The Atmosphere During the Younger Dryas
One of the most dramatic climate change events observed in marine and ice core records is the Younger Dryas, a return to near-glacial conditions that punctuated the last deglaciation. High-resolution, continuous glaciochemical records, newly retrieved from central Greenland, record the chemical comp...
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| Veröffentlicht in: | Science (American Association for the Advancement of Science) 1993-07, Vol.261 (5118), p.195-197 |
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| creator | Mayewski, P. A. Meeker, L. D. Whitlow, S. Twickler, M. S. Morrison, M. C. Alley, R. B. Bloomfield, P. Taylor, K. |
| description | One of the most dramatic climate change events observed in marine and ice core records is the Younger Dryas, a return to near-glacial conditions that punctuated the last deglaciation. High-resolution, continuous glaciochemical records, newly retrieved from central Greenland, record the chemical composition of the arctic atmosphere at this time. This record shows that both the onset and the termination of the Younger Dryas occurred within 10 to 20 years and that massive, frequent, and short-term (decadal or less) changes in atmospheric composition occurred throughout this event. Changes in atmospheric composition are attributable to changes in the size of the polar atmospheric cell and resultant changes in source regions and to the growth and decay of continental biogenic source regions. |
| doi_str_mv | 10.1126/science.261.5118.195 |
| format | Article |
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A. ; Meeker, L. D. ; Whitlow, S. ; Twickler, M. S. ; Morrison, M. C. ; Alley, R. B. ; Bloomfield, P. ; Taylor, K.</creator><creatorcontrib>Mayewski, P. A. ; Meeker, L. D. ; Whitlow, S. ; Twickler, M. S. ; Morrison, M. C. ; Alley, R. B. ; Bloomfield, P. ; Taylor, K.</creatorcontrib><description>One of the most dramatic climate change events observed in marine and ice core records is the Younger Dryas, a return to near-glacial conditions that punctuated the last deglaciation. High-resolution, continuous glaciochemical records, newly retrieved from central Greenland, record the chemical composition of the arctic atmosphere at this time. This record shows that both the onset and the termination of the Younger Dryas occurred within 10 to 20 years and that massive, frequent, and short-term (decadal or less) changes in atmospheric composition occurred throughout this event. 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A.</creatorcontrib><creatorcontrib>Meeker, L. D.</creatorcontrib><creatorcontrib>Whitlow, S.</creatorcontrib><creatorcontrib>Twickler, M. S.</creatorcontrib><creatorcontrib>Morrison, M. C.</creatorcontrib><creatorcontrib>Alley, R. B.</creatorcontrib><creatorcontrib>Bloomfield, P.</creatorcontrib><creatorcontrib>Taylor, K.</creatorcontrib><title>The Atmosphere During the Younger Dryas</title><title>Science (American Association for the Advancement of Science)</title><addtitle>Science</addtitle><description>One of the most dramatic climate change events observed in marine and ice core records is the Younger Dryas, a return to near-glacial conditions that punctuated the last deglaciation. High-resolution, continuous glaciochemical records, newly retrieved from central Greenland, record the chemical composition of the arctic atmosphere at this time. 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Changes in atmospheric composition are attributable to changes in the size of the polar atmospheric cell and resultant changes in source regions and to the growth and decay of continental biogenic source regions.</description><subject>540110</subject><subject>Air masses</subject><subject>ALKALI METALS</subject><subject>ALKALINE EARTH METALS</subject><subject>AMMONIUM COMPOUNDS</subject><subject>Atmosphere</subject><subject>ATMOSPHERIC CHEMISTRY</subject><subject>ATMOSPHERIC PRECIPITATIONS</subject><subject>CALCIUM</subject><subject>CHEMICAL ANALYSIS</subject><subject>CHEMICAL COMPOSITION</subject><subject>CHEMISTRY</subject><subject>CHLORIDES</subject><subject>CHLORINE COMPOUNDS</subject><subject>Climate change</subject><subject>CLIMATIC CHANGE</subject><subject>Climatic changes</subject><subject>Correlation</subject><subject>EARTH ATMOSPHERE</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>ELEMENTS</subject><subject>ENVIRONMENTAL SCIENCES</subject><subject>Exact sciences and technology</subject><subject>GENERAL CIRCULATION MODELS</subject><subject>GLACIERS</subject><subject>HALIDES</subject><subject>HALOGEN COMPOUNDS</subject><subject>Ice ages</subject><subject>Ice sheets</subject><subject>MAGNESIUM</subject><subject>Marine and continental quaternary</subject><subject>MATHEMATICAL MODELS</subject><subject>METALS</subject><subject>NITRATES</subject><subject>NITROGEN COMPOUNDS</subject><subject>Organic Chemistry</subject><subject>OXYGEN COMPOUNDS</subject><subject>PALEOCLIMATOLOGY</subject><subject>PALEONTOLOGY</subject><subject>POTASSIUM</subject><subject>QUANTITATIVE CHEMICAL ANALYSIS</subject><subject>Quaternary ammonium compounds</subject><subject>Salts</subject><subject>Seas</subject><subject>SODIUM</subject><subject>SULFATES</subject><subject>SULFUR COMPOUNDS</subject><subject>Surficial geology</subject><subject>Younger Dryas period</subject><issn>0036-8075</issn><issn>1095-9203</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1993</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>BEC</sourceid><sourceid>BENPR</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNqN0kFr2zAUB3AzNta02zcoI4yx7lBnkizL0jFLt6wQlsO6wU5CkZ8dB1vKJBnabz-ZhJRAGEEHgd5Pekj6J8k1RhOMCfvsdQNGw4QwPMkx5hMs8hfJCCORp4Kg7GUyQihjKUdFfpFcer9BKNZE9jq5wAUnghRslNw8rGE8DZ312zU4GN_1rjH1OMTVP7Y3NbjxnXtS_k3yqlKth7f7-Sr59e3rw-x7uljO72fTRao4IiGlHK_oChCvilWVa4RVqWkpKBRKadCoorkqGeWCcMpZLkqaE6gYEbgQAiGWXSXvd-daHxoZ7xhAr7U1BnSQjFDGEY_oZoe2zv7twQfZNV5D2yoDtveyyDJCUcaH4z7-VxKWIYIJfu57gBvbOxOvKmM1j8-GB3S7Q7VqQTamssEpXYMBp1proGri8hRTUhSMDc3TEzyOErpGn_KfjnwkAR5DrXrv5f3PH2fT5e-z6Zf5uZTPF0f09hTVtm2hBhkzMVsecbrj2lnvHVRy65pOuSeJkRziLPdxjj-C5RBnGeMct73b_0q_6qB83rTPbwQf9kB5rdrKKaMbf3CU5wXBIrLrHdv4YN2hTDjHHJPsHyKq_70</recordid><startdate>19930709</startdate><enddate>19930709</enddate><creator>Mayewski, P. 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A.</au><au>Meeker, L. D.</au><au>Whitlow, S.</au><au>Twickler, M. S.</au><au>Morrison, M. C.</au><au>Alley, R. B.</au><au>Bloomfield, P.</au><au>Taylor, K.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The Atmosphere During the Younger Dryas</atitle><jtitle>Science (American Association for the Advancement of Science)</jtitle><addtitle>Science</addtitle><date>1993-07-09</date><risdate>1993</risdate><volume>261</volume><issue>5118</issue><spage>195</spage><epage>197</epage><pages>195-197</pages><issn>0036-8075</issn><eissn>1095-9203</eissn><coden>SCIEAS</coden><abstract>One of the most dramatic climate change events observed in marine and ice core records is the Younger Dryas, a return to near-glacial conditions that punctuated the last deglaciation. High-resolution, continuous glaciochemical records, newly retrieved from central Greenland, record the chemical composition of the arctic atmosphere at this time. This record shows that both the onset and the termination of the Younger Dryas occurred within 10 to 20 years and that massive, frequent, and short-term (decadal or less) changes in atmospheric composition occurred throughout this event. Changes in atmospheric composition are attributable to changes in the size of the polar atmospheric cell and resultant changes in source regions and to the growth and decay of continental biogenic source regions.</abstract><cop>Washington, DC</cop><pub>American Society for the Advancement of Science</pub><pmid>17829276</pmid><doi>10.1126/science.261.5118.195</doi><tpages>3</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0036-8075 |
| ispartof | Science (American Association for the Advancement of Science), 1993-07, Vol.261 (5118), p.195-197 |
| issn | 0036-8075 1095-9203 |
| language | eng |
| recordid | cdi_osti_scitechconnect_6246808 |
| source | American Association for the Advancement of Science; Jstor Complete Legacy |
| subjects | 540110 Air masses ALKALI METALS ALKALINE EARTH METALS AMMONIUM COMPOUNDS Atmosphere ATMOSPHERIC CHEMISTRY ATMOSPHERIC PRECIPITATIONS CALCIUM CHEMICAL ANALYSIS CHEMICAL COMPOSITION CHEMISTRY CHLORIDES CHLORINE COMPOUNDS Climate change CLIMATIC CHANGE Climatic changes Correlation EARTH ATMOSPHERE Earth sciences Earth, ocean, space ELEMENTS ENVIRONMENTAL SCIENCES Exact sciences and technology GENERAL CIRCULATION MODELS GLACIERS HALIDES HALOGEN COMPOUNDS Ice ages Ice sheets MAGNESIUM Marine and continental quaternary MATHEMATICAL MODELS METALS NITRATES NITROGEN COMPOUNDS Organic Chemistry OXYGEN COMPOUNDS PALEOCLIMATOLOGY PALEONTOLOGY POTASSIUM QUANTITATIVE CHEMICAL ANALYSIS Quaternary ammonium compounds Salts Seas SODIUM SULFATES SULFUR COMPOUNDS Surficial geology Younger Dryas period |
| title | The Atmosphere During the Younger Dryas |
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