globalchange  > 气候变化与战略
DOI: 10.5194/cp-12-1519-2016
Scopus记录号: 2-s2.0-84978933381
论文题名:
The PRISM4 (mid-Piacenzian) paleoenvironmental reconstruction
作者: Dowsett H.; Dolan A.; Rowley D.; Moucha R.; Forte A.M.; Mitrovica J.X.; Pound M.; Salzmann U.; Robinson M.; Chandler M.; Foley K.; Haywood A.
刊名: Climate of the Past
ISSN: 18149324
出版年: 2016
卷: 12, 期:7
起始页码: 1519
结束页码: 1538
语种: 英语
Scopus关键词: boundary condition ; climate modeling ; lake ; paleoclimate ; paleoenvironment ; paleogeography ; Pliocene ; reconstruction ; sea ice ; sea surface temperature ; soil structure ; topography ; vegetation dynamics
英文摘要: The mid-Piacenzian is known as a period of relative warmth when compared to the present day. A comprehensive understanding of conditions during the Piacenzian serves as both a conceptual model and a source for boundary conditions as well as means of verification of global climate model experiments. In this paper we present the PRISM4 reconstruction, a paleoenvironmental reconstruction of the mid-Piacenzian (∼ 3Ma) containing data for paleogeography, land and sea ice, sea-surface temperature, vegetation, soils, and lakes. Our retrodicted paleogeography takes into account glacial isostatic adjustments and changes in dynamic topography. Soils and lakes, both significant as land surface features, are introduced to the PRISM reconstruction for the first time. Sea-surface temperature and vegetation reconstructions are unchanged but now have confidence assessments. The PRISM4 reconstruction is being used as boundary condition data for the Pliocene Model Intercomparison Project Phase 2 (PlioMIP2) experiments. © Author(s) 2016.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/48993
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Recommended Citation:
Dowsett H.,Dolan A.,Rowley D.,et al. The PRISM4 (mid-Piacenzian) paleoenvironmental reconstruction[J]. Climate of the Past,2016-01-01,12(7)
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