1) subsurface water
次表层水
1.
Results were shown that,subsurface water mostly comes from the North Pacific while the intermediate water originates from both the North and South Pacific Ocean,even possibly from the Indian Ocean.
分析结果表明,ITF的次表层水源主要来自北太平洋,中层水源地既包括北太平洋、南太平洋,同时也不能排除有印度洋的可能性。
2) subsurface warm water
次表层暖水
1.
The subsurface warm water has been observed frequently in the summer ice-free sea area of the Arctic Ocean, that is, a temperature maximum occurred in water depths of 20 to 50 m.
在夏季北冰洋的无冰海域,经常可以观测到次表层暖水现象,即在水深20～50m的范围内发生海水温度的极大值。
3) subsurface ocean temperature anomaly(SOTA)
次表层水温
1.
To study the relation between the subsurface ocean temperature anomaly(SOTA)of the equatorial western Pacific Warm Pool and the tropical cyclone(TC),the impact of TC has done a Statistical analysis using observed data.
为探索赤道西太平洋暖池次表层水温异常与热带气旋的关系,用赤道西太平洋暖池和南海SOTA实测资料,对TC的影响做了统计分析,结果表明:赤道西太平洋暖池SOTA与同步西太平洋TC个数不存在线性相关;赤道西太平洋暖池1月SOTA滞后5-7个月影响西太平洋的TC;赤道西太平洋暖池区1月的SOTA出现正(负)距平值时,当年西北太平洋和南海的TC生成时间比常年提早(推迟)是主要现象,极值年份尤其明显,当年夏季西北太平洋副热带高压偏弱(强),位置偏北(南),西太平洋暖池区上空对流加强(减弱),对台风生成有(不)利,台风生成平均位置偏西(东),TC的个数偏多(少)、偏强(弱),易于出现西行(东北转向)路径为主;南海中北部2月SOTA出现偏暖(冷)年,当年南海TC生成日期偏早(晚)、数量偏多(少)、偏强(弱)是主要现象。
4) subsurface high-salinity water types
次表层高盐水类型
5) subsurface
[英]['sʌb'sə:fis] [美]['sʌb,sɚfəs, sʌb'sɚ-]
次表层
1.
Variations of surface and subsurface heat contents in Indian Ocean and their relationship to ENSO based on SODA data;
基于SODA数据的印度洋表层和次表层热含量变化及其与ENSO的关系
2.
Under larger current,such as 50A,the recrystallization layer appears obviously in the subsurface,causing large tensile stress between the subsurface and the surface w.
在较大电流(50A)作用下,合金次表层中会产生明显再结晶层,与表面未再结晶层之间存在较大拉应力,从而促进磨损裂纹的萌生和扩展,加速磨损过程。
3.
The content of dissolved trace metals (Cu, Pb, Zn, Cd) in the surface microlayer and subsurface water in the Nansha region was determined.
对南沙海区微表层和次表层中溶解态痕量金属铜、铅、锌、镉的含量进行了测定，并探讨了其与ＤＯＣ的关系。
6) sub-surface
次表层
1.
Examining and analyzing of the glassy carbon surface and section which suffered oxidation for different time, results show that the oxidizing behavior of glassy carbon begins from the sub-surface instead of the normal surface, which resulted by the different state of stress between the matrix and the surface.
利用SEM对经不同氧化所得到的玻璃碳表面和截面进行观察和分析 ,结果表明玻璃碳的氧化行为并不是从最外表面开始 ,而是从次表层进行 ,基体与表层的不同应力状态导致了这种特别的氧化行
补充资料：十字水期韦潘侍御同年不至,时韦寓居水次故
【诗文】：
伊水溅溅相背流，朱栏画阁几人游。漆灯夜照真无数，
蜡炬晨炊竟未休。顾我有怀同大梦，期君不至更沈忧。
西园碧树今谁主，与近高窗卧听秋。
【注释】：
【出处】：
全唐诗：卷540-75
伊水溅溅相背流，朱栏画阁几人游。漆灯夜照真无数，
蜡炬晨炊竟未休。顾我有怀同大梦，期君不至更沈忧。
西园碧树今谁主，与近高窗卧听秋。
【注释】：
【出处】：
全唐诗：卷540-75
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