首页> 外文期刊>Exchanges : Newsletter of the Climate Variability and Predictability Programme (CLIVAR) >The International CLIVAR Climate of the 20th Century Plus (C20C+) Project: Report of the Sixth Workshop
【24h】

The International CLIVAR Climate of the 20th Century Plus (C20C+) Project: Report of the Sixth Workshop

机译:20世纪国际CLIVAR气候变化(C20C +)项目:第六次研讨会报告

获取原文
       

摘要

The International CLIVAR Climate of the 20th CenturyProject (C20C; Folland et al., 2002) held its Sixth Workshopon 5-8 November 2013 at the University of Melbourne,Australia. C20C brings together climate modelling and dataanalysis groups to study climate variations and changes overperiods up to the last 150 years using observational data andgeneral circulation models (GCMs). There is an emphasison atmospheric GCMs (AGCMs) forced with observedvalues of atmospheric composition (concentrations ofgreenhouse gases, aerosols, etc.) and surface conditions(SST, sea ice, land surface vegetation, etc.) as well as onnatural variations alone. As agreed at the fifth Workshopin Beijing in 2010 (Kinter and Folland, 2011), the new C20Ccore project involves research in collaboration with theInternational Detection and Attribution Group and theinternational Attribution of Climate-related Events activityinto the influence of anthropogenic forcing on climaticevents, particularly extreme climate events. This is partlyto support new research on quasi-operational attribution.The goal of the Sixth Workshop was to review early progressin the new core activity, observational data sets that willsupport C20C activities, and other key C20C projects. As inprevious C20C meetings, the forcing data sets being used ina new set of coordinated model experiments, including the more observations and attain greater accuracy andresolution. Titchner and Rayner (2014) describes the sea icecomponent. Key improvements of HadISST2 over HadISST1are multiple (100) realizations (though only a small subsetis likely to be used by C20C+), better resolution in time, newbias corrections to SST right up to the present, inclusion ofAATSR satellite data and a considerably improved sea iceextent data set. Talks on the complex process used to createthe SST and sea ice components of HadISST were presentedat the Workshop.
机译:20世纪国际CLIVAR气候项目(C20C; Folland等,2002)于2013年11月5日至8日在澳大利亚墨尔本大学举行了第六次研讨会。 C20C聚集了气候建模和数据分析小组,以使用观测数据和一般环流模型(GCM)研究近150年来的气候变化和周期变化。重点强调了大气GCM(AGCM),其强迫值取决于大气成分(温室气体,气溶胶等的浓度)和地表条件(海表温度,海冰,陆地表面植被等)的观测值以及仅是自然变化。正如2010年在北京举行的第五次研讨会(Kinter和Folland,2011年)所商定的那样,新的C20Ccore项目涉及与国际检测与归因小组以及国际气候相关事件归因活动合作进行研究,以研究人为强迫对气候事件(特别是极端气候事件)的影响。气候事件。这部分是为了支持对准运营归属的新研究。第六次研讨会的目的是回顾新的核心活动,支持C20C活动的观测数据集以及其他关键C20C项目的早期进展。作为以前的C20C会议,强制数据集被用于一组新的协调模型实验中,包括更多的观察结果,以及更高的准确性和分辨率。 Titchner和Rayner(2014)描述了海冰成分。与HadISST1相比,HadISST2的关键改进是多(100)个实现(尽管C20C +可能仅使用一小部分子集),更及时的分辨率,直到现在为止对SST的newbias校正,包括了AATSR卫星数据以及大大改善的海冰范围数据集。在研讨会上,讨论了用于创建HadISST的SST和海冰组件的复杂过程。

著录项

相似文献

  • 外文文献
  • 中文文献
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号