ssw中文是什么意思

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用"ssw"造句"ssw"怎么读"ssw" in a sentence

中文翻译手机版

南南西
南西南

"ssweet spring" 中文翻译 : 甜春
"ssv" 中文翻译 : 超亮炫丽液晶屏; 猴肉瘤簿; 斯库尔曼-施瓦茨簿; 索广映像有限公司
"sswf" 中文翻译 : 应测器超音波防尘机构
"ssuzhen" 中文翻译 : 白素贞
"sswid" 中文翻译 : 地下盐水注入和处置
"ssuyuanyakuo" 中文翻译 : 哑口
"sswind" 中文翻译 : 左冷蟾
"ssuyuan" 中文翻译 : 思源垭口
"sswws" 中文翻译 : 海啸警报系统
"ssutu" 中文翻译 : 司徒

例句与用法

Annual data collection form of ssw
学校社会工作年度资料收集表
Secondly , i studied the climate and it ' s abnormity character of strong ssw
其次，对强ssw的气候及异常特征进行了分析研究。
The main coupled mode of ssw and sst in the tropical pacific - south china sea - tropical indian ocean on interannual time scale
印度洋海面风与海面温度年际变化整体耦合的主模态
4 ) the occurring source of the strong ssw event had strong regional character . the northeast land of europe - asia was the region which strong ssw occurred most frequently
4 )强ssw事件发生源地有较强的地域性，欧亚大陆的东北部是发生源地最为频繁的地区。
2 ) the appearance frequency of strong ssw event had obvious interannual change . from the 1970s to 1980s it happened frequently , average 1 times per year . but from the 1990s it happened less , 0 . 42 times per year
2 )强ssw事件发生频数存在明显年代际变化，上世纪70年代和80年代为高发阶段，平均发生频数为1 . 0次年， 90年代起为低发阶段，发生频数下降为0 . 42次年。
The strike - slip faulting was caused by asymmetrical distribution of barriers on the subducting plate . the nne - ssw distributed aftershocks occurred on , or near , the fault plane of the main shock ; while the nw - se distributed aftershocks , on , or near , the mentawai fault
北北东?南南西向分布的余震发生在主震的断层面上(或其附近) ；而西北?东南向分布的余震则发生在明打威断层上(或其附近) 。
3 ) the upper air stream circumstances along with strong ssw event mainly was separated to three kinds : the northern advance of aleutian high pressure , the northern advance of north atlantic high pressure , the northern advance of aleutian high pressure and north atlantic high pressure at the same time . their final effect was to make polar region vortex collapse and to increase polar region temperature
3 )伴随强ssw事件的高空环流形势主要有3种：阿留申高压北进，北大西洋高压北进，北大西洋高压和阿留申高压共同北进，它们的最终效果是使极涡崩溃、极区增温。
According to the analysis of the structure deformation variant direction the structure superposition during late period , and the tectonic stress field and deformation variant field , the cover extended nearly sn direction in early stage ( d - c ) , maybe changed the direction in pernian ( especial the late permian ) , and developed some new half - graben along sn direction except the succession activity at great fault zone . the direction of compression deformation variant , however , was nearly sn direction in indo - chinese epoch , ne - sw direction in early yanshan movement epoch , nne - ssw direction in late yanshan movement epoch , and transformed from ew to sn direction in himalayan movement epoch
根据不同构造层中变形方向及后期构造叠加的分析，对本区的构造应力场及变形场进行了探讨，本区盖层早期阶段( d - c )为近南北向的伸展拉张，二叠纪(特别是晚二叠世)的伸展方向可能发生了改变，除在各断裂带继承性活动外，沿南北方向又新生了一些半地堑。而在挤压变形时，印支期主要为近南北向挤压，燕山早期为nw - se向挤压，燕山晚期为nne - ssw向挤压，而喜山运动可能经历了从ew向向sn向方向挤压的转变。
At first , according to the definition of wmo , i gave the index to identify strong ssw event , and by which , i had a systemic statistic on the day - by - day temperature , air pressure , wind field in the stratosphere from january to march during the period of 1950 - 2002 . finally , i got 35 strong ssw events . comparing these with labitake " s research result , i found the index and process are rational
首先，根据世界气象组织定义，给出了识别强ssw事件发生的指标，用它对1950 ? 2002年1 ? 3月期间平流层大气逐日温、压、风场进行了系统的统计，共得到35次强ssw过程，并将其与labitzke研究结果进行比较，证明了所定指标及过程的合理性。