{"NOAAStudyId":"15974","contactInfo":{"address":"325 Broadway, E/NE31","city":"Boulder","constraints":"Please cite original publication, online resource, dataset and publication DOIs (where available), and date accessed when using downloaded data. If there is no publication information, please cite investigator, title, online resource, and date accessed. The appearance of external links associated with a dataset does not constitute endorsement by the Department of Commerce/National Oceanic and Atmospheric Administration of external Web sites or the information, products or services contained therein. For other than authorized activities, the Department of Commerce/NOAA does not exercise any editorial control over the information you may find at these locations. These links are provided consistent with the stated purpose of this Department of Commerce/NOAA Web site.","country":"USA","dataCenterUrl":"https://www.ncdc.noaa.gov/data-access/paleoclimatology-data","email":"paleo@noaa.gov","fax":"303-497-6513","longName":"National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce ","phone":"303-497-6280","postalCode":"80305-3328","shortName":"DOC/NOAA/NESDIS/NCEI","state":"CO","type":"CONTACT INFORMATION"},"contributionDate":"2014-01-24","dataPublisher":"NOAA","dataType":"LAKE LEVELS","dataTypeInformation":"https://www.ncdc.noaa.gov/data-access/paleoclimatology-data/datasets/lake-level-reconstruction","difMetadataLink":"http://www1.ncdc.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-lakelevel-15974.xml","doi":null,"earliestYearBP":650,"earliestYearCE":1300,"entryId":"noaa-lakelevel-15974","funding":[],"investigators":"Naderi Beni, A.; Lahijani, H.; Mousavi Harami, R.; Arpe, K.; Leroy, S.A.G.; Marriner, N.; Berberian, M.; Andrieu-Ponel, V.; Djamali, M.; Mahboubi, A.; Reimer, P.J.","mostRecentYearBP":75,"mostRecentYearCE":1875,"onlineResourceLink":"https://www.ncdc.noaa.gov/paleo/study/15974","originalSource":null,"publication":[{"abstract":"Historical literature may constitute a valuable source of information to reconstruct sea-level changes. Here, historical documents and geological records have been combined to reconstruct Caspian sea-level (CSL) changes during the last millennium. In addition to a comprehensive literature review, new data from two short sediment cores were obtained from the south-eastern Caspian coast to identify coastal change driven by water-level changes and to compare the results with other geological and historical findings.","author":{"name":"Naderi Beni, A., H. Lahijani, R. Mousavi Harami, K. Arpe, S.A.G. Leroy, N. Marriner, M. Berberian, V. Andrieu-Ponel, M. Djamali, A. Mahboubi, and P.J. Reimer"},"citation":"Naderi Beni, A., H. Lahijani, R. Mousavi Harami, K. Arpe, S.A.G. Leroy, N. Marriner, M. Berberian, V. Andrieu-Ponel, M. Djamali, A. Mahboubi, and P.J. Reimer. 2013. Caspian sea-level changes during the last millennium: historical and geological evidence from the south Caspian Sea. Climate of the Past, 9, 1645-1665. doi: 10.5194/cp-9-1645-2013","edition":null,"identifier":{"id":"10.5194/cp-9-1645-2013","type":"doi","url":"http://dx.doi.org/10.5194/cp-9-1645-2013"},"issue":null,"journal":"Climate of the Past","pages":"1645-1665","pubRank":"1","pubYear":2013,"reportNumber":null,"title":"Caspian sea-level changes during the last millennium: historical and geological evidence from the south Caspian Sea","type":"publication","volume":"9"}],"reconstruction":"N","scienceKeywords":["sea level"],"site":[{"NOAASiteId":"55794","geo":{"geoType":"Feature","geometry":{"coordinates":["34","47","46","55"],"type":"POLYGON"},"properties":{"easternmostLongitude":"55","maxElevationMeters":"-27","minElevationMeters":"-27","northernmostLatitude":"47","southernmostLatitude":"34","westernmostLongitude":"46"}},"locationName":"Continent>Europe>Eastern Europe","mappable":"N","paleoData":[{"NOAADataTableId":"25953","coreLengthMeters":null,"dataFile":[{"NOAAKeywords":["earth science>paleoclimate>lake levels"],"fileUrl":"https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/naderibeni2013/naderibeni2013.txt","linkText":"Caspian Sea Level","urlDescription":"Data File","variables":[{"cvAdditionalInfo":"historical observation","cvDataType":"LAKE LEVELS|PALEOLIMNOLOGY","cvDetail":null,"cvError":null,"cvFormat":"Character","cvMaterial":null,"cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":null,"cvWhat":"sampling metadata>notes"},{"cvAdditionalInfo":"geological event","cvDataType":"LAKE LEVELS|PALEOLIMNOLOGY","cvDetail":null,"cvError":null,"cvFormat":"Character","cvMaterial":null,"cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":null,"cvWhat":"sampling metadata>notes"},{"cvAdditionalInfo":null,"cvDataType":"LAKE LEVELS|PALEOLIMNOLOGY","cvDetail":null,"cvError":null,"cvFormat":"Character","cvMaterial":null,"cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":null,"cvWhat":"sampling metadata>notes"},{"cvAdditionalInfo":"meters above present lake level","cvDataType":"LAKE LEVELS|PALEOLIMNOLOGY","cvDetail":"raw","cvError":null,"cvFormat":"Character","cvMaterial":null,"cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":"meter","cvWhat":"earth system variable>hydrographic variable>lake level"},{"cvAdditionalInfo":null,"cvDataType":"LAKE LEVELS|PALEOLIMNOLOGY","cvDetail":null,"cvError":null,"cvFormat":"Numeric","cvMaterial":null,"cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":"year Common Era","cvWhat":"age variable>age"}]}],"dataTableName":"Caspian Sea Level NB13","dataTableNotes":"The study extends further back in time, but the data are not submitted here yet.","earliestYear":1300,"earliestYearBP":650,"earliestYearCE":1300,"mostRecentYear":1875,"mostRecentYearBP":75,"mostRecentYearCE":1875,"species":[],"timeUnit":"AD"}],"siteName":"Caspian Sea Boundary"}],"studyCode":null,"studyName":"Caspian Sea-Level Changes During the Last Millennium","studyNotes":"additional information, not in the publication, for circle points in fig. 9\t\t\t\nYear (AD)\tCSL\tReference\tExplanation\n1100-1125\t<-25\t Varushchenko et al.\tVarushchenko et al. (1987) findings, based on\n\t\t-1987\tdating, are more compatible with our findings\n\t\t\tin this paper than Bruckner (1890) or\n\t\t\tKarpychev (1998, 2001) historical evidence.\n1425-1450\t-26\tVarushchenko et al.\tThese 2 papers support each other while the\n\t\t-1987\tfindings of Bruckner (1890) seem to be\n\t\tKarpychev (1998, 2001)\toverestimated. I have chosen the overlapped\n\t\t\tyears, reported by the researchers for this\n\t\t\ttime. (the extended timeframe is 1350-1478\n\t\t\tAD for -26)\n1680\t<-24 \tBruckner (1890)\tAll the graphs of the referenced authors meet\n\t\tKarpychev (1998, 2001)\teach other in this time that support Komarova\n\t\tVarushchenko et al.\t(1980) sea level curve for this period.\n                -1987\t\n1700\t<-26 \tBruckner (1890)\tThe reported sea level is around the same for\n\t\tKarpychev (1998, 2001)\tthis time by different researchers. Moreover,\n\t\tFedchina (1980)\tthis is supported by the findings of Fedchina\n\t\tKomarova (1980)\t(1980) and Komarova (1980).\n1740\t>-23\t Bruckner (1890)\tThere is a good agreement between different\n\t\tKarpychev (1998, 2001)\tresearchers on CSL in this time based on\n\t\tFedchina (1980)\tdifferent approaches Komarova (1980)\t\n1775-1790\t<-22 \tBruckner (1890)\tIn addition to the references, Karpychev\n\t\tVarushchenko et al.\t(1998, 2001) indicated CSL for 1770-1790\n\t\t-1987\tand 1790-1810 as -25 and -22, respectively.\n\t\tKomarova (1980)\tAccording to radiocarbon dating method and\n\t\t\tits errors, I have preferred to choose the -22 CSL for this time.\n1825\t>-25\t Bruckner (1890)\tBruckner (1890) indicated CSL as -25.8 m in\n\t\tVarushchenko et al.\t1825 and Varushchenko et al. (1987) indicated\n\t\t-1987\tthe CSL -25 in 1825-1826. When we plot\n\t\t\tother results from Karpychev (1998, 2001),\n\t\t\tall the graphs meet each other in -25 m in 1825\n","version":"1.0","xmlId":"13739"}