1) minus-SSTA
负距平海温异常
1.
This study investigates the influences of the minus-SSTA over the northern Pacific Ocean in the mid-latitudes in Summer of 1993 on the subtropical anticyclone by using the T42L9 global circulation spectral model developed by the IAP/CAS.
数值试验结果表明:(1)中纬度地区负距平海温异常对其南侧太平洋副热带高压的形态和脊线位置都有影响,负距平海温异常试验的500hPa副热带高压的形态明显比气候平均海温试验更接近于NCEP资料实况,对流层中下层副热带高压脊线的平均位置也比气候平均海温试验要偏南,与实况比也更接近了;(2)在500hPa上,北太平洋中纬度负距平海温异常在其南侧产生的高度扰动使副热带高压向南偏移,而在其北侧产生的高度扰动则沿北太平洋中高纬度、北美中高纬度、北大西洋和欧洲南部以及地中海和北非地区的大圆路径传播,并影响和改变整个北半球大气环流的变化。
2) sea surface temperature anomaly
海温异常
1.
It is found that waters within 5°S-5°N,60°-75°E are the key areas of sea surface temperature anomaly(SSTA) that affect the winter temperature of these regions from Apri.
利用近40a全球海温、500hPa高度场、300hPa纬向风场和海平面气压场月平均资料以及大连地区冬季的气温资料,分析了大连地区冬季气温异常的变化特征,探讨了大连地区冬季气温异常与前期印度洋海温异常的相互联系。
2.
The composites for circulation anomaly and sea surface temperature anomaly(SSTA) show that both the low .
对比分析旱涝月的环流异常和海温异常 (SSTA)发现 ,南海地区SSTA和对流层低层经向风异常均与长江中下游旱涝显著相关 ,尤其正SSTA和涝月的关系更为密切 ,因此南海SSTA为我国长江中下游地区旱涝的一个强讯号。
3.
More attention was paid on studying the relationship between sea surface temperature anomaly (SSTA) over the north Pacific and summer precipitation anomaly in North China and an AGCM was utilized to con.
为了揭示华北夏季降水异常规律及其成因，本文详细分析了华北夏季降水的气候特征及有关的环流特征、水汽输送特征和向外长波辐射(OLR)特征，着重研究了北太平洋海温异常与华北夏季降水异常的关系，并应用大气环流模式初步验证了北太平洋海温异常对华北夏季降水的影响。
3) SST anomaly
海温异常
1.
The important effects of SST(SST heating and SST anomaly) on low-frequency oscillation systems in tropics are studied by baroclinic equation groups for the characteristics of strong evaporation,convergence ascending and SST anomaly in the tropics.
根据热带地区蒸发、辐合上升运动剧烈以及海温异常的特点,构造了一个斜压模式方程组,讨论了海表温度(海温加热和海温异常变化)对热带低频波动的影响。
2.
In order to study the effects of SST anomaly in tropical western Pacific during winter and spring on the early summer monsoon in East Asia, a set of numerical experiments is conducted using OSU AGCM.
用ＯＳＵ的两层大气环流模式进行了热带西太平洋冬春海温异常对东亚初夏（５月）季风环流影响的数值试验。
3.
Using a primitive equation model with a spheric band domain,a numerical study iscarried out of the effect on rainfall of 1991 Pacific SST anomaly in the leading region with theaffecting mechanisms investigated.
利用球圈范围的初始方程模式，就１９９１年太平洋主要海温异常区对降水的影响进行了数值试验，并对影响机制进行了讨论。
4) SSTA
海温异常
1.
ANOMALIES OF THE NORTHEAST CHINA FLOODS SEASON PRECIPITATION AND SVD ANALYSIS WITH SSTA IN WORLD OCEANS;
东北地区汛期降水与全球大洋海温异常关系的SVD分析
2.
Mechanism for SSTA Impact on Summer Rainfall in North China;
热带海温异常影响华北夏季降水的机制研究
3.
Relationship of the SSTA Temporal Variation in the Middle and East Equatorial Pacific in Spring and Summer to East Asia Summer Monsoon;
春夏季赤道中东太平洋海温异常变化与东亚夏季风关系的研究
5) SST anomalies
海温异常
1.
Waters bounded by 9-1°S, 121-129°E are the key zones of SST anomalies that affect the precipitation in these regions over May - July in preceding years.
影响江南汛期降水的海温异常关键区位于9～1°S,121～129°E,关键影响时段为前一年的5～7月。
6) sea surface temperature anomalies
海温异常
1.
In 1985, negative sea surface temperature anomalies(SSTA) distributed in the eastern equatorial Pacific broadly, and positive SSTA which were about 0.
本文应用中国科学院大气物理研究所的两层大气环流模式（ＩＡＰ－ＡＧＣＭ），分别以观测得到的１９８５年赤道东太平洋和赤道西太平洋月平均海表温度场为外强迫源进行了两个区域海温异常的敏感性试验，分析了造成１９８５年夏季华南、华中和江淮流域干旱，而华北多雨的原因。
2.
By using the atmosphere-land coupled model IAP9L_CoLM of the Institute of Atmospheric Physics,Chinese Academy of Sciences,the imapct of sea surface temperature anomalies(SSTAs) in different ocean basins on the extreme climate events affecting Southern China during January 2008 has been investigated through four sets of ensemble numerical simulations.
利用中国科学院大气物理研究所陆气耦合模式IAP9L_CoLM,通过4组集合模拟试验,分别考察了不同海域的海温异常对2008年1月中国南方极端气候异常的可能影响。
补充资料：枕山负海
1.见"枕山襟海"。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条