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1.
南海表层水温的季节内振荡   总被引:9,自引:2,他引:7  
采用谱估计和相关分析等方法分析了1985年夏半年的水文气象资料,证实南海表层水温存在季节内振荡,这种振荡在深水区与浅海区有着明显的差异。分析表明:南海水温季节内振荡与南海纬向风分量u的振荡密切相关。  相似文献   

2.
南海表层水温甚低频振荡的动力学机制   总被引:1,自引:1,他引:0  
用一个简单的海洋模式,研究了东亚季风异常对南海表层水温(SST)的影响,发现南海表层水温的甚低频振荡是东亚季风异常风应力强迫所致.这种甚低频振荡主要反映在深水区,其空间分布呈椭圆形,几乎与南海海盆形状一致。从海盆中央到边缘振幅逐渐减少,SST的甚低频振荡是非行进波,无明显传播特征。  相似文献   

3.
对南海季风实验(SCSMEX)期间布设于南海中部的3个ATLS海洋锚定浮标所观测的水温资料进行分析,结果表明:南海上层水温存在准双周(10-20d)变化,且主要发生在次表层,尤其在冬半年,温跃层的年循环对其有调制作用;次表层水温的振幅北部大于南部;南海上层的准双周振荡可分为3个垂向模态,即上下同位相、反位相、次表层先于表层;低层大气准双周振荡的强迫,是造成这种变化的主要原因,海面风应力强迫使得温跃层发生垂直位移,从而引起次表层水温的变化;表层水温(SST)的变化小于次表层,海面热收支是引起表层水温变化的主要原因,但次表层水温可以影响表层。  相似文献   

4.
南海表层水温场的时空特征与长期变化趋势   总被引:9,自引:0,他引:9  
本文利用月平均表层水温(SST)、850hPa经向风和西太平洋副热带高压等资料分析了南海表层水温距平(SSTA)场的时空特征和长期变化趋势,并探讨了SST的年际和长期变化原因.结果表明,南海SSTA场分别存在着以全域同位相振荡和东南一西北向反位相振荡的两个主要模态.其中,前者是主要模态,以年际振荡为主,而后者则是次要模态,以季节振荡为主.进一步分析发现,南海中部的SST存在着显著的年际和年代际变化,并在1981年前后发生了一次由低到高的气候转变,而且南海中部SST的长期变化趋势非常明显,在1950—2006年间增温0.92℃.相关和合成分析表明,南海SST的年际和长期变化可能是由南海上空的经向风异常和西太平洋副热带高压的纬向变动引起的.  相似文献   

5.
南海暖池初探(Ⅰ)   总被引:3,自引:0,他引:3  
南海暖池是西太平洋-南海-印度洋热库的重要组成部分。与SST比较,次表层水中表层至100m的垂直平均温度(TAV)是描述南海暖池特征的较好工具,因此采用TAV变化来讨论南海海温的时空变化特征。南海暖池有显著的季节和年际变化,其上层海洋热力结构年际变化与赤道西太平洋的变化趋势相反,是独立于“西太暖池”的暖水体。  相似文献   

6.
春夏季季风转换期南海南部的异常表层水   总被引:4,自引:4,他引:0  
对1985-1998年期间的海洋调查温盐深(CTD)资料进行综合分析,发现南海南部春夏季季风转换期存在盐度逆转的异常表层水。实测资料表明,该异常表层水覆盖在南海南部的中部、东部大部分地区。冬季风停止引起苏禄海高温高超国水西向侵入,成为该海区东部近表面异常高盐水的来源之一。海面强的蒸发和表层水弱的垂向混合导致近表面水具有高盐特性,近表面高盐水与其下部保持着冬季遗存的局地低盐水叠置,形成了盐度逆转现象。  相似文献   

7.
以南海夏季不同深度层次的各站位的温度,盐度,pH,O2,硝酸盐,亚硝酸盐,铵,磷酸盐,硅酸盐等水化学参数作为变量,实施Q型多维聚类分析,聚类分析结果表明,在垂直方向上,南海的水团可划分为南海表层水,南海次表层水,南海中层水,南海深层水和南海深海盆水等5种类型,聚类分析结果与温盐点聚图解所得的结论完全一致,南海夏季调查的多维聚类分析及T-S点聚图一致表明,南海的海水有着良好的成层结构,自海面至海底的水体运动自然形成了化学性质各异的五个水团。  相似文献   

8.
1998年夏、冬季南海水团分析   总被引:17,自引:2,他引:15  
为了解南海水团的特征和分布 ,基于 1 998年夏季和冬季两个航次的实测资料 ,采用聚类分析、判别分析和模糊分析方法 ,对南海的水团进行了分析。结果表明 ,南海外海水可划分为 6个水团 ,即南海表层水团、南海次表层水团、南海次 中层混合水团、南海中层水团、南海深层水团和南海底盆水。越南附近夏季存在一个暖涡 ;1 998年夏季还可鉴别出黑潮表层水团和黑潮次表层水团 ,但在冬季观测期间无黑潮水越过 1 1 9.5°E经线进入南海 ;这些现象可能与厄尔尼诺现象有关联。夏季有苏禄海海水在 5 0— 75m层经由民都洛海峡侵入南海  相似文献   

9.
调查海区的表层水可划分为四个变性水团,即南海北部沿岸水(NSCW)、南海太平洋表层水(SPSW)、泰国湾—巽他陆架一带表层水(SSSW)和南海中央表层水(CSSW).其中SPSW和SSSW属季节性水团,NSCW和CSSW终年存在。这些变性水团的消长变化与南海的季风密切相关.CSSW以南海中部为活动中心,在西南季风和东北季风的作用下,分别向南海北部和南部移动.SPSW和SSSW仅分别在冬半年和夏半年出现于调查海区的北部和西南部.NSCW的消长变化不但受到广东沿海江河径流量的制约,而且在东北季风潮期间还受到东海沿岸水的强烈影响。  相似文献   

10.
1998年夏、冬季南海的水团及其与太平洋的水交换   总被引:7,自引:4,他引:3  
根据 1998年夏季和冬季 2个航次的实测资料 ,对南海的水团进行划分和分析 ,并利用1997年 7月和 12月的实测资料 ,对巴士海峡 (吕宋海峡 )和民都洛水道附近的温盐分布进行分析。1998年冬季的资料分析结果表明 ,可将南海外海水划分为 6个水团 ,即南海表层水团 (S)、南海次表层水团 (U)、南海次 -中层混合水团 (UI)、南海中层水团 (I)、南海深层水团 (D)和南海底盆水(B)。 1998年夏季还可在南海中鉴别出黑潮表层水团 (KS)和黑潮次表层水团 (KU) ,但在冬季观测期间无黑潮水越过 119.5°E经线进入南海 ;夏季有苏禄海水在 5 0~ 75 m层经民都洛水道侵入南海。然而 ,1997年夏季和冬季的资料分析表明 :夏、冬两季都有大洋水通过吕宋海峡北段进入南海 ,南段有南海水流入太平洋。这些现象可能与 1998年前后的厄尔尼诺有关。  相似文献   

11.
本文在对位于黄海南部陆架上的朝连岛站30年水温资料进行分析时发现,该站的表层水温有周期大于20个月的低频振动,其中以准两年周期和6年周期最显著。陆架水温的这种低频振动是对东亚季风异常的响应。这种低频振动在冬季与渤海冰情的变化同步;在夏季与黄海底层冷水团的强弱相关。同时,这种低频振动在对马暖流上也有一定的反映。  相似文献   

12.
东海沿海季节性海平面异常成因   总被引:1,自引:0,他引:1  
Based on the analysis of sea level, air temperature, sea surface temperature(SST), air pressure and wind data during 1980–2013, the causes of seasonal sea level anomalies in the coastal region of the East China Sea(ECS) are investigated. The research results show:(1) sea level along the coastal region of the ECS takes on strong seasonal variation. The annual range is 30–45 cm, larger in the north than in the south. From north to south, the phase of sea level changes from 140° to 231°, with a difference of nearly 3 months.(2) Monthly mean sea level(MSL)anomalies often occur from August to next February along the coast region of the ECS. The number of sea level anomalies is at most from January to February and from August to October, showing a growing trend in recent years.(3) Anomalous wind field is an important factor to affect the sea level variation in the coastal region of the ECS. Monthly MSL anomaly is closely related to wind field anomaly and air pressure field anomaly. Wind-driven current is essentially consistent with sea surface height. In August 2012, the sea surface heights at the coastal stations driven by wind field have contributed 50%–80% of MSL anomalies.(4) The annual variations for sea level,SST and air temperature along the coastal region of the ECS are mainly caused by solar radiation with a period of12 months. But the correlation coefficients of sea level anomalies with SST anomalies and air temperature anomalies are all less than 0.1.(5) Seasonal sea level variations contain the long-term trends and all kinds of periodic changes. Sea level oscillations vary in different seasons in the coastal region of the ECS. In winter and spring, the oscillation of 4–7 a related to El Ni?o is stronger and its amplitude exceeds 2 cm. In summer and autumn, the oscillations of 2–3 a and quasi 9 a are most significant, and their amplitudes also exceed 2 cm. The height of sea level is lifted up when the different oscillations superposed. On the other hand, the height of sea level is fallen down.  相似文献   

13.
南海沿海季节性海平面异常变化特征及成因分析   总被引:1,自引:1,他引:0  
Based on sea level, air temperature, sea surface temperature(SST), air pressure and wind data during 1980–2014,this paper uses Morlet wavelet transform, Estuarine Coastal Ocean Model(ECOM) and so on to investigate the characteristics and possible causes of seasonal sea level anomalies along the South China Sea(SCS) coast. The research results show that:(1) Seasonal sea level anomalies often occur from January to February and from June to October. The frequency of sea level anomalies is the most in August, showing a growing trend in recent years. In addition, the occurring frequency of negative sea level anomaly accounts for 50% of the total abnormal number.(2) The seasonal sea level anomalies are closely related to ENSO events. The negative anomalies always occurred during the El Ni?o events, while the positive anomalies occurred during the La Ni?a(late El Ni?o) events. In addition, the seasonal sea level oscillation periods of 4–7 a associated with ENSO are the strongest in winter, with the amplitude over 2 cm.(3) Abnormal wind is an important factor to affect the seasonal sea level anomalies in the coastal region of the SCS. Wind-driven sea level height(SSH) is basically consistent with the seasonal sea level anomalies. Moreover, the influence of the tropical cyclone in the coastal region of the SCS is concentrated in summer and autumn, contributing to the seasonal sea level anomalies.(4) Seasonal variations of sea level, SST and air temperature are basically consistent along the coast of the SCS, but the seasonal sea level anomalies have no much correlation with the SST and air temperature.  相似文献   

14.
tn order to find the relationships between the flood and drought of the Changjiang and Huaihe River valleys and Pacific SST anomalies, the synoptic analysis Has been made. Two types of opposite distribution of SST departure for flood and drought years have been found. These states have set up basically preceding winter and have strengthened and persisted in summer.The time of the effect of anomalous SST on the flood and drought are different for different areas over the Pacific, the north Pacific is the earliest and the west and southeast Pacific are later. The evolution of SST anomalies with different types in every part of the Pacific has been shown. Finally, the formation of SST anomalies in Pacific has been elucidated by virtue of the surface wind anomalies which drive the ocean current anomaly.  相似文献   

15.
用Niiler—Kraus类型的混合层积分模式,对TOGA—COARE强化观测期间由《实验3号》科学考察船观测资料得到的混合层深度和SST在季节内时间尺度的变化进行了模式研究。指出:1.混合层耗散参数与较长时间尺度过程风应力的变化存在着比较好的对应关系;2.模式可以较好的对风场和热通量场在季节内时间尺度的变化作出响应,模拟出季节内时间尺度SST的变化;3.Niiler,-Kraus模式在考虑耗散作用后,可用于海洋季节内时间尺度变化的模式研究。  相似文献   

16.
Long-term monthly sea level and sea surface temperature (SST) anomalies from central California show that during winter months, positive anomalies are associated with El Niño events and the negative ones with La Niña events. There is no significant impact on monthly mean anomalies associated with Pacific decadal oscillations, although there is a tendency for more extreme events and greater variance during positive decadal oscillations. The very strong 1997–1998 El Niño was analyzed with respect to the long-term historic record to assess the forcing mechanisms for sea level and SST. Beginning in the spring of 1997, we observed several long-period (>30 days) fluctuations in daily sea level with amplitudes of over 10 cm at San Francisco, California. Fluctuations of poleward long-period alongshore wind stress anomalies (AWSA) are coherent with the sea level anomalies. However, the wind stress cannot entirely account for the observed sea level signals. The sea level fluctuations are also correlated with sea level fluctuations observed further south at Los Angeles and Tumaco, Columbia, which showed a poleward phase propagation of the sea level signal. We suggest that the sea level fluctuations were, to a greater degree, forced by the passage of remotely generated and coastally trapped waves that were generated along the equator and propagated to the north along the west coast of North America. However, both local and remote AWSA can significantly modulate the sea level signals. The arrival of coastally trapped waves began in the spring of 1997, which is earlier than previous strong El Niño events such as the 1982–1983 event.  相似文献   

17.
北太平洋海表温度及各贡献因子的变化   总被引:2,自引:0,他引:2       下载免费PDF全文
刘珊  王辉  姜华  金啟华 《海洋学报》2013,35(1):63-75
采用1958年1月至2007年12月SODA海洋上层温度的月平均资料,基于海温变化方程和统计分析方法,分析了北太平洋海表面温度(SST)异常特征及各局地因子贡献比例的变化。结果表明,伴随着1976/1977风场最强中心位置的南北移动,形成了两个北太平洋SST年际-年代际变化的异常中心:一个是位于30°N附近的副热带海盆内区,SST异常主要受风应力强度的主导;一个是位于40°N附近的副热带和副极地环流交汇区,SST异常主要受风应力旋度的位置即风场位置的影响。在副热带海盆内区,最强降温发生在1978-1982年,SST异常的主要局地贡献因子为海表热通量和经向平流,二者所占比例和约为50%~60%,均为同相增温或降温作用,余项所占比例约为20%~50%。在副热带和副极地环流交汇区,海盆内区和西部边界区的SST异常的跃变时间同为1975年,但是内区的垂直混合项的跃变时间早于西部5年左右。SST异常的主要贡献因子为海表热通量和经向平流,但在1983-1988年海温强降温期间,经向平流项贡献大于海表热通量项的贡献。两个区域的垂直混合项均为降温贡献,虽然量值小却显示出很强的年代际变化信号。平流项中经向平流最大,垂直平流最小。  相似文献   

18.
热带海洋SST与北半球大气环流的低频振荡特征   总被引:6,自引:2,他引:4  
采用复经验正交函数展开(CEOF)等方法研究了热带海洋海表温度异常(SSTA)和北半球500hPa高度场异常(H500)的甚低频(LF)和准两年(QB)两种低频振荡空间振幅和位相变化,发现SSTA变化信号在热带西太平洋最先出现,其后是热带中东太平洋,最后是热带中东太平洋,最后是热带印度洋和南海。副热带中西太平洋H500滞后于中东太平洋SSTA 1 ̄2月,H500的LF分量从副热带中西太平洋经西北太  相似文献   

19.
郑建  刘秦玉 《海洋与湖沼》2010,41(6):799-806
根据英国Hadley气候中心的海表温度资料和美国NCEP/NCAR中心的大气资料,研究了热带太平洋与热带大西洋海表温度主模态的相互作用。热带太平洋的ENSO可以导致大西洋Nino模态或经向偶极子模态,这主要是通过热带海洋-大气相互作用,或大气的太平洋-北美遥相关过程实现的。大西洋Nino模态的暖(冷)位相会导致赤道中东太平洋的海表温度降低(升高)。这可能是通过两种途径完成的:一种可能是大西洋Nino使印度洋增暖(变冷),进而引起赤道中太平洋的东(西)风异常,通过海洋-大气相互作用正反馈机制能发展成为La Nina(El Nino),使赤道东太平洋海温降低(升高);另一种可能是大西洋Nino直接可以导致太平洋Walker环流增强(减弱),从而使赤道东太平洋海温降低(升高)。  相似文献   

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