1) A dipole VIMT anomaly
偶极型水汽输送异常
2) poleward moisture transport
向极地水汽输送
4) Water vapor transport
水汽输送
1.
Atmospheric water vapor transport from westerly and monsoon over the Northwest China;
西风带与季风对中国西北地区的水汽输送
2.
Based on the NCEP/NCAR reanalysis data,atmospheric water vapor transport is explore.
根据地面气象站观测资料,分析1961—2004年青南高原汛期降水变化的区域特征,并依据NCEP/NCAR再分析资料分析了典型多雨和少雨年份的大气水汽输送。
3.
It is found that the water vapor transportation concentrates in summer,the westerly is the main carrier,the Atlantic,the Arctic Ocean,the Black Sea and the Caspian Sea are the main water vapor sources,and the most part of the water vapor transported to Northwest China continuously moves eastwards and exports across the east side.
5°)再分析逐月资料,分析了我国西北地区的水汽输送和收支的平均状况。
5) moisture transport
水汽输送
1.
The results show that the occurrence of the heavy rains is mainly induced by the abnormity of atmospheric circulation, moisture transport, over-mightiness of southwest monsoon, and that the water vapor of the rainy zones mainly comes from the regions from the Arabian Sea to the Bengal Gulf and from the north Pacific Oc.
结果表明:暴雨出现与大气环流异常以及水汽输送、西南季风的异常偏强有关;暴雨区的水汽来源于阿拉伯海至孟加拉湾及北太平洋至中国南海地区。
2.
The July-August Asian monsoon moisture transport and its relationship with the rainfall over North China have been investigated using NCEP/NCAR monthly mean reanalyses and precipitation data of 160 stations in China over 1951-2005.
利用1951~2005年NCEP再分析资料和中国160站月降水资料,分析了华北汛期水汽输送的时空特征及其与降水的关系,发现不同水汽通道对华北降水的影响区域不同。
3.
The daily moisture transport flux(Q)calculated by using NCAR/NCEP reanalyzed data from 1950 to 2004 and the monthly mean moisture transport flux are used to analyze the characteristics of moisture transport over Asian-Australian monsoon region.
用1950-2004年NCAR/NCEP再分析资料计算得到逐日垂直积分水汽输送通量矢量Q,然后进行月平均处理,分析了亚澳季风区的水汽输送特征。
6) Water vapor transportation
水汽输送
1.
The characteristics of water vapor transportation over China and its relationship with precipitation anomalies in the Yangtze River Basin are analyzed by using the observed data in China and ECMWF reanalysis data from 1981 to 2002 in summer.
利用中国地区1981-2002年的常规观测资料和ECMWF再分析资料,研究了中国地区水汽输送的异常特征、水汽输送异常与长江流域降水的关系及其环流特征。
2.
Using the sounding and ground-based observational data in the east and nearby area of Tibetan Plateau and ECMWF reanalysis data from 1981 to 2002 in summer, with many diagnostic methods, first, we analyzed the water vapor transportation characteristics in summer in the east and nearby area of Tibetan Plateau.
利用青藏高原东部及其邻近地区1981年—2002年22年探空资料、地面观测资料、ECMWF再分析资料,使用多种诊断方法,首先分析了青藏高原东部及其邻近地区夏季水汽输送的基本特征,然后研究了水汽输送异常的年际变化特征及相应的大气环流异常特征,最后讨论了水汽输送异常与长江流域降水异常之间的关系,并深入分析了青藏高原东部水汽变化对长江流域降水的影响。
3.
Based on the drought strength index the periodic change of drought strength and frequency distribution were analyzed,and contemporary relationship between the variation of summer drought strength and water vapor transportation anomalies were also analyzed.
在此基础上分析了干旱强度的周期变化和频率分布特征,以及夏季干旱强度变化与同期水汽输送异常的联系。
补充资料：“质子-电子偶极-偶极”质子弛豫增强
“质子-电子偶极-偶极”质子弛豫增强
物理学术语。原子核外层中不成对的电子质量小，但磁动性很强，可使局部磁场波动增强，促使氢质子弛豫加快，从而使T1和T2缩短，这种效应即为PEDDPRE。过渡元素和镧系元素大部分在d和f轨道有多个不成对电子，所以其离子往往具有PEDDPRE，可用来作顺磁性对比剂，如钆(Gd)。Gd在外层有7个不成对电子，具有很强的顺磁性。
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