{"title":"PMIP4 simulations: what is new?","authors":"P. Braconnot","doi":"10.4316/GEOREVIEW.2016.0.0.291","DOIUrl":null,"url":null,"abstract":"The Paleoclimate Modeling Intercomparison Project (PMIP) enters its fourth phase. Five PMIP periods have been retained for tier one simulations as part of CMIP6 (coupled model intercomparison project, phase 6): the last millennium, the mid-Holocene (6ka BP), the Last Glacial maximum (21ka BP), the Last Interglacial (127ka BP) and the Pliocene (3 Ma BP). The talk will review the rationale behind these simulations and highlight what would be needed from the paleoclimate community to fully benefit from this huge simulation effort.  The discussion will also discuss how this suite of PMIP4CMIP6 experiments is connected to several other periods and sensitivity experiments as part of PMIP. I propose to illustrate some of the new challenges that can now be tackled to improve the understanding of the rate of climate change, major feedbacks and the interplay between climate trends and climate variability","PeriodicalId":30470,"journal":{"name":"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series","volume":"26 1","pages":"6"},"PeriodicalIF":0.0000,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.4316/GEOREVIEW.2016.0.0.291","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

Abstract

The Paleoclimate Modeling Intercomparison Project (PMIP) enters its fourth phase. Five PMIP periods have been retained for tier one simulations as part of CMIP6 (coupled model intercomparison project, phase 6): the last millennium, the mid-Holocene (6ka BP), the Last Glacial maximum (21ka BP), the Last Interglacial (127ka BP) and the Pliocene (3 Ma BP). The talk will review the rationale behind these simulations and highlight what would be needed from the paleoclimate community to fully benefit from this huge simulation effort.  The discussion will also discuss how this suite of PMIP4CMIP6 experiments is connected to several other periods and sensitivity experiments as part of PMIP. I propose to illustrate some of the new challenges that can now be tackled to improve the understanding of the rate of climate change, major feedbacks and the interplay between climate trends and climate variability
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PMIP4模拟:有什么新的?
古气候模拟比对项目(PMIP)进入第四阶段。作为CMIP6(耦合模式比较项目,第6阶段)的一部分,一级模拟保留了5个PMIP时期:上千年、中全新世(6ka BP)、末次冰期(21ka BP)、末次间冰期(127ka BP)和上新世(3ma BP)。这次演讲将回顾这些模拟背后的基本原理,并强调古气候界需要什么才能从这一巨大的模拟努力中充分受益。讨论还将讨论这套PMIP4CMIP6实验如何连接到其他几个周期和灵敏度实验作为PMIP的一部分。我想说明一些现在可以解决的新挑战,以提高对气候变化速度、主要反馈以及气候趋势与气候变率之间相互作用的理解
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