Global coastal hazards from future sea level rise
Identifieur interne : 001110 ( Istex/Corpus ); précédent : 001109; suivant : 001111Global coastal hazards from future sea level rise
Auteurs : Vivien GornitzSource :
- Palaeogeography, Palaeoclimatology, Palaeoecology [ 0031-0182 ] ; 1991.
Abstract
A rise of sea level between 0.3 and 0.9 m by the end of the next century, caused by predicted greenhouse climate warming, would endanger human populations, cities, ports, and wetlands in low-lying coastal areas, through inundation, erosion and salinization. The consequences of a global sea level rise would be spatially non-uniform because of local or regional vertical crustal movements, differential resistance to erosion, varying wave climates, and changeable longshore currents.Although many factors can influence sea level, leading to a noisy record, various studies utilizing tide-gauge data find an average global rate of sea level rise of 1–2 mm/yr, over the last 100 years. This trend is part of a general rise over the last 300 years, since the low point of the Little Ice Age. Sea level rise may accelerate 3–8 times over present rates, within the next century.The permanently inundated coastal zone would extend to a depth equivalent to the vertical rise in sea level. Major river deltas, coastal wetlands and coral islands would be most affected. Episodic flooding by storm waves and surges would penetrate even farther inland. Beach and cliff erosion will be accentuated. Saltwater penetration into coastal aquifers and estuaries could contaminate urban water supplies and affect agricultural production.Research on relative risks and impacts of sea level rise on specific localities is still at an early stage. Development of a global coastal hazards data base, intended to provide an overview of the relative vulnerabilities of the world's coastlines, is described in this paper. To date, information on seven variables, associated with inundation and erosion hazards, has been compiled for the U.S., and parts of Canada and Mexico. A coastal vulnerability index (CVI) has been designed to flag high risk coastal segments. Preliminary results are presented for the eastern United States, as a test case.
Url:
DOI: 10.1016/0031-0182(91)90173-O
Links to Exploration step
ISTEX:F3A148B34877B996E99A66026F4E183CE1654A53Le document en format XML
<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title>Global coastal hazards from future sea level rise</title><author><name sortKey="Gornitz, Vivien" sort="Gornitz, Vivien" uniqKey="Gornitz V" first="Vivien" last="Gornitz">Vivien Gornitz</name><affiliation><mods:affiliation>NASA GSFC Institute for Space Studies and Columbia University, New York, NY 10025, USA</mods:affiliation></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:F3A148B34877B996E99A66026F4E183CE1654A53</idno><date when="1991" year="1991">1991</date><idno type="doi">10.1016/0031-0182(91)90173-O</idno><idno type="url">https://api.istex.fr/document/F3A148B34877B996E99A66026F4E183CE1654A53/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">001110</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">001110</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a">Global coastal hazards from future sea level rise</title><author><name sortKey="Gornitz, Vivien" sort="Gornitz, Vivien" uniqKey="Gornitz V" first="Vivien" last="Gornitz">Vivien Gornitz</name><affiliation><mods:affiliation>NASA GSFC Institute for Space Studies and Columbia University, New York, NY 10025, USA</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Palaeogeography, Palaeoclimatology, Palaeoecology</title><title level="j" type="abbrev">PALAEO</title><idno type="ISSN">0031-0182</idno><imprint><publisher>ELSEVIER</publisher><date type="published" when="1991">1991</date><biblScope unit="volume">89</biblScope><biblScope unit="issue">4</biblScope><biblScope unit="page" from="379">379</biblScope><biblScope unit="page" to="398">398</biblScope></imprint><idno type="ISSN">0031-0182</idno></series><idno type="istex">F3A148B34877B996E99A66026F4E183CE1654A53</idno><idno type="DOI">10.1016/0031-0182(91)90173-O</idno><idno type="PII">0031-0182(91)90173-O</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0031-0182</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">A rise of sea level between 0.3 and 0.9 m by the end of the next century, caused by predicted greenhouse climate warming, would endanger human populations, cities, ports, and wetlands in low-lying coastal areas, through inundation, erosion and salinization. The consequences of a global sea level rise would be spatially non-uniform because of local or regional vertical crustal movements, differential resistance to erosion, varying wave climates, and changeable longshore currents.Although many factors can influence sea level, leading to a noisy record, various studies utilizing tide-gauge data find an average global rate of sea level rise of 1–2 mm/yr, over the last 100 years. This trend is part of a general rise over the last 300 years, since the low point of the Little Ice Age. Sea level rise may accelerate 3–8 times over present rates, within the next century.The permanently inundated coastal zone would extend to a depth equivalent to the vertical rise in sea level. Major river deltas, coastal wetlands and coral islands would be most affected. Episodic flooding by storm waves and surges would penetrate even farther inland. Beach and cliff erosion will be accentuated. Saltwater penetration into coastal aquifers and estuaries could contaminate urban water supplies and affect agricultural production.Research on relative risks and impacts of sea level rise on specific localities is still at an early stage. Development of a global coastal hazards data base, intended to provide an overview of the relative vulnerabilities of the world's coastlines, is described in this paper. To date, information on seven variables, associated with inundation and erosion hazards, has been compiled for the U.S., and parts of Canada and Mexico. A coastal vulnerability index (CVI) has been designed to flag high risk coastal segments. Preliminary results are presented for the eastern United States, as a test case.</div></front></TEI><istex><corpusName>elsevier</corpusName><author><json:item><name>Vivien Gornitz</name><affiliations><json:string>NASA GSFC Institute for Space Studies and Columbia University, New York, NY 10025, USA</json:string></affiliations></json:item></author><language><json:string>eng</json:string></language><originalGenre><json:string>Full-length article</json:string></originalGenre><abstract>A rise of sea level between 0.3 and 0.9 m by the end of the next century, caused by predicted greenhouse climate warming, would endanger human populations, cities, ports, and wetlands in low-lying coastal areas, through inundation, erosion and salinization. The consequences of a global sea level rise would be spatially non-uniform because of local or regional vertical crustal movements, differential resistance to erosion, varying wave climates, and changeable longshore currents.Although many factors can influence sea level, leading to a noisy record, various studies utilizing tide-gauge data find an average global rate of sea level rise of 1–2 mm/yr, over the last 100 years. This trend is part of a general rise over the last 300 years, since the low point of the Little Ice Age. Sea level rise may accelerate 3–8 times over present rates, within the next century.The permanently inundated coastal zone would extend to a depth equivalent to the vertical rise in sea level. Major river deltas, coastal wetlands and coral islands would be most affected. Episodic flooding by storm waves and surges would penetrate even farther inland. Beach and cliff erosion will be accentuated. Saltwater penetration into coastal aquifers and estuaries could contaminate urban water supplies and affect agricultural production.Research on relative risks and impacts of sea level rise on specific localities is still at an early stage. Development of a global coastal hazards data base, intended to provide an overview of the relative vulnerabilities of the world's coastlines, is described in this paper. To date, information on seven variables, associated with inundation and erosion hazards, has been compiled for the U.S., and parts of Canada and Mexico. A coastal vulnerability index (CVI) has been designed to flag high risk coastal segments. Preliminary results are presented for the eastern United States, as a test case.</abstract><qualityIndicators><score>8</score><pdfVersion>1.2</pdfVersion><pdfPageSize>576 x 764 pts</pdfPageSize><refBibsNative>true</refBibsNative><keywordCount>0</keywordCount><abstractCharCount>1920</abstractCharCount><pdfWordCount>11194</pdfWordCount><pdfCharCount>58426</pdfCharCount><pdfPageCount>20</pdfPageCount><abstractWordCount>299</abstractWordCount></qualityIndicators><title>Global coastal hazards from future sea level rise</title><pii><json:string>0031-0182(91)90173-O</json:string></pii><genre><json:string>research-article</json:string></genre><serie><editor><json:item><name>J.G. Titus</name></json:item></editor><pages><last>149</last><first>87</first></pages><language><json:string>unknown</json:string></language><title>Greenhouse Effect, Sea Level Rise and Coastal Wetlands</title></serie><host><volume>89</volume><pii><json:string>S0031-0182(00)X0373-2</json:string></pii><pages><last>398</last><first>379</first></pages><issn><json:string>0031-0182</json:string></issn><issue>4</issue><genre><json:string>journal</json:string></genre><language><json:string>unknown</json:string></language><title>Palaeogeography, Palaeoclimatology, Palaeoecology</title><publicationDate>1991</publicationDate></host><categories><wos><json:string>science</json:string><json:string>paleontology</json:string><json:string>geosciences, multidisciplinary</json:string><json:string>geography, physical</json:string></wos><scienceMetrix><json:string>natural sciences</json:string><json:string>earth & environmental sciences</json:string><json:string>paleontology</json:string></scienceMetrix></categories><publicationDate>1991</publicationDate><copyrightDate>1991</copyrightDate><doi><json:string>10.1016/0031-0182(91)90173-O</json:string></doi><id>F3A148B34877B996E99A66026F4E183CE1654A53</id><score>0.03916354</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/F3A148B34877B996E99A66026F4E183CE1654A53/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/F3A148B34877B996E99A66026F4E183CE1654A53/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/F3A148B34877B996E99A66026F4E183CE1654A53/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a">Global coastal hazards from future sea level rise</title></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>ELSEVIER</publisher><availability><p>ELSEVIER</p></availability><date>1991</date></publicationStmt><notesStmt><note type="content">Section title: Research paper</note></notesStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a">Global coastal hazards from future sea level rise</title><author xml:id="author-1"><persName><forename type="first">Vivien</forename><surname>Gornitz</surname></persName><affiliation>NASA GSFC Institute for Space Studies and Columbia University, New York, NY 10025, USA</affiliation></author></analytic><monogr><title level="j">Palaeogeography, Palaeoclimatology, Palaeoecology</title><title level="j" type="abbrev">PALAEO</title><idno type="pISSN">0031-0182</idno><idno type="PII">S0031-0182(00)X0373-2</idno><imprint><publisher>ELSEVIER</publisher><date type="published" when="1991"></date><biblScope unit="volume">89</biblScope><biblScope unit="issue">4</biblScope><biblScope unit="page" from="379">379</biblScope><biblScope unit="page" to="398">398</biblScope></imprint></monogr><idno type="istex">F3A148B34877B996E99A66026F4E183CE1654A53</idno><idno type="DOI">10.1016/0031-0182(91)90173-O</idno><idno type="PII">0031-0182(91)90173-O</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1991</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>A rise of sea level between 0.3 and 0.9 m by the end of the next century, caused by predicted greenhouse climate warming, would endanger human populations, cities, ports, and wetlands in low-lying coastal areas, through inundation, erosion and salinization. The consequences of a global sea level rise would be spatially non-uniform because of local or regional vertical crustal movements, differential resistance to erosion, varying wave climates, and changeable longshore currents.Although many factors can influence sea level, leading to a noisy record, various studies utilizing tide-gauge data find an average global rate of sea level rise of 1–2 mm/yr, over the last 100 years. This trend is part of a general rise over the last 300 years, since the low point of the Little Ice Age. Sea level rise may accelerate 3–8 times over present rates, within the next century.The permanently inundated coastal zone would extend to a depth equivalent to the vertical rise in sea level. Major river deltas, coastal wetlands and coral islands would be most affected. Episodic flooding by storm waves and surges would penetrate even farther inland. Beach and cliff erosion will be accentuated. Saltwater penetration into coastal aquifers and estuaries could contaminate urban water supplies and affect agricultural production.Research on relative risks and impacts of sea level rise on specific localities is still at an early stage. Development of a global coastal hazards data base, intended to provide an overview of the relative vulnerabilities of the world's coastlines, is described in this paper. To date, information on seven variables, associated with inundation and erosion hazards, has been compiled for the U.S., and parts of Canada and Mexico. A coastal vulnerability index (CVI) has been designed to flag high risk coastal segments. Preliminary results are presented for the eastern United States, as a test case.</p></abstract></profileDesc><revisionDesc><change when="1991">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/F3A148B34877B996E99A66026F4E183CE1654A53/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Elsevier, elements deleted: tail"><istex:xmlDeclaration>version="1.0" encoding="UTF-8" </istex:xmlDeclaration><istex:docType PUBLIC="-//ES//DTD journal article DTD version 4.5.2//EN//XML" URI="art452.dtd" name="istex:docType"></istex:docType><istex:document><converted-article version="4.5.2" docsubtype="fla"><item-info><jid>PALAEO</jid><aid>90173</aid><ce:pii>0031-0182(91)90173-O</ce:pii><ce:doi>10.1016/0031-0182(91)90173-O</ce:doi><ce:copyright type="unknown" year="1991"></ce:copyright></item-info><head><ce:dochead><ce:textfn>Research paper</ce:textfn></ce:dochead><ce:title>Global coastal hazards from future sea level rise</ce:title><ce:author-group><ce:author><ce:given-name>Vivien</ce:given-name><ce:surname>Gornitz</ce:surname></ce:author><ce:affiliation><ce:textfn>NASA GSFC Institute for Space Studies and Columbia University, New York, NY 10025, USA</ce:textfn></ce:affiliation></ce:author-group><ce:date-received day="6" month="12" year="1989"></ce:date-received><ce:date-accepted day="7" month="6" year="1990"></ce:date-accepted><ce:abstract><ce:section-title>Abstract</ce:section-title><ce:abstract-sec><ce:simple-para id="SP0005">A rise of sea level between 0.3 and 0.9 m by the end of the next century, caused by predicted greenhouse climate warming, would endanger human populations, cities, ports, and wetlands in low-lying coastal areas, through inundation, erosion and salinization. The consequences of a global sea level rise would be spatially non-uniform because of local or regional vertical crustal movements, differential resistance to erosion, varying wave climates, and changeable longshore currents.</ce:simple-para><ce:simple-para id="SP0010">Although many factors can influence sea level, leading to a noisy record, various studies utilizing tide-gauge data find an average global rate of sea level rise of 1–2 mm/yr, over the last 100 years. This trend is part of a general rise over the last 300 years, since the low point of the Little Ice Age. Sea level rise may accelerate 3–8 times over present rates, within the next century.</ce:simple-para><ce:simple-para id="SP0015">The permanently inundated coastal zone would extend to a depth equivalent to the vertical rise in sea level. Major river deltas, coastal wetlands and coral islands would be most affected. Episodic flooding by storm waves and surges would penetrate even farther inland. Beach and cliff erosion will be accentuated. Saltwater penetration into coastal aquifers and estuaries could contaminate urban water supplies and affect agricultural production.</ce:simple-para><ce:simple-para id="SP0020">Research on relative risks and impacts of sea level rise on specific localities is still at an early stage. Development of a global coastal hazards data base, intended to provide an overview of the relative vulnerabilities of the world's coastlines, is described in this paper. To date, information on seven variables, associated with inundation and erosion hazards, has been compiled for the U.S., and parts of Canada and Mexico. A coastal vulnerability index (CVI) has been designed to flag high risk coastal segments. Preliminary results are presented for the eastern United States, as a test case.</ce:simple-para></ce:abstract-sec></ce:abstract></head></converted-article></istex:document></istex:metadataXml><mods version="3.6"><titleInfo><title>Global coastal hazards from future sea level rise</title></titleInfo><titleInfo type="alternative" contentType="CDATA"><title>Global coastal hazards from future sea level rise</title></titleInfo><name type="personal"><namePart type="given">Vivien</namePart><namePart type="family">Gornitz</namePart><affiliation>NASA GSFC Institute for Space Studies and Columbia University, New York, NY 10025, USA</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="research-article" displayLabel="Full-length article"></genre><originInfo><publisher>ELSEVIER</publisher><dateIssued encoding="w3cdtf">1991</dateIssued><copyrightDate encoding="w3cdtf">1991</copyrightDate></originInfo><language><languageTerm type="code" authority="iso639-2b">eng</languageTerm><languageTerm type="code" authority="rfc3066">en</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType></physicalDescription><abstract lang="en">A rise of sea level between 0.3 and 0.9 m by the end of the next century, caused by predicted greenhouse climate warming, would endanger human populations, cities, ports, and wetlands in low-lying coastal areas, through inundation, erosion and salinization. The consequences of a global sea level rise would be spatially non-uniform because of local or regional vertical crustal movements, differential resistance to erosion, varying wave climates, and changeable longshore currents.Although many factors can influence sea level, leading to a noisy record, various studies utilizing tide-gauge data find an average global rate of sea level rise of 1–2 mm/yr, over the last 100 years. This trend is part of a general rise over the last 300 years, since the low point of the Little Ice Age. Sea level rise may accelerate 3–8 times over present rates, within the next century.The permanently inundated coastal zone would extend to a depth equivalent to the vertical rise in sea level. Major river deltas, coastal wetlands and coral islands would be most affected. Episodic flooding by storm waves and surges would penetrate even farther inland. Beach and cliff erosion will be accentuated. Saltwater penetration into coastal aquifers and estuaries could contaminate urban water supplies and affect agricultural production.Research on relative risks and impacts of sea level rise on specific localities is still at an early stage. Development of a global coastal hazards data base, intended to provide an overview of the relative vulnerabilities of the world's coastlines, is described in this paper. To date, information on seven variables, associated with inundation and erosion hazards, has been compiled for the U.S., and parts of Canada and Mexico. A coastal vulnerability index (CVI) has been designed to flag high risk coastal segments. Preliminary results are presented for the eastern United States, as a test case.</abstract><note type="content">Section title: Research paper</note><relatedItem type="host"><titleInfo><title>Palaeogeography, Palaeoclimatology, Palaeoecology</title></titleInfo><titleInfo type="abbreviated"><title>PALAEO</title></titleInfo><genre type="journal">journal</genre><originInfo><dateIssued encoding="w3cdtf">199103</dateIssued></originInfo><identifier type="ISSN">0031-0182</identifier><identifier type="PII">S0031-0182(00)X0373-2</identifier><part><date>199103</date><detail type="volume"><number>89</number><caption>vol.</caption></detail><detail type="issue"><number>4</number><caption>no.</caption></detail><extent unit="issue pages"><start>315</start><end>414</end></extent><extent unit="pages"><start>379</start><end>398</end></extent></part></relatedItem><identifier type="istex">F3A148B34877B996E99A66026F4E183CE1654A53</identifier><identifier type="DOI">10.1016/0031-0182(91)90173-O</identifier><identifier type="PII">0031-0182(91)90173-O</identifier><recordInfo><recordContentSource>ELSEVIER</recordContentSource></recordInfo></mods></metadata></istex></record>Pour manipuler ce document sous Unix (Dilib)
EXPLOR_STEP=$WICRI_ROOT/Wicri/Agronomie/explor/SisAgriV1/Data/Istex/Corpus
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 001110 | SxmlIndent | more
Ou
HfdSelect -h $EXPLOR_AREA/Data/Istex/Corpus/biblio.hfd -nk 001110 | SxmlIndent | more
Pour mettre un lien sur cette page dans le réseau Wicri
{{Explor lien
|wiki= Wicri/Agronomie
|area= SisAgriV1
|flux= Istex
|étape= Corpus
|type= RBID
|clé= ISTEX:F3A148B34877B996E99A66026F4E183CE1654A53
|texte= Global coastal hazards from future sea level rise
}}
| This area was generated with Dilib version V0.6.28. |  |