{"_buckets": {"deposit": "5b4c76b8-61e0-4be9-902f-f18b06956127"}, "_deposit": {"id": "11172", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "11172"}, "status": "published"}, "_oai": {"id": "oai:nagoya.repo.nii.ac.jp:00011172"}, "item_12_biblio_info_6": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2008-03-25", "bibliographicIssueDateType": "Issued"}, "bibliographic_titles": [{}]}]}, "item_12_date_granted_64": {"attribute_name": "\u5b66\u4f4d\u6388\u4e0e\u5e74\u6708\u65e5", "attribute_value_mlt": [{"subitem_dategranted": "2008-03-25"}]}, "item_12_description_4": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "The atmospheric water balance over different domains within the South Asian\nMonsoon region has been studied using moisture convergence (C) computed from JRA-\n25, ERA-40 and NCEP/NCAR reanalysis datasets, GPCP precipitation data (P) and\nevaporation (E) as a residual of these two parameters. 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. It is also evident that the structure of\nvariability for early (JJ) and late (AS) summer precipitation is different over south Asian\nMonsoon region. Over northwest India E dominates C on seasonal time scale, but only C\ncontribute to interannual variability of P. Similarly, over central India C dominates E\nduring early summer (JJ) on seasonal timescale, but E contributes higher to P variability\non interannual time scale and during late summer (AS) over central India E dominates C\non seasonal time scale, but C contributes higher to P variability on interannual time scale.\nOver northeast India, C dominates E on seasonal time scale, but only E contributes to\ninterannual variability of P. The importances of land-atmosphere interactions over each\ndomain are discussed. The regionality in the mechanism of precipitation generation and\nits contribution to the all India summer monsoon precipitation variability are also\ndiscussed in detail. The role of evaporation on the interannual variability of precipitation\nis stronger over Bay of Bengal sector and the role of convergence on the interannual\nvariability of precipitation is stronger over Arabian Sea sector.\nThe interannual variability of P, C and E for the northeast monsoon season\n(October to December) over the south Peninsular India and Sri Lanka have also been\nexamined. The spatial and temporal characteristics of P, C and E characteristics have\nproved that over this region, E principally dominates during the entire monsoon months\n(OND). The moisture transport from the Indian Ocean sector modulates the precipitation\nover this region on a year-to-year basis. It has been noted that the positive northeast\nmonsoon rainfall is associated with El-Nino coupled with positive Indian Ocean Dipole\nmode, but negative northeast monsoon rainfall is weakly associated only with La-Nina\ncondition. The role of land-atmospheric interaction over the region in modulating the\ninterannual variability of hydrological cycle has also been discussed.", "subitem_description_type": "Abstract"}]}, "item_12_description_5": {"attribute_name": "\u5185\u5bb9\u8a18\u8ff0", "attribute_value_mlt": [{"subitem_description": "\u540d\u53e4\u5c4b\u5927\u5b66\u535a\u58eb\u5b66\u4f4d\u8ad6\u6587 \u5b66\u4f4d\u306e\u7a2e\u985e:\u535a\u58eb(\u7406\u5b66) (\u8ab2\u7a0b) \u5b66\u4f4d\u6388\u4e0e\u5e74\u6708\u65e5:\u5e73\u621020\u5e743\u670825\u65e5", "subitem_description_type": "Other"}]}, "item_12_dissertation_number_65": {"attribute_name": "\u5b66\u4f4d\u6388\u4e0e\u756a\u53f7", "attribute_value_mlt": [{"subitem_dissertationnumber": "13901\u7532\u7b2c7824\u53f7"}]}, "item_12_identifier_60": {"attribute_name": "URI", "attribute_value_mlt": [{"subitem_identifier_type": "HDL", "subitem_identifier_uri": "http://hdl.handle.net/2237/13043"}]}, "item_12_select_15": {"attribute_name": "\u8457\u8005\u7248\u30d5\u30e9\u30b0", "attribute_value_mlt": [{"subitem_select_item": "publisher"}]}, "item_12_text_14": {"attribute_name": "\u30d5\u30a9\u30fc\u30de\u30c3\u30c8", "attribute_value_mlt": [{"subitem_text_value": "application/pdf"}]}, "item_12_text_63": {"attribute_name": "\u5b66\u4f4d\u6388\u4e0e\u5e74\u5ea6", "attribute_value_mlt": [{"subitem_text_value": "2007"}]}, "item_creator": {"attribute_name": "\u8457\u8005", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Prasanna, Venkatraman"}], "nameIdentifiers": [{"nameIdentifier": "33802", "nameIdentifierScheme": "WEKO"}]}]}, "item_files": {"attribute_name": "\u30d5\u30a1\u30a4\u30eb\u60c5\u5831", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2018-02-20"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "Prasanna.pdf", "filesize": [{"value": "3.4 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 3400000.0, "url": {"label": "Prasanna.pdf", "url": "https://nagoya.repo.nii.ac.jp/record/11172/files/Prasanna.pdf"}, "version_id": "fb355bc1-bf47-4ec7-9b1c-fac9f86fa6c2"}]}, "item_language": {"attribute_name": "\u8a00\u8a9e", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_resource_type": {"attribute_name": "\u8cc7\u6e90\u30bf\u30a4\u30d7", "attribute_value_mlt": [{"resourcetype": "thesis", "resourceuri": "http://purl.org/coar/resource_type/c_46ec"}]}, "item_title": "STUDY OF ATMOSPHERIC WATER BALANCE OVER SOUTH ASIAN MONSOON REGION", "item_titles": {"attribute_name": "\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_title": "STUDY OF ATMOSPHERIC WATER BALANCE OVER SOUTH ASIAN MONSOON REGION"}]}, "item_type_id": "12", "owner": "1", "path": ["488/641/642"], "permalink_uri": "http://hdl.handle.net/2237/13043", "pubdate": {"attribute_name": "\u516c\u958b\u65e5", "attribute_name_i18n": "\u516c\u958b\u65e5", "attribute_value": "2010-03-31"}, "publish_date": "2010-03-31", "publish_status": "0", "recid": "11172", "relation": {}, "relation_version_is_last": true, "title": ["STUDY OF ATMOSPHERIC WATER BALANCE OVER SOUTH ASIAN MONSOON REGION"], "weko_shared_id": null}