{"NOAAStudyId":"17595","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":"2014-12-16","dataPublisher":"NOAA","dataType":"CLIMATE RECONSTRUCTIONS","dataTypeInformation":"https://www.ncdc.noaa.gov/data-access/paleoclimatology-data/datasets/climate-reconstruction","difMetadataLink":"http://www1.ncdc.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-recon-17595.xml","doi":null,"earliestYearBP":350,"earliestYearCE":1600,"entryId":"noaa-recon-17595","funding":[{"fundingAgency":"US National Science Foundation","fundingGrant":"AGS 1159430, 1202218"}],"investigators":"Wiles, G.; Solomina, O.; D'Arrigo, R.D.; Anchukaitis, K.J.; Gensiarovsky, Y.V.; Wiesenberg, N.","mostRecentYearBP":-54,"mostRecentYearCE":2004,"onlineResourceLink":"https://www.ncdc.noaa.gov/paleo/study/17595","originalSource":null,"publication":[{"abstract":"A new ring-width record from the eastern flanks of the Eastern Sakhalin Range, Sakhalin Island, Russian Federation is significantly correlated with summer temperatures and allows for the reconstruction of May-July average temperatures for the past 400 years. The reconstruction explains 37 % of the variance in May-July temperatures and shows a strong cooling between 1680 and 1710 CE coincident with the Maunder solar minimum and in agreement with other independent tree-ring reconstructions and glacier histories from sites along the margin of the Sea of Okhotsk. While recent decades are among the warmest in the record they are rivaled by periods centered on 1650 and 1850 CE. Warming in the observational record and the reconstruction is consistent with the influence of the declining strength of the Siberian High and loss of sea ice over the same interval. Decadal (17-25 year) variability persists throughout the reconstruction. At interannual timescales the Sakhalin reconstruction is most strongly correlated with local and central North Pacific sea surface temperatures over the past 120 years, whereas at decadal timescales there is an additional association with Asian land surface temperatures.","author":{"name":"Gregory C. Wiles, Olga Solomina, Rosanne D’Arrigo, Kevin J. Anchukaitis, Yury V. Gensiarovsky, Nicholas Wiesenberg"},"citation":"Gregory C. Wiles, Olga Solomina, Rosanne D’Arrigo, Kevin J. Anchukaitis, Yury V. Gensiarovsky, Nicholas Wiesenberg. 2014. Reconstructed summer temperatures over the last 400 years based on larch ring widths: Sakhalin Island, Russian Far East. Climate Dynamics. . doi: 10.1007/s00382-014-2209-2","edition":null,"identifier":{"id":"10.1007/s00382-014-2209-2","type":"doi","url":"http://dx.doi.org/10.1007/s00382-014-2209-2"},"issue":null,"journal":"Climate Dynamics","pages":null,"pubRank":"1","pubYear":2014,"reportNumber":null,"title":"Reconstructed summer temperatures over the last 400 years based on larch ring widths: Sakhalin Island, Russian Far East","type":"publication","volume":null}],"reconstruction":"Y","scienceKeywords":["Air Temperature Reconstruction"],"site":[{"NOAASiteId":"56375","geo":{"geoType":"Feature","geometry":{"coordinates":["51.03","143.59"],"type":"POINT"},"properties":{"easternmostLongitude":"143.59","maxElevationMeters":"10","minElevationMeters":"10","northernmostLatitude":"51.03","southernmostLatitude":"51.03","westernmostLongitude":"143.59"}},"locationName":"Continent>Asia>Eastern Asia","mappable":"Y","paleoData":[{"NOAADataTableId":"27914","coreLengthMeters":null,"dataFile":[{"NOAAKeywords":["earth science>paleoclimate>reconstructions>air temperature"],"fileUrl":"https://www1.ncdc.noaa.gov/pub/data/paleo/treering/reconstructions/asia/russia/sakhalin2015temp.txt","linkText":"Sakhalin Island Summer Temperature Reconstruction","urlDescription":"Data File","variables":[{"cvAdditionalInfo":null,"cvDataType":"CLIMATE RECONSTRUCTIONS|TREE RING","cvDetail":null,"cvError":null,"cvFormat":"Numeric","cvMaterial":null,"cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":"year Common Era","cvWhat":"age variable>age"},{"cvAdditionalInfo":"simple linear regression","cvDataType":"CLIMATE RECONSTRUCTIONS|TREE RING","cvDetail":null,"cvError":null,"cvFormat":"Numeric","cvMaterial":"reconstruction material>physical measurement>ring width","cvMethod":"regression analysis","cvSeasonality":"3-month period>May-Jul","cvShortName":null,"cvUnit":"degree Celsius","cvWhat":"earth system variable>temperature variable>temperature>surface temperature"}]}],"dataTableName":"Sakhalin2015temp","dataTableNotes":null,"earliestYear":1600,"earliestYearBP":350,"earliestYearCE":1600,"mostRecentYear":2004,"mostRecentYearBP":-54,"mostRecentYearCE":2004,"species":[],"timeUnit":"AD"}],"siteName":"Chamga Pass"}],"studyCode":null,"studyName":"Sakhalin Island, Russian Far East 400 Year Summer Temperature Reconstruction","studyNotes":"Summer (May-July) temperature reconstruction for the past 400 years for Sakhalin Island, Russian Far East. Reconstruction is based on linear regression of larch tree ring widths from Chamga Pass, Sakhalin Island, against monthly average temperature values from Yuhzno-Sakhalinsk, Sakhalin Oblast. The tree ring data are archived in the International Tree-Ring Data Bank, site code RUSS243.","version":"1.0","xmlId":"15277"}