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Submonthly scale (7-25 days) ISO is a dominant mode of summer rainfall fluctuation over Bangladesh. In the active (suppressed) ISO phases, a cyclonic (anticyclonic) circulation anomaly develops at the low-level troposphere from northeastern India to Bangladesh, and an anticyclonic (cyclonic) circulation anomaly appears over the Bay of Bengal, accompanied by the enhancement of westerly/southwesterly (easterly/southeasterly) moisture flux anomalies over Bangladesh. The IAV of total summer monsoon rainfall is significantly correlated with that of the rainfall variance, mainly in the submonthly scale, suggesting that the ISO activity controls the IAV of the total summer monsoon rainfall. Moreover, the spatial patterns of atmospheric circulation and convection associated with the ISO and the IAV are quite similar to each other around the monsoon trough, especially from northeastern India to Bangladesh. In wet monsoon years, more frequent strong submonthly scale ISOs and a larger number of rainy days related to the active ISO phase are evident compared with that of dry monsoon years. Climatologically, Bangladesh is one of the most predominant areas of submonthly scale ISO; however, 30-60-day ISO is not prominent. These characteristic features probably allow the submonthly scale ISO to modulate the total seasonal rainfall and the spatial patterns of circulation and convection over and near Bangladesh. Copyright. 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  1. 防災科研関係論文

Characteristic intraseasonal oscillation of rainfall and its effect on interannual variability over Bangladesh during boreal summer

https://nied-repo.bosai.go.jp/records/2739
https://nied-repo.bosai.go.jp/records/2739
1d837fac-021e-466b-8920-a7b60b770d81
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Characteristic intraseasonal oscillation of rainfall and its effect on interannual variability over Bangladesh during boreal summer
言語
言語 eng
著者 Hatsuki Fujinami

× Hatsuki Fujinami

en Hatsuki Fujinami

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Daisuke Hatsuzuka

× Daisuke Hatsuzuka

en Daisuke Hatsuzuka

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Tetsuzo Yasunari

× Tetsuzo Yasunari

en Tetsuzo Yasunari

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Taiichi Hayashi

× Taiichi Hayashi

en Taiichi Hayashi

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Toru Terao

× Toru Terao

en Toru Terao

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Fumie Murata

× Fumie Murata

en Fumie Murata

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Masashi Kiguchi

× Masashi Kiguchi

en Masashi Kiguchi

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Yusuke Yamane

× Yusuke Yamane

en Yusuke Yamane

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Jun Matsumoto

× Jun Matsumoto

en Jun Matsumoto

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Md. Nazrul Islam

× Md. Nazrul Islam

en Md. Nazrul Islam

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Arjumand Habib

× Arjumand Habib

en Arjumand Habib

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抄録
内容記述タイプ Other
内容記述 Intraseasonal oscillation (ISO) of rainfall during the summer monsoon season (June-August) and its plausible effect on interannual variation (IAV) of total summer monsoon rainfall over Bangladesh are examined using daily rainfall data from 25 rain-gauge stations for 20 years (1981-2000). Submonthly scale (7-25 days) ISO is a dominant mode of summer rainfall fluctuation over Bangladesh. In the active (suppressed) ISO phases, a cyclonic (anticyclonic) circulation anomaly develops at the low-level troposphere from northeastern India to Bangladesh, and an anticyclonic (cyclonic) circulation anomaly appears over the Bay of Bengal, accompanied by the enhancement of westerly/southwesterly (easterly/southeasterly) moisture flux anomalies over Bangladesh. The IAV of total summer monsoon rainfall is significantly correlated with that of the rainfall variance, mainly in the submonthly scale, suggesting that the ISO activity controls the IAV of the total summer monsoon rainfall. Moreover, the spatial patterns of atmospheric circulation and convection associated with the ISO and the IAV are quite similar to each other around the monsoon trough, especially from northeastern India to Bangladesh. In wet monsoon years, more frequent strong submonthly scale ISOs and a larger number of rainy days related to the active ISO phase are evident compared with that of dry monsoon years. Climatologically, Bangladesh is one of the most predominant areas of submonthly scale ISO; however, 30-60-day ISO is not prominent. These characteristic features probably allow the submonthly scale ISO to modulate the total seasonal rainfall and the spatial patterns of circulation and convection over and near Bangladesh. Copyright. (C) 2010 Royal Meteorological Society
言語 en
書誌情報 en : International Journal of Climatology

巻 31, 号 8, p. 1192-1204, 発行日 2011-06-30
出版者
言語 en
出版者 Wiley
ISSN
収録物識別子タイプ EISSN
収録物識別子 1097-0088
DOI
関連識別子 10.1002/joc.2146
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