Modeling the middle Pliocene climate with a global atmospheric general circulation model
文献类型：期刊论文
| 作者 | Jiang, DB; Wang, HJ; Ding, ZL; Lang, XM; Drange, H |
| 刊名 | JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
 |
| 出版日期 | 2005-07-27 |
| 卷号 | 110期号:D14 |
| ISSN号 | 2169-897X |
| DOI | 10.1029/2004JD005639 |
| 文献子类 | Article |
| 英文摘要 | A new climate simulation for the middle Pliocene (ca. 3 Ma BP) is performed by a global grid-point atmospheric general circulation model developed at the Institute of Atmospheric Physics (IAP AGCM) with boundary conditions provided by the U. S. Geological Survey's Pliocene Research, Interpretations, and Synoptic Mapping (PRISM) group. It follows that warmer and slightly wetter conditions dominated at the middle Pliocene with a globally annual mean surface temperature increase of 2.60 degrees C, and an increase in precipitation of 4.0% relative to today. At the middle Pliocene, globally annual terrestrial warming was 1.86 degrees C, with stronger warming toward high latitudes. Annual precipitation enhanced notably at high latitudes, with the augment reaching 33.5% (32.5%) of the present value at 60-90 degrees N (60-90 degrees S). On the contrary, drier conditions were registered over most parts at 0-30 degrees N, especially in much of East Asia and the northern tropical Pacific. In addition, both boreal summer and winter monsoon significantly decreased in East Asia at the middle Pliocene. It is indicated that the IAPAGCM simulation is generally consistent with the results from other atmospheric models and agrees well with available paleoclimatic reconstructions in East Asia. Additionally, it is further revealed that the PRISM warmer sea surface temperature and reduced sea ice extent are main factors determining the middle Pliocene climate. The simulated climatic responses arising from the PRISM reconstructed vegetation and continental ice sheet cannot be neglected on a regional scale at mid to high latitudes (like over Greenland and the Qinghai-Tibetan Plateau, and around the circum-Antarctic) but have little influence on global climate. |
| WOS关键词 | LAST GLACIAL MAXIMUM ; CHINESE LOESS PLATEAU ; RED CLAY ; NORTHERN-HEMISPHERE ; ICE-SHEET ; JOINT INVESTIGATIONS ; BOUNDARY-CONDITIONS ; PALEOCLIMATE ; MA ; VEGETATION |
| WOS研究方向 | Meteorology & Atmospheric Sciences |
| 语种 | 英语 |
| WOS记录号 | WOS:000230941200003 |
| 出版者 | AMER GEOPHYSICAL UNION |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/65640]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Jiang, DB |
| 作者单位 | 1.Chinese Acad Sci, Inst Atmospher Phys, Nansen Zhu Int Res Ctr, Beijing 100029, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China 3.Nansen Environm & Remote Sensing Ctr, Bergen, Norway |
| 推荐引用方式 GB/T 7714 | Jiang, DB,Wang, HJ,Ding, ZL,et al. Modeling the middle Pliocene climate with a global atmospheric general circulation model[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2005,110(D14). |
| APA | Jiang, DB,Wang, HJ,Ding, ZL,Lang, XM,&Drange, H.(2005).Modeling the middle Pliocene climate with a global atmospheric general circulation model.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,110(D14). |
| MLA | Jiang, DB,et al."Modeling the middle Pliocene climate with a global atmospheric general circulation model".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 110.D14(2005). |
入库方式： OAI收割
来源：地质与地球物理研究所
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