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The seasonal climatology of P, C,\nand E for the selected regions shows generally large contribution of E to P. The interannual\ncharacteristics of P, C and E over selected key domains with in the South Asian\nMonsoon region have also been examined for both early (JJ) and late summer (AS)\nmonsoon periods from 1979 to 2000. The spatial and temporal characteristics of the\nhydrological cycle and the contribution of E and C to P are discussed in detail. One\nimportant aspect on seasonal time scale is that from dry regions of Northwest to Central\nand to the wettest Northeast regions, the monthly variations of E or C are large during the\nmonsoon months specific to that region. However, the interannual variability of P over\neach domain is not necessarily be influenced by the same criteria like C or E, which\ninfluences the mean seasonal precipitation. 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  1. D300 大学院環境学研究科
  2. D300d 学位論文
  3. 博士論文(環境博・論環境博)

STUDY OF ATMOSPHERIC WATER BALANCE OVER SOUTH ASIAN MONSOON REGION

http://hdl.handle.net/2237/13043
da0bab3b-8cda-4469-b2cd-ca29a5a126c6
名前 / ファイル ライセンス アクション
Prasanna.pdf Prasanna.pdf (3.4 MB)
Item type 学位論文 / Thesis or Dissertation(1)
公開日 2010-03-31
タイトル
タイトル STUDY OF ATMOSPHERIC WATER BALANCE OVER SOUTH ASIAN MONSOON REGION
著者 Prasanna, Venkatraman

× Prasanna, Venkatraman

WEKO 33802

Prasanna, Venkatraman

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内容記述 The atmospheric water balance over different domains within the South Asian
Monsoon region has been studied using moisture convergence (C) computed from JRA-
25, ERA-40 and NCEP/NCAR reanalysis datasets, GPCP precipitation data (P) and
evaporation (E) as a residual of these two parameters. The seasonal climatology of P, C,
and E for the selected regions shows generally large contribution of E to P. The interannual
characteristics of P, C and E over selected key domains with in the South Asian
Monsoon region have also been examined for both early (JJ) and late summer (AS)
monsoon periods from 1979 to 2000. The spatial and temporal characteristics of the
hydrological cycle and the contribution of E and C to P are discussed in detail. One
important aspect on seasonal time scale is that from dry regions of Northwest to Central
and to the wettest Northeast regions, the monthly variations of E or C are large during the
monsoon months specific to that region. However, the interannual variability of P over
each domain is not necessarily be influenced by the same criteria like C or E, which
influences the mean seasonal precipitation. It is also evident that the structure of
variability for early (JJ) and late (AS) summer precipitation is different over south Asian
Monsoon region. Over northwest India E dominates C on seasonal time scale, but only C
contribute to interannual variability of P. Similarly, over central India C dominates E
during early summer (JJ) on seasonal timescale, but E contributes higher to P variability
on interannual time scale and during late summer (AS) over central India E dominates C
on seasonal time scale, but C contributes higher to P variability on interannual time scale.
Over northeast India, C dominates E on seasonal time scale, but only E contributes to
interannual variability of P. The importances of land-atmosphere interactions over each
domain are discussed. The regionality in the mechanism of precipitation generation and
its contribution to the all India summer monsoon precipitation variability are also
discussed in detail. The role of evaporation on the interannual variability of precipitation
is stronger over Bay of Bengal sector and the role of convergence on the interannual
variability of precipitation is stronger over Arabian Sea sector.
The interannual variability of P, C and E for the northeast monsoon season
(October to December) over the south Peninsular India and Sri Lanka have also been
examined. The spatial and temporal characteristics of P, C and E characteristics have
proved that over this region, E principally dominates during the entire monsoon months
(OND). The moisture transport from the Indian Ocean sector modulates the precipitation
over this region on a year-to-year basis. It has been noted that the positive northeast
monsoon rainfall is associated with El-Nino coupled with positive Indian Ocean Dipole
mode, but negative northeast monsoon rainfall is weakly associated only with La-Nina
condition. The role of land-atmospheric interaction over the region in modulating the
interannual variability of hydrological cycle has also been discussed.
内容記述タイプ Abstract
内容記述
内容記述 名古屋大学博士学位論文 学位の種類:博士(理学) (課程) 学位授与年月日:平成20年3月25日
内容記述タイプ Other
言語
言語 eng
資源タイプ
資源 http://purl.org/coar/resource_type/c_46ec
タイプ thesis
書誌情報 発行日 2008-03-25
学位授与年度
学位授与年度 2007
学位授与年月日
学位授与年月日 2008-03-25
学位授与番号
学位授与番号 13901甲第7824号
フォーマット
application/pdf
著者版フラグ
値 publisher
URI
識別子 http://hdl.handle.net/2237/13043
識別子タイプ HDL
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