1) East Asian summer paleomonsoon
东亚古夏季风
2) East Asia summer monsoon
东亚夏季风
1.
Wave-packet propagation feature of East Asia summer monsoon in 1998;
1998年东亚夏季风波包传播特征研究
2.
On the basis of analyzing the relationship between the setting of the East Asia summer monsoon over the South China Sea(the South China Sea monsoon) and the outbreak of harmful algal bloom over the East China Sea, the result of analyses shows that over three weeks after the South China Sea monsoon breaks out, the harmful algal bloom will occur over the East China Sea.
通过分析东亚夏季风在南海的爆发(南海夏季风)与东海赤潮之间的关系,发现南海夏季风爆发后的1～3周内,东海有一次赤潮过程。
3.
East Asia summer monsoon has a distinct interannual variability,and the external forcing is one of main causes resulting in the interannual difference of East Asia summer monsoon,but the effect of the tropical sea surface temperature is the most prominent.
4区的海温异常变化和高低空纬向风垂直切变之间的关系,发现海温异常变化与东亚夏季风的环流场之间也有很好的关系。
3) East Asian summer monsoon
东亚夏季风
1.
Features of interdecadal changes of the East Asian summer monsoon and similarity and discrepancy in ERA-40 and NCEP/NCAR Reanalysis;
东亚夏季风年代际变化的若干重要特征及两份大气再分析资料的异同
2.
Recent progresses of studies on influence of ENSO on the East Asian summer monsoon and China summer rainfall;
ENSO对东亚夏季风和我国夏季降水的影响研究进展
3.
Abrupt Character of the East Asian Summer Monsoon Recorded in the Annual Layer Thickness of Stalagmites During the Last Deglaciation;
末次冰消期东亚夏季风突变性的石笋年纹层记录
4) East-Asian summer monsoon
东亚夏季风
1.
A nonlinear projection of the East-Asian summer monsoon onto the summer precipitation over China was performed by applying a neural-network-based nonlinear canonical correlation analysis method(NLCCA).
运用一种基于人工神经网络的非线性典型相关分析方法(NLCCA),对中国夏季降水与东亚夏季风之间的非线性关系进行了分析。
5) the East Asian summer monsoon
东亚夏季风
1.
,the South Asian summer monsoon(SASM) over area(0°-25°N,60°E-100°E) and the East Asian summer monsoon(EASM) over area(0°-45°N,100°E-140°E) in boreal summer,and the North Australian summer monsoon(NASM) over area(0°-15°S,110°E-150°E) in austral summer,are investigated by using the ERA-40 daily reanalysis data,the NCEP/NCAR daily reanalysis data and the Climate Predicti.
利用1979~2002年的ERA-40和NCEP/NCAR逐日再分析资料以及CMAP降水资料探讨了亚澳季风各夏季风子系统(南亚夏季风、东亚夏季风、北澳夏季风)水汽输送的气候学特征及其与夏季降水的关系。
2.
,the South Asian summer monsoon(SASM) over the area(0°-25°N,60°E-100°E) and the East Asian summer monsoon(EASM) over the area(0°-45°N,100°E-140°E) in boreal summer,and the North Australian summer monsoon(NASM) over the area(0°-15°S,110°E-150°E) in austral summer,are respectively investigated.
利用1979~2003年的NCEP/NCAR再分析资料探讨了亚澳季风各夏季风子系统(南亚夏季风、东亚夏季风、北澳夏季风)流场结构及其季节演变的气候学特征。
3.
The interannual and interdecadal variations of the northerly wind system circulating around the west side of the Tibetan Plateau and their relation to the East Asian summer monsoon and the summer rainfall in North China are analyzed from the observed data.
从观测资料分析了青藏高原西侧绕流偏北风系的年际和年代际变化及其与东亚夏季风和华北地区夏季降水的关系。
6) East Asian paleomonsoon
东亚古季风
补充资料：风穴延沼禅师《释氏稽古略》
【风穴延沼禅师《释氏稽古略》】
汝州风穴禅师。讳延沼。钱塘余杭人。姓刘氏幼不茹荤。习儒应进士。一举不第乃出家。依本州开元寺智恭披剃。受具习天台止观。年二十五谒镜清。参南院颙禅师悟旨。依止六年辞去。后唐明宗长兴二年至汝水。草屋数椽依山如逃亡家。问之父老。田父曰。古风穴寺世以律居僧物故众弃去。师曰。我居之可乎。父曰可师乃留止。日乞村落。夜然松脂单丁者七年。至是天福二年州牧李使君闻师之道尽礼致之。上元日开堂说法。禀嗣南院颙。汉隐帝乾祐二年李君移守郢州。师避寇往依之馆于郡斋。汝州有宋太师者施第为宝坊号新寺。延师住持。法席雄冠。周太祖广顺元年。赐其寺额曰广慧。师住二十二年。当余百众。僧问如何是佛。师曰。杖林山下竹筋鞭。宋太祖开宝六年八月旦日。登座说偈曰。道在乘时须济物。远方来慕自腾腾。他年有叟情相似。日日香烟夜夜灯。至十四日手书别诸檀越。十五日跏趺而逝。寿七十八。夏五十九。师嗣南院颙。颙嗣兴化奖。奖嗣临济玄禅师
汝州风穴禅师。讳延沼。钱塘余杭人。姓刘氏幼不茹荤。习儒应进士。一举不第乃出家。依本州开元寺智恭披剃。受具习天台止观。年二十五谒镜清。参南院颙禅师悟旨。依止六年辞去。后唐明宗长兴二年至汝水。草屋数椽依山如逃亡家。问之父老。田父曰。古风穴寺世以律居僧物故众弃去。师曰。我居之可乎。父曰可师乃留止。日乞村落。夜然松脂单丁者七年。至是天福二年州牧李使君闻师之道尽礼致之。上元日开堂说法。禀嗣南院颙。汉隐帝乾祐二年李君移守郢州。师避寇往依之馆于郡斋。汝州有宋太师者施第为宝坊号新寺。延师住持。法席雄冠。周太祖广顺元年。赐其寺额曰广慧。师住二十二年。当余百众。僧问如何是佛。师曰。杖林山下竹筋鞭。宋太祖开宝六年八月旦日。登座说偈曰。道在乘时须济物。远方来慕自腾腾。他年有叟情相似。日日香烟夜夜灯。至十四日手书别诸檀越。十五日跏趺而逝。寿七十八。夏五十九。师嗣南院颙。颙嗣兴化奖。奖嗣临济玄禅师
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