冬季黑潮延伸体区域涡旋尺度海面温度季节内变化特征Intraseasonal Variation of Mesoscale Sea Surface Temperature in Kuroshio Extension Region During Winter
杨小绘,贾英来
摘要(Abstract):
利用ERA_interim再分析资料以及OISST高分辨率海面温度(Sea surface temperature,SST)卫星观测数据,通过小波分析、二维模态相关(Pattern correlation)等方法系统地分析了黑潮延伸体区域涡旋尺度SST信号的季节内变化特征。发现涡旋尺度SST季节内变化信号在冬季最强、夏季最弱。该信号主要分布在黑潮-亲潮海洋锋面区域,在日本沿岸振幅最强、并沿黑潮、亲潮锋面向东延伸,其标准差高达1℃,是该海域冬季SST的重要变化信号。涡旋尺度SST的季节内变化周期以40~100 d周期为主,会引起大气边界层的响应,激发海气界面湍流热通量、海面气温、边界层高度等同位相的季节内变化。在该区域涡旋信号较强个数较多的时间段SST异常的季节内变化信号更明显,边界层大气与涡旋尺度SST季节内变化信号的相关程度更大。
关键词(KeyWords): 黑潮延伸体;涡旋尺度海面温度;季节内变化特征;边界层大气
基金项目(Foundation): 国家重点基础研究发展计划项目(2017YFC1404101);; 国家自然科学基金项目(41975065)资助~~
作者(Author): 杨小绘,贾英来
DOI: 10.16441/j.cnki.hdxb.20190185
参考文献(References):
- [1] Kwon Y O,Alexander M A,Bond N A,et al.Role of the Gulf Stream and Kuroshio-Oyashio systems in large-scale atmosphere-ocean interaction:A review[J].Journal of Climate,2010,23(12):3249-3281.
- [2] Minobe S,Miyashita M,Kuwano-Yoshida A,et al.Atmospheric response to the Gulf Stream:Seasonal variations[J].Journal of Climate,2010,23(13):3699-3719.
- [3] Wang L,Li T,Zhou T.Intraseasonal SST variability and air-sea interaction over the Kuroshio Extension region during boreal summer[J].Journal of Climate,2012,25(5):1619-1634.
- [4] Li F,Sang H,Jing Z.Quantify the continuous dependence of SST-turbulent heat flux relationship on spatial scales[J].Geophysical Research Letters,2017,44:6326-6333.doi:10.1002/2017GL073695.
- [5] Namias J,Cayan D R.Large-scale air-sea interactions and short-period climatic fluctuations[J].Science,1981,214(4523):869-876.
- [6] Wallace J M,Smith C,Jiang Q.Spatial patterns of atmosphere-ocean interaction in the northern winter[J].Journal of Climate,1990,3(9):990-998.
- [7] Smirnov D,Newman M,Alexander M A.Investigating the role of ocean-atmosphere coupling in the North Pacific Ocean[J].Journal of Climate,2013,27(2):592-606.
- [8] Putrasahan D A,Kamenkovich I,Le Hénaff,et al.Importance of ocean mesoscale variability for air sea interactions in the Gulf of Mexico[J].Geophysical Research Letters,2017,44(12):6352-6362.
- [9] Ma J,Xu H,Dong C,et al.Atmospheric responses to oceanic eddies in the Kuroshio Extension region[J].Journal of Geophysical Research:Atmospheres,2015,120(13):6313-6330.
- [10] Chen L,Jia Y,Liu Q.Oceanic eddy-driven atmospheric secondary circulation in the winter Kuroshio Extension region[J].Journal of Oceanography,2017,73(3):295-307.
- [11] Ma J,Xu H,Dong C.Seasonal variations in atmospheric responses to oceanic eddies in the Kuroshio Extension[J].Tellus A:Dynamic Meteorology and Oceanography,2016,68(1):31563.http://dx.doi.org/10.3402/tellusa.v68.31563.
- [12] Ma X,Chang P,Saravanan R,et al.Importance of resolving Kuroshio Front and eddy influence in simulating the North Pacific storm track[J].Journal of Climate,2016,30(20):1861-1880.doi:10.1175/jcli-d-16-0154.1.
- [13] Chelton D B,Xie S P.Coupled ocean-atmosphere interaction at oceanic mesoscales[J].Oceanography,2010,23(4):52-69.doi:10.5670/oceanog.2010.05.
- [14] 马静,徐海明,董昌明.大气对黑潮延伸区中尺度海洋涡旋的响应——冬季暖、冷涡个例分析[J].大气科学.2014(3):438-452.Ma J,Xu H,Dong C.Atmospheric response to mesoscale oceanic eddies over the Kuroshio Extension:case analyses of warm and cold eddy in winter[J].Chinese Journal of Atmospheric Sciences,2014(3):438-452.
- [15] 陈隆京.冬季黑潮延伸体海区海洋涡旋对大气的影响[D].青岛:中国海洋大学,2017.Chen L.Impact of Oceanic Deey on Atmosphere in the Winter Kuroshio Extension Region[D].Qingdao:Ocean University of China,2017.
- [16] Frenger I,Gruber N,Knutti R,et al.Imprint of southern ocean eddies on winds,clouds and rainfall[J].Nature Geoscience,2013,6(8):608-612.
- [17] Villas B?as A B,Sato O T,Chaigneau A,et al.The signature of mesoscale eddies on the air-sea turbulent heat fluxes in the South Atlantic Ocean[J].Geophysical Research Letters,2015,42:1856-1862.doi:10.1002/2015GL063105.
- [18] Park K A,Cornillon P,Codiga D L.Modification of surface winds near ocean fronts:Effects of Gulf Stream rings on scatterometer (QuikSCAT,NSCAT) wind observations[J].Journal of Geophysical Research Oceans,2006,111(C3):11-19.
- [19] Tracey K L,Watts D R,Donohue K A,et al.Propagation of Kuroshio extension meanders between 143°E and 149°E[J].Journal of Physical Oceanography,2012,42(4):581-601.
- [20] Itoh S,Yasuda I.Characteristics of mesoscale dddies in the Kuroshio-Oyashio extension region detected from the distribution of the sea surface height anomaly[J].Journal of Physical Oceanography,2010,40(5):1018-1034.
- [21] Shan H,Dong C.Atmospheric responses to oceanic mesoscale eddies based on an idealized model[J].International Journal of Climatology,2019,39(20):1665-1683.doi:10.1002/joc.5908.
文章评论(Comment):
|
||||||||||||||||||
|
||||||||||||||||||