NUIST ESM v3 Data Submission to CMIP6
This paper introduces the experimental designs and outputs of the Diagnostic, Evaluation and Characterization of Klima (DECK), historical, Scenario Model Intercomparison Project (MIP), and Paleoclimate MIP (PMIP) experiments from the Nanjing University of Information Science and Technology Earth Sys...
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| Veröffentlicht in: | Advances in atmospheric sciences 2021-02, Vol.38 (2), p.268-284 |
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| creator | Cao, Jian Ma, Libin Liu, Fei Chai, Jing Zhao, Haikun He, Qiong Wang, Bo Bao, Yan Li, Juan Yang, Young-min Deng, Hua Wang, Bin |
| description | This paper introduces the experimental designs and outputs of the Diagnostic, Evaluation and Characterization of Klima (DECK), historical, Scenario Model Intercomparison Project (MIP), and Paleoclimate MIP (PMIP) experiments from the Nanjing University of Information Science and Technology Earth System Model version 3 (NESM3). Results show that NESM3 reasonably simulates the modern climate and the major internal modes of climate variability. In the Scenario MIP experiment, changes in the projected surface air temperature (SAT) show robust “Northern Hemisphere (NH) warmer than Southern Hemisphere (SH)” and “land warmer than ocean” patterns, as well as an El Niño-like warming over the tropical Pacific. Changes in the projected precipitation exhibit “NH wetter than SH” and “eastern hemisphere gets wetter and western hemisphere gets drier” patterns over the tropics. These precipitation patterns are driven by circulation changes owing to the inhomogeneous warming patterns. Two PMIP experiments show enlarged seasonal cycles of SAT and precipitation over the NH due to the seasonal redistribution of solar radiation. Changes in the climatological mean SAT, precipitation, and ENSO amplitudes are consistent with the results from PMIP4 models. The NESM3 outputs are available on the Earth System Grid Federation nodes for data users. |
| doi_str_mv | 10.1007/s00376-020-0173-9 |
| format | Article |
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Results show that NESM3 reasonably simulates the modern climate and the major internal modes of climate variability. In the Scenario MIP experiment, changes in the projected surface air temperature (SAT) show robust “Northern Hemisphere (NH) warmer than Southern Hemisphere (SH)” and “land warmer than ocean” patterns, as well as an El Niño-like warming over the tropical Pacific. Changes in the projected precipitation exhibit “NH wetter than SH” and “eastern hemisphere gets wetter and western hemisphere gets drier” patterns over the tropics. These precipitation patterns are driven by circulation changes owing to the inhomogeneous warming patterns. Two PMIP experiments show enlarged seasonal cycles of SAT and precipitation over the NH due to the seasonal redistribution of solar radiation. Changes in the climatological mean SAT, precipitation, and ENSO amplitudes are consistent with the results from PMIP4 models. The NESM3 outputs are available on the Earth System Grid Federation nodes for data users.</description><identifier>ISSN: 0256-1530</identifier><identifier>EISSN: 1861-9533</identifier><identifier>DOI: 10.1007/s00376-020-0173-9</identifier><language>eng</language><publisher>Heidelberg: Science Press</publisher><subject>Air temperature ; Atmospheric Sciences ; Climate ; Climate change ; Climate variability ; Climatological means ; CMIP6 Experiments: Model and Dataset Descriptions ; Data Description Article ; Decks ; Diagnostic systems ; Earth and Environmental Science ; Earth Sciences ; Eastern Hemisphere ; El Nino ; El Nino phenomena ; El Nino-Southern Oscillation event ; Geophysics/Geodesy ; Intercomparison ; Meteorology ; Northern Hemisphere ; Paleoclimate ; Precipitation ; Precipitation patterns ; Science and technology ; Seasonal variation ; Solar radiation ; Southern Hemisphere ; Southern Oscillation ; Surface temperature ; Surface-air temperature relationships ; Tropical climate ; Tropical environments ; Western Hemisphere</subject><ispartof>Advances in atmospheric sciences, 2021-02, Vol.38 (2), p.268-284</ispartof><rights>The Authors 2021</rights><rights>The Authors 2021. This work is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c393t-310e4c1acbd41cedfe2e2aaaeb9cfea5c6a668986704858138a8f43e312851093</citedby><cites>FETCH-LOGICAL-c393t-310e4c1acbd41cedfe2e2aaaeb9cfea5c6a668986704858138a8f43e312851093</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://www.wanfangdata.com.cn/images/PeriodicalImages/dqkxjz-e/dqkxjz-e.jpg</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s00376-020-0173-9$$EPDF$$P50$$Gspringer$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00376-020-0173-9$$EHTML$$P50$$Gspringer$$Hfree_for_read</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Cao, Jian</creatorcontrib><creatorcontrib>Ma, Libin</creatorcontrib><creatorcontrib>Liu, Fei</creatorcontrib><creatorcontrib>Chai, Jing</creatorcontrib><creatorcontrib>Zhao, Haikun</creatorcontrib><creatorcontrib>He, Qiong</creatorcontrib><creatorcontrib>Wang, Bo</creatorcontrib><creatorcontrib>Bao, Yan</creatorcontrib><creatorcontrib>Li, Juan</creatorcontrib><creatorcontrib>Yang, Young-min</creatorcontrib><creatorcontrib>Deng, Hua</creatorcontrib><creatorcontrib>Wang, Bin</creatorcontrib><title>NUIST ESM v3 Data Submission to CMIP6</title><title>Advances in atmospheric sciences</title><addtitle>Adv. Atmos. Sci</addtitle><description>This paper introduces the experimental designs and outputs of the Diagnostic, Evaluation and Characterization of Klima (DECK), historical, Scenario Model Intercomparison Project (MIP), and Paleoclimate MIP (PMIP) experiments from the Nanjing University of Information Science and Technology Earth System Model version 3 (NESM3). Results show that NESM3 reasonably simulates the modern climate and the major internal modes of climate variability. In the Scenario MIP experiment, changes in the projected surface air temperature (SAT) show robust “Northern Hemisphere (NH) warmer than Southern Hemisphere (SH)” and “land warmer than ocean” patterns, as well as an El Niño-like warming over the tropical Pacific. Changes in the projected precipitation exhibit “NH wetter than SH” and “eastern hemisphere gets wetter and western hemisphere gets drier” patterns over the tropics. These precipitation patterns are driven by circulation changes owing to the inhomogeneous warming patterns. Two PMIP experiments show enlarged seasonal cycles of SAT and precipitation over the NH due to the seasonal redistribution of solar radiation. Changes in the climatological mean SAT, precipitation, and ENSO amplitudes are consistent with the results from PMIP4 models. The NESM3 outputs are available on the Earth System Grid Federation nodes for data users.</description><subject>Air temperature</subject><subject>Atmospheric Sciences</subject><subject>Climate</subject><subject>Climate change</subject><subject>Climate variability</subject><subject>Climatological means</subject><subject>CMIP6 Experiments: Model and Dataset Descriptions</subject><subject>Data Description Article</subject><subject>Decks</subject><subject>Diagnostic systems</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Eastern Hemisphere</subject><subject>El Nino</subject><subject>El Nino phenomena</subject><subject>El Nino-Southern Oscillation event</subject><subject>Geophysics/Geodesy</subject><subject>Intercomparison</subject><subject>Meteorology</subject><subject>Northern Hemisphere</subject><subject>Paleoclimate</subject><subject>Precipitation</subject><subject>Precipitation patterns</subject><subject>Science and technology</subject><subject>Seasonal variation</subject><subject>Solar radiation</subject><subject>Southern Hemisphere</subject><subject>Southern Oscillation</subject><subject>Surface temperature</subject><subject>Surface-air temperature relationships</subject><subject>Tropical climate</subject><subject>Tropical environments</subject><subject>Western Hemisphere</subject><issn>0256-1530</issn><issn>1861-9533</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>C6C</sourceid><recordid>eNp1kMFOAjEQhhujiYg-gLdNjAcP1Zl22-0eDaKSgJoA56aULgFlF9pF1Ke3mzXh5Gku3__NzE_IJcItAmR3AYBnkgIDCphxmh-RDiqJNBecH5MOMCEpCg6n5CyEVaRzrrBDrl-mg_Ek6Y9HySdPHkxtkvFutl6GsKzKpK6S3mjwJs_JSWE-grv4m10yfexPes90-Po06N0PqY26mnIEl1o0djZP0bp54Zhjxhg3y23hjLDSSKlyJTNIlVDIlVFFyh1HpgRCzrvkpvXuTVmYcqFX1c6XcaOeb9-_Vj_aMWAYnwQV2auW3fhqu3OhPsAsVSxPBaiGwpayvgrBu0Jv_HJt_LdG0E1zum1OR6lumtPNFazNhMiWC-cP5v9Dv6z7bHU</recordid><startdate>20210201</startdate><enddate>20210201</enddate><creator>Cao, Jian</creator><creator>Ma, Libin</creator><creator>Liu, Fei</creator><creator>Chai, Jing</creator><creator>Zhao, Haikun</creator><creator>He, Qiong</creator><creator>Wang, Bo</creator><creator>Bao, Yan</creator><creator>Li, Juan</creator><creator>Yang, Young-min</creator><creator>Deng, Hua</creator><creator>Wang, Bin</creator><general>Science Press</general><general>Springer Nature B.V</general><general>Department of Atmospheric Sciences, University of Hawaii at Manoa, Honolulu, HI 96825, USA</general><general>Earth System Modeling Center, Nanjing University of Information Science and Technology, Nanjing 210044, China%State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081, China%Key Laboratory of Meteorological Disaster, Ministry of Education/Joint International Research Laboratory of Climateand Environment Change/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science and Technology, Nanjing 210044, China%Earth System Modeling Center, Nanjing University of Information Science and Technology, Nanjing 210044, China</general><general>Key Laboratory of Meteorological Disaster, Ministry of Education/Joint International Research Laboratory of Climateand Environment Change/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science and Technology, Nanjing 210044, China</general><scope>C6C</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>20210201</creationdate><title>NUIST ESM v3 Data Submission to CMIP6</title><author>Cao, Jian ; 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Atmos. Sci</stitle><date>2021-02-01</date><risdate>2021</risdate><volume>38</volume><issue>2</issue><spage>268</spage><epage>284</epage><pages>268-284</pages><issn>0256-1530</issn><eissn>1861-9533</eissn><abstract>This paper introduces the experimental designs and outputs of the Diagnostic, Evaluation and Characterization of Klima (DECK), historical, Scenario Model Intercomparison Project (MIP), and Paleoclimate MIP (PMIP) experiments from the Nanjing University of Information Science and Technology Earth System Model version 3 (NESM3). Results show that NESM3 reasonably simulates the modern climate and the major internal modes of climate variability. In the Scenario MIP experiment, changes in the projected surface air temperature (SAT) show robust “Northern Hemisphere (NH) warmer than Southern Hemisphere (SH)” and “land warmer than ocean” patterns, as well as an El Niño-like warming over the tropical Pacific. Changes in the projected precipitation exhibit “NH wetter than SH” and “eastern hemisphere gets wetter and western hemisphere gets drier” patterns over the tropics. These precipitation patterns are driven by circulation changes owing to the inhomogeneous warming patterns. Two PMIP experiments show enlarged seasonal cycles of SAT and precipitation over the NH due to the seasonal redistribution of solar radiation. Changes in the climatological mean SAT, precipitation, and ENSO amplitudes are consistent with the results from PMIP4 models. The NESM3 outputs are available on the Earth System Grid Federation nodes for data users.</abstract><cop>Heidelberg</cop><pub>Science Press</pub><doi>10.1007/s00376-020-0173-9</doi><tpages>17</tpages><oa>free_for_read</oa></addata></record> |
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| subjects | Air temperature Atmospheric Sciences Climate Climate change Climate variability Climatological means CMIP6 Experiments: Model and Dataset Descriptions Data Description Article Decks Diagnostic systems Earth and Environmental Science Earth Sciences Eastern Hemisphere El Nino El Nino phenomena El Nino-Southern Oscillation event Geophysics/Geodesy Intercomparison Meteorology Northern Hemisphere Paleoclimate Precipitation Precipitation patterns Science and technology Seasonal variation Solar radiation Southern Hemisphere Southern Oscillation Surface temperature Surface-air temperature relationships Tropical climate Tropical environments Western Hemisphere |
| title | NUIST ESM v3 Data Submission to CMIP6 |
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