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潮汐混合对大西洋经圈翻转环流(AMOC)模拟影响的数值模拟研究

于子棚 刘海龙 林鹏飞

大气科学2017,Vol.41Issue(5):1087-1100,14.
大气科学2017,Vol.41Issue(5):1087-1100,14.DOI:10.3878/j.issn.1006-9895.1702.16263

潮汐混合对大西洋经圈翻转环流(AMOC)模拟影响的数值模拟研究

A Numerical Study of the Influence of Tidal Mixing on Atlantic Meridional Overturning Circulation (AMOC) Simulation

于子棚 1刘海龙 2林鹏飞1

作者信息

  • 1. 中国科学院大气物理研究所大气科学和地球流体力学数值模拟国家重点试验室,北京100029
  • 2. 中国科学院大学,北京100049
  • 折叠

摘要

Abstract

The impact of the tidal mixing on the simulation of the Atlantic Meridional Overturning Circulation (AMOC)is an important issue in the ocean general circulation model.The response of AMOC to the tidal mixing is investigated in this study by comparing two experiments with and without tidal mixing using the LASG/IAP Climate System Ocean Model version 2 (LICOM2) that is coupled with the Community Ice Code version 4 (CICE4).The study is focused on impacts of tidal mixing on the change of AMOC intensity in the model.The simulation results show that the maximum strength of AMOC in the experiment with tidal mixing is closer to the value provided by RAPID (Rapid Climate Change Programme),which is almost double that in the control experiment without considering the tidal mixing.Meanwhile,the NADW cell reaches a depth of 3200 m,about 1000 m deeper than that in the control experiment,and is closer to that of the RAPID.The enhanced vertical diffusivity near the seafloor topography in the experiment with tidal mixing leads to a more unstable ocean stratification,which will enhance deep convection in the high latitudes of North Atlantic,especially in the Labrador Sea.This will strengthen AMOC intensity directly.Meanwhile,the upper ocean circulation is stronger in the experiment of tidal mixing,bringing more heat and salinity from the subtropics to the high latitudes and leading to denser surface water.The denser water subsequently destroys the stable stratification and intensifies the deep convection,resulting in stronger AMOC indirectly.

关键词

LASG/IAP气候系统海洋模式/潮汐混合/大西洋经圈翻转环流

Key words

LASG/IAP Climate system Ocean Model/Tidal mixing/Atlantic Meridional Overturning Circulation

分类

天文与地球科学

引用本文复制引用

于子棚,刘海龙,林鹏飞..潮汐混合对大西洋经圈翻转环流(AMOC)模拟影响的数值模拟研究[J].大气科学,2017,41(5):1087-1100,14.

基金项目

国家重点基础研究发展计划项目 2013CB956204,中国科学院战略重点研究项目“西太平洋系统:结构、动力、影响”XDA11010304,国家自然科学基金项目 41376019、41275084、41075059 ()

the National Basic Research and Development Program (973 Program) of China (Grant 2013CB956204),Strategic Priority Research Program of the Chinese Academy of Sciences (Grant XDA11010304),National Natural Science Foundation of China (Grants 41376019,41275084,and 41075059) (973 Program)

大气科学

OA北大核心CSCDCSTPCD

1006-9895

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