{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1360855570676861440.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1017/cbo9780511781247"}}],"dc:title":[{"@value":"River Discharge to the Coastal Ocean"}],"dcterms:alternative":[{"@value":"A Global Synthesis"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Rivers provide the primary link between land and sea. Utilizing the world's largest database, this book presents a detailed analysis and synthesis of the processes affecting fluvial discharge of water, sediment and dissolved solids. It also discusses the ways in which climatic variation, episodic events and anthropogenic activities – past, present and future – affect the quantity and quality of river discharge. The book contains more than 165 figures – many in full color – including global and regional maps. An extensive appendix presents the 1534-river database as a series of 44 tables that provide quantitative data regarding the discharge of water, sediment and dissolved solids. The complete database is also presented within a GIS-based package available online at www.cambridge.org/milliman. Now available in paperback, reprinted with corrections, this is an invaluable resource for researchers, professionals and graduate students in hydrology, oceanography, geology, geomorphology and environmental policy.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380855570676861441","@type":"Researcher","foaf:name":[{"@value":"John D. Milliman"}]},{"@id":"https://cir.nii.ac.jp/crid/1380855570676861440","@type":"Researcher","foaf:name":[{"@value":"Katherine L. Farnsworth"}]}],"publication":{"publicationIdentifier":[{"@type":"ISBN","@value":"9780521879873"},{"@type":"ISBN","@value":"9780511781247"},{"@type":"ISBN","@value":"9781107612181"}],"dc:publisher":[{"@value":"Cambridge University Press"}],"prism:publicationDate":"2011-02-24"},"reviewed":"false","dc:rights":["https://www.cambridge.org/core/terms"],"createdAt":"2011-05-04","modifiedAt":"2022-10-11","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050003824926010880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Super typhoon induced high silica export from Arakawa River, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229805610368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Distinct control mechanism of fine‐grained sediments from <scp>Y</scp>ellow <scp>R</scp>iver and <scp>K</scp>yushu supply in the northern <scp>O</scp>kinawa <scp>T</scp>rough since the last glacial"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004235822176128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sediment distribution and depositional processes along the fluvial to marine transition zone of the Mekong River delta, Vietnam"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004236253563520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sedimentology of Late Holocene fluvial levee and point-bar deposits from the Cambodian tract of the Mekong River"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168738628736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Late Holocene stratigraphic evolution and sedimentary facies of an active to abandoned tide‐dominated distributary channel and its mouth bar"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168749561344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Distribution of Holocene Marine Mud and Its Relation to Damage from the 1923 Earthquake Disaster in the Tokyo Metropolitan Area, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285713317807360","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tide- and River-Generated Mud Pebbles from the Fluvial To Marine Transition Zone of the Mekong River Delta, Vietnam"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643714716928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Abandonment and rapid infilling of a tide-dominated distributary channel at 0.7 ka in the Mekong River Delta"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643725364736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Recycling of clastics in coastal areas inferred from quantitative analysis of reworked radiocarbon samples"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580232397160832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dissolved Lead (Pb) Concentrations and Pb Isotope Ratios Along the East China Sea and Kuroshio Transect—Evidence for Isopycnal Transport and Particle Exchange"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848660752245888","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Millennial‐scale stratigraphy of a tide‐dominated incised valley during the last 14 kyr: Spatial and quantitative reconstruction in the Tokyo Lowland, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206241252864","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Depositional process of an estuary mouth shoal identified in the Alluvium of the Tokyo Lowland along the Tokyo Bay, central Japan"},{"@language":"ja","@value":"東京低地臨海部の沖積層にみられる湾口砂州の形成機構"},{"@language":"ja-Kana","@value":"トウキョウ テイチ リンカイブ ノ チュウセキソウ ニ ミラレル ワンコウ サス ノ ケイセイ キコウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206497039360","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Coastal depositional systems and sea-level change"},{"@language":"ja","@value":"沿岸域の堆積システムと海水準変動"},{"@value":"2009年度日本第四紀学会学術賞受賞記念論文 沿岸域の堆積システムと海水準変動"},{"@language":"ja-Kana","@value":"2009ネンド ニホン ダイ4キ ガッカイ ガクジュツショウ ジュショウ キネン ロンブン エンガンイキ ノ タイセキ システム ト ウミ スイジュン ヘンドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288129600896","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Formation mechanisms of the post-LGM incised-valley fills beneath the Tokyo and Nakagawa lowlands, central Japan"},{"@language":"ja","@value":"東京低地と中川低地における沖積層の形成機構"},{"@language":"ja-Kana","@value":"トウキョウ テイチ ト ナカガワ テイチ ニ オケル チュウセキソウ ノ ケイセイ キコウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390285300181384704","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"東京低地南部における沖積層の基盤地形"},{"@language":"en","@value":"Incised-valley topography formed into the Last Glacial Maximum beneath the southern area of the Tokyo Lowland, central Japan"},{"@language":"ja-Kana","@value":"トウキョウ テイチ ナンブ ニ オケル チュウセキソウ ノ キバン チケイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390858131663515904","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Denudation Rates since the Middle Holocene Based on Sediment Storage in the Kiso-Nagara-Ibi and Shonai, and Yahagi River Basins, Central Japan"},{"@language":"ja","@value":"木曽三川・庄内川および矢作川流域における堆積土砂量に基づく完新世中期以降の侵食速度"},{"@language":"ja-Kana","@value":"キソ サンガワ ・ ショウナイガワ オヨビ ヤハギガワ リュウイキ ニ オケル タイセキ ドシャリョウ ニ モトズク カンシン セイ チュウキ イコウ ノ シンショク ソクド"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367075061120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Integrated Pliocene-Pleistocene magnetostratigraphy and tephrostratigraphy of deep-sea sediments at IODP Site U1424 (Yamato Basin, Japan Sea)"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842051771520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Development of a global sediment dynamics model"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792008805120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Formation of undulating topography and gravel beds at the bases of incised valleys : Last Glacial Maximum examples beneath the lowlands facing Tokyo Bay"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1017/cbo9780511781247"},{"@type":"CROSSREF","@value":"10.1002/2016gc006764_references_DOI_3Nspsw7v8IEDt5xIuYrSl1E4AOe"},{"@type":"CROSSREF","@value":"10.1111/sed.12489_references_DOI_3Nspsw7v8IEDt5xIuYrSl1E4AOe"},{"@type":"CROSSREF","@value":"10.1144/jgs2017-047_references_DOI_3Nspsw7v8IEDt5xIuYrSl1E4AOe"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2018.0021_references_DOI_3Nspsw7v8IEDt5xIuYrSl1E4AOe"},{"@type":"CROSSREF","@value":"10.1111/sed.12940_references_DOI_3Nspsw7v8IEDt5xIuYrSl1E4AOe"},{"@type":"CROSSREF","@value":"10.1007/s11356-020-09634-y_references_DOI_3Nspsw7v8IEDt5xIuYrSl1E4AOe"},{"@type":"CROSSREF","@value":"10.3390/geosciences11070272_references_DOI_3Nspsw7v8IEDt5xIuYrSl1E4AOe"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2011.0020_references_DOI_3Nspsw7v8IEDt5xIuYrSl1E4AOe"},{"@type":"CROSSREF","@value":"10.1186/s40645-020-00368-6_references_DOI_3Nspsw7v8IEDt5xIuYrSl1E4AOe"},{"@type":"CROSSREF","@value":"10.1038/s41598-021-90268-6_references_DOI_3Nspsw7v8IEDt5xIuYrSl1E4AOe"},{"@type":"CROSSREF","@value":"10.4157/grj.94.187_references_DOI_3Nspsw7v8IEDt5xIuYrSl1E4AOe"},{"@type":"CROSSREF","@value":"10.9795/bullgsj.71.201_references_DOI_3Nspsw7v8IEDt5xIuYrSl1E4AOe"},{"@type":"CROSSREF","@value":"10.1038/s41598-021-04660-3_references_DOI_3Nspsw7v8IEDt5xIuYrSl1E4AOe"},{"@type":"CROSSREF","@value":"10.4116/jaqua.50.95_references_DOI_3Nspsw7v8IEDt5xIuYrSl1E4AOe"},{"@type":"CROSSREF","@value":"10.2110/jsr.2018.54_references_DOI_3Nspsw7v8IEDt5xIuYrSl1E4AOe"},{"@type":"CROSSREF","@value":"10.1029/2022jc019423_references_DOI_3Nspsw7v8IEDt5xIuYrSl1E4AOe"},{"@type":"CROSSREF","@value":"10.1111/sed.12204_references_DOI_3Nspsw7v8IEDt5xIuYrSl1E4AOe"},{"@type":"CROSSREF","@value":"10.1186/s40645-020-00373-9_references_DOI_3Nspsw7v8IEDt5xIuYrSl1E4AOe"},{"@type":"CROSSREF","@value":"10.1186/s40645-021-00411-0_references_DOI_3Nspsw7v8IEDt5xIuYrSl1E4AOe"}]}