| 北极径流增加对大西洋经向翻转环流影响的模拟研究 |
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| 引用本文： | 舒启,乔方利,宋振亚,肖斌.北极径流增加对大西洋经向翻转环流影响的模拟研究[J].海洋学报(英文版),2017,36(8):59-65. |
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| 作者姓名： | 舒启 乔方利 宋振亚 肖斌 |
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| 作者单位： | 国家海洋局第一海洋研究所;青岛海洋科学与技术国家实验室, 区域海洋动力学与数值模拟功能实验室;海洋环境科学和数值模拟国家海洋局重点实验室,国家海洋局第一海洋研究所;青岛海洋科学与技术国家实验室, 区域海洋动力学与数值模拟功能实验室;海洋环境科学和数值模拟国家海洋局重点实验室,国家海洋局第一海洋研究所;青岛海洋科学与技术国家实验室, 区域海洋动力学与数值模拟功能实验室;海洋环境科学和数值模拟国家海洋局重点实验室,国家海洋局第一海洋研究所;青岛海洋科学与技术国家实验室, 区域海洋动力学与数值模拟功能实验室;海洋环境科学和数值模拟国家海洋局重点实验室 |
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| 基金项目： | The Project of Comprehensive Evaluation of Polar Areas on Global and Regional Climate Changes under contract No. CHINARE2016-04-04; the National Natural Science Foundation of China under contract No. 41406027; the NSFC-Shandong Joint Fund for Marine Science Research Centers under contract No. U1406404; the Basic Research Operating Funds of The First Institute of Oceanography, State Oceanic Administration of China under contract Nos 2015P03 and 2015P01. |
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| 摘 要： | 观测显示过去几十年间北极入海径流呈现增加趋势，CMIP5耦合模式预测表明21世纪北极入海径流仍会增加，在RCP8.5路径下，21世纪末北极入海径流量将会是1950年的1.4倍。本文利用冰-海耦合数值模式研究了北极径流增加对大西洋经向翻转环流的影响。基于两个数值实验的结果表明，如果北极入海径流按每年0.22%的速度（与RCP8.5路径下的速度相当）增加，大西洋经向翻转环流的强度在100、150和200年后将会分别减弱0.6（3%）、1.2（7%）和1.8（11%） Sv。北极入海径流增加导致大西洋经向翻转环流减弱的主要原因是，北极入海径流增加的淡水被输运到北大西洋后，会抑制北大西洋深层水的生成，这也会导致北大西洋深层水海水年龄的增加。
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| 关 键 词： | 气候变化 北极径流 大西洋经向翻转环流 |
| 收稿时间： | 2016/7/6 0:00:00 |
Effect of increasing Arctic river runoff on the Atlantic meridional overturning circulation:a model study |
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| SHU Qi,QIAO Fangli,SONG Zhenya and XIAO Bin.Effect of increasing Arctic river runoff on the Atlantic meridional overturning circulation:a model study[J].Acta Oceanologica Sinica,2017,36(8):59-65. |
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| Authors: | SHU Qi QIAO Fangli SONG Zhenya and XIAO Bin |
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| Institution: | The First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China;Laboratory for Regional Oceanography and Numerical Modeling, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China;Key Laboratory of Marine Science and Numerical Modeling, State Oceanic Administration, Qingdao 266061, China |
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| Abstract: | An increasing amount of freshwater has been observed to enter the Arctic Ocean from the six largest Eurasian rivers over the past several decades. The increasing trend is projected to continue in the twenty-first century according to Coupled Model Intercomparison Project Phase 5 (CMIP5) coupled models. The present study found that water flux from rivers to the Arctic Ocean at the end of the century will be 1.4 times that in 1950 according to CMIP5 projection results under Representative Concentration Pathway 8.5. The effect of increasing Arctic river runoff on the Atlantic meridional overturning circulation (AMOC) was investigated using an ocean-ice coupled model. Results obtained from two numerical experiments show that 100, 150 and 200 years after the start of an increase in the Arctic river runoff at a rate of 0.22%/a, the AMOC will weaken by 0.6 (3%), 1.2 (7%) and 1.8 (11%) Sv. AMOC weakening is mainly caused by freshwater transported from increasing Arctic river runoff inhibiting the formation of North Atlantic Deep Water (NADW). As the AMOC weakens, the deep seawater age will become older throughout the Atlantic Basin owing to the increasing of Arctic runoff. |
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| Keywords: | climate change Arctic river runoff Atlantic meridional overturning circulation |
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