| 1. | Mld ; mean logistic delay
平均后勤延迟 |
| 2. | However , the space distribution and seasonal variability of mld obtained from different criteria are consistent with each other
尽管如此，三种定义下得到的mld的空间分布特征及季节变化规律却是大体一致的。 |
| 3. | Therefore , to find the suboptimum detection schemes which have low complexity as well as good performance close to mld is the main problem of mimo signal detection
因此,低复杂度、逼近mld性能的次优信号检测算法一直是mimo信号检测所要解决的问题。 |
| 4. | The mld of the ocean near the equator from 10 ? s to 10 ? n are less than 50 m and have no evident seasonal variability
而在10 s 10 n之间的赤道附近海域，因风应力和净热通量的季节变化不大，且该区降水量较大，浮力通量增加， mld较浅，低于50米，且没有明显的季节变化。 |
| 5. | This method is demonstrated by an example in water industry systems . 5 . optimization of n - removal in sewage treatment is accomplished by exploiting mixed logical dynamic method ( mld )
结果显示itl适合于建立水工业混杂实时模型，摘要而且它能表达混杂系统中的专家经验。 |
| 6. | The global climatological monthly mean data of the mixed layer depth ( mld ) supplied by levitus ( 1994 ) in nodc based on three different criteria , are used to analyze the space distribution and seasonal variability of mld
利用nodc提供的levitus ( 1994 )全球气候月平均混合层深度资料，分析了三种不同混合层深度定义下的混合层深度的空间分布特征和季节变化规律。 |
| 7. | When the effect of surface wave breaking is considered , mld is 50 cm deeper than that obtained without wave breaking , and with the enhancement of wind stress forcing , the deepening of mld is increased
模拟结果表明，当考虑波浪破碎的影响时，混合层深度比无波浪影响时的结果加深了约50cm ；随着风应力作用的增加，波浪破碎加强了混合层中的湍流混合，促使加深幅度也增加。 |
| 8. | Though maximum likelihood detection ( mld ) can obtain optimum detection performance in mimo communication systems , the ergodic search increases the complexity exponentially with the number of the antennas , which lead to implemental difficulty
在mimo通信系统信号检测中,最大似然检测( mld )可以获得最佳的误码性能,然而遍历式搜索方式使得mld的计算复杂度随天线数呈指数形式递增,在实际系统中,往往难以实时实现或者不能实现。 |
| 9. | It is found that mld based on a temperature change from the ocean surface of 0 . 5 degree celsius is deeper , especially from jan . to apr . , while mld based on a variable density change from the ocean surface with a temperature change of 0 . 5 degree celsius is shallower
分析表明，基于温度阶跃0 . 5得到的mld较深，尤其在1 4月，这可能主要是因为没考虑mld此时受到的盐度变化的影响；基于温差为0 . 5对应的密度定义的mld最浅。 |
| 10. | During the el nino ( la nina ) events , the negative ( positive ) sst anomaly occurs and the corresponding the olr mjo intensity weakens ( enhances ) in the tropical western pacific ; at the same time , the positive ( negative ) surface westerly anomaly leads to positive ( negative ) mld anomaly , and the corresponding sst mjo intensity weakens ( enhances ) in the equatorial eastern pacific , 4 ) the interdecadal variation of the atmospheric mjo intensity took place distinctly in 1970s in the tropical western , northwest and eastern pacific , with the stronger intensity in the former than the back stage , and the interdacadal variation of sst is its cause
Elnino ( lanina )事件中热带两太平洋sst出现负(正)异常， olr季内振荡强度出现减弱(增强)的变化。 elnino ( lanina )事件中，赤道太平洋出现地面信风西风分量正(负)异常，并引起热带东太平洋mld出现正(负)异常，造成热带东太平洋sst季内振荡强度出现减弱(增强)的变化。 4 )热带印度洋、热带西太平洋和热带东太平洋季内振荡强度在上世纪70年代发生了明显的年代际变化，均为前弱、后强， sst本身的年代际变化是其原因。 |
