1) African monsoon
非洲季风
1.
We studied the variability of the African monsoon and the Mediterranean sea surface productivity during the early Pliocene based on the analysis of some paleoenvironment proxies such as planktonic foraminifera oxygen isotope and biogenic compositions(carbonate,biogenic opal and organic carbon) in three profiles respectively,Punta Piccola,Cape Spertivento and Punta Rossello in southern Italy.
主要研究了意大利上新统3个剖面Punta Piccola、Cape Spertivento以及Punta Rossello蛋白石含量的变化,综合其它古环境指标对非洲季风和地中海表层生产力加以分析,研究表明,PuntaPiccola剖面和Cape Spertivento剖面各古环境指标对岁差周期影响的响应明显而单纯,即岁差低值,对应氧同位素偏负,有机碳和蛋白石高值以及碳酸盐低值,说明地中海表层生产力明显受到岁差的驱动。
2) Asian summer monsoon
亚洲季风
1.
The relationship between the location change of the East Asian subtropical westerly jet(EASWJ) and Asian summer monsoon onset is investigated by using NCEP/NCAR pentad mean reanalysis data.
利用1961～2000年的NCEP/NCAR候平均再分析资料,初步探讨了季节转换期间东亚副热带西风急流南北和东西向位置变化与亚洲季风爆发之间的联系。
2.
By use of IAP9 AGCMⅡ, a numerical experiment is made, in which the influence of the south west Indian Ocean SSTA on the outbreak of the Asian summer monsoon has been discussed.
试验结果表明 ,当该海域 1～ 3月份的海温出现异常增暖时 ,印度夏季风和东亚夏季风的爆发均较平常晚 ,反之 ,二者的建立均较平常早 ;该海域 1～ 3月份的海温异常对亚洲季风区的降水也有明显的影
3) Asian monsoon
亚洲季风
1.
The spatial and temporal distribution features of onset period of mean rainy season over Asian monsoon region;
亚洲季风区平均雨季起始期的时空分布特征
2.
The variations of Asian monsoon as revealed by the variations of kinetic energy of barotropic/baroclinic modes of the wind field;
亚洲季风变动与大气正压/斜压运动动能变化的气候特征
3.
Thrusts and prospects on understanding and predicting Asian monsoon climate.;
认识和预报亚洲季风气候:前沿突破点和展望
4) Asian summer monsoon
亚洲夏季风
1.
Interannual and interdecadal variations of moisture transport by Asian summer monsoon and their association with droughts or floods in China;
亚洲夏季风水汽输送的年际年代际变化与中国旱涝的关系
2.
Roles of tropical and subtropical land_sea distribution and the Qinghai-Xizang Plateau in the formation of the Asian summer monsoon;
热带、副热带海陆分布与青藏高原在亚洲夏季风形成中的作用
3.
The snow cover on the Tibetan Plateau has obvious seasonal,interannual and interdecadal changes,and is one of the most important factors which control the Asian summer monsoon precipitation.
青藏高原(以下简称高原)积雪具有明显的季节、年际和年代际变化特征,是影响亚洲夏季风降水的重要因子之一。
5) Asian monsoon region
亚洲季风区
1.
Results show that: (1) The zonal-mean moisture transport in Asian monsoon region is unique because of the monsoon activities.
利用1948—2005年NCEP/NCAR逐日及月平均资料,研究了亚洲季风区水汽输送的气候特征及其与中国夏季降水的关系。
2.
The impact of the diurnal variation of the surface heating in the Tibetan Plateau on the circulation over the Asian monsoon region is analyzed using the twice daily NCEP data from 1982 to 1996.
利用1982～1996年每天两次的NCEP再分析资料,研究青藏高原地面加热场的日变化对亚洲季风区环流的影响。
6) Asian Winter Monsoon
亚洲冬季风
1.
Using the CCM3/NCAR,a series of numerical experiments are designed to explore the ocean-land interlaced distribution of Africa—Arabian Sea(AS)—India Peninsula—Bay of Bengal(BOB)—Indochina Peninsula-South China Sea(SCS) on the formation of the Asian Winter Monsoon circulation.
利用美国国家大气研究中心研制的第三代公共气候模式CCM3/NCAR,设计了一系列数值试验,研究非洲大陆、印度半岛、中南半岛与其周围的阿拉伯海、印度洋和孟加拉湾及南海海陆交叉分布对亚洲冬季风环流形成的重要作用。
补充资料：季风(见季风气候)
季风(见季风气候)
j!feng候季风见季风气
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