journal lastpage5291
    treeJournal of Climate:;2011:;volume( 024 ):;issue: 020
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian