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    Empirical Analysis of Intraseasonal Climate Variability over the Greater Horn of Africa

    Source: Journal of Climate:;2007:;volume( 020 ):;issue: 023::page 5715
    Author:
    Bowden, Jared H.
    ,
    Semazzi, Fredrick H. M.
    DOI: 10.1175/2007JCLI1587.1
    Publisher: American Meteorological Society
    Abstract: This study examines the intraseasonal climate variability over the Greater Horn of Africa (GHA) during the rainy season of October?December (OND). The investigation is primarily based on empirical orthogonal function (EOF) analysis of the pentad Climate Prediction Center Merged Analysis of Precipitation (CMAP) data for the period 1979?2001. The EOF analysis reveals two dominant modes of intraseasonal variability for the OND season: mixed El Niño?Southern Oscillation?Indian Ocean dipole (ENSO-IOD) and a decadal mode. The leading mode is associated with ENSO?IOD covariability. Case studies of several intraseasonal ENSO?IOD events within the recent decades indicate that during the warm (positive) events pentad rainfall is consistently above normal during the entire season despite fluctuations between pentads. However, case study analyses of negative ENSO?IOD events show that the negative cases are not mirror images of the warm events. The negative events exhibit pronounced wet and dry spells superimposed on the consistent dry anomaly background conditions. There is no large signal regarding the onset for either case, but the withdrawal of the positive (negative) events is anomalously wet (dry). The second mode of variability is associated with a decadal shift in the rainfall with the northern (southern) GHA becoming wetter (drier) in the recent decade. The decadal change in individual pentads can be quite different across the season and has a tendency to manifest itself through extreme events. The analysis underscores the need to exercise caution when applying seasonal-average-based statistics to infer the long-term behavior on subseasonal time scales. Additional analyses further confirm the decadal rainfall shift using four different rainfall datasets. Averaging the datasets to help aid in removing bias of individual datasets shows that, on average, northern (southern) portions of GHA are 29% (19%) wetter (drier) in the recent decade.
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      Empirical Analysis of Intraseasonal Climate Variability over the Greater Horn of Africa

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4206929
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    contributor authorBowden, Jared H.
    contributor authorSemazzi, Fredrick H. M.
    date accessioned2017-06-09T16:19:13Z
    date available2017-06-09T16:19:13Z
    date copyright2007/12/01
    date issued2007
    identifier issn0894-8755
    identifier otherams-65678.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4206929
    description abstractThis study examines the intraseasonal climate variability over the Greater Horn of Africa (GHA) during the rainy season of October?December (OND). The investigation is primarily based on empirical orthogonal function (EOF) analysis of the pentad Climate Prediction Center Merged Analysis of Precipitation (CMAP) data for the period 1979?2001. The EOF analysis reveals two dominant modes of intraseasonal variability for the OND season: mixed El Niño?Southern Oscillation?Indian Ocean dipole (ENSO-IOD) and a decadal mode. The leading mode is associated with ENSO?IOD covariability. Case studies of several intraseasonal ENSO?IOD events within the recent decades indicate that during the warm (positive) events pentad rainfall is consistently above normal during the entire season despite fluctuations between pentads. However, case study analyses of negative ENSO?IOD events show that the negative cases are not mirror images of the warm events. The negative events exhibit pronounced wet and dry spells superimposed on the consistent dry anomaly background conditions. There is no large signal regarding the onset for either case, but the withdrawal of the positive (negative) events is anomalously wet (dry). The second mode of variability is associated with a decadal shift in the rainfall with the northern (southern) GHA becoming wetter (drier) in the recent decade. The decadal change in individual pentads can be quite different across the season and has a tendency to manifest itself through extreme events. The analysis underscores the need to exercise caution when applying seasonal-average-based statistics to infer the long-term behavior on subseasonal time scales. Additional analyses further confirm the decadal rainfall shift using four different rainfall datasets. Averaging the datasets to help aid in removing bias of individual datasets shows that, on average, northern (southern) portions of GHA are 29% (19%) wetter (drier) in the recent decade.
    publisherAmerican Meteorological Society
    titleEmpirical Analysis of Intraseasonal Climate Variability over the Greater Horn of Africa
    typeJournal Paper
    journal volume20
    journal issue23
    journal titleJournal of Climate
    identifier doi10.1175/2007JCLI1587.1
    journal fristpage5715
    journal lastpage5731
    treeJournal of Climate:;2007:;volume( 020 ):;issue: 023
    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
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