koe

Further magnetic measurements reveal that the nanotube array shows no anisotropy , the coercivity and squareness ratio are about 1 kOe and 0.37 .

进一步的磁性测量表明，纳米管阵列无明显的各向异性，其矫顽力约1kOe，磁滞回线的方形度约0.37。

On the other hand , the wind stress curl anomaly also strengthens the subpolar gyre so as to cool the Kuroshio / Oyashio Extension region ( KOE ) .

另一方面该风应力旋度变化也可增强副极地海洋涡旋，从而引起黑潮及其续流区（KOE）海温降低。

The magnetization of the sample is saturated for fields higher than 2 kOe at 300 K. In our experiment , a maximum remnant magnetization is observed in samples with 5 mol % Mn .

在300K的温度下磁场强度高于2k0e时，样品的磁化强度达到饱和，当Mn原子的摩尔比为5%时出现最大剩磁强度。

In the KOE region , the vertical advection , heat flux and horizontal advection anomalies are all important in producing the regime shift and the horizontal advection anomalies were found crucial for the time of the regime shift .

在KOE区，垂直平流、热通量和水平平流三者都起了重要作用，其中水平平流异常对这一区域海温年代际跃变出现的时间起了至关重要的作用。

The room temperature Mssbauer spectrum of this alloy consists of seven ferromagnetic and one paramagnetic sextet superposition . The seven ferromagnetic spectra belong to α 1 phase in the alloy , the magnitude of their internal magnetic field is 309 kOe .

在室温下，该合金的穆斯堡尔谱可以分解为八套亚谱，其中7个铁磁性亚谱属于合金中脱溶的α1相，它的平均超精细磁场约为309kOe；

Since the anomaly of the subpolar gyre is found persisting longer than that of the subtropical gyre , the negative SST anomaly in the KOE region is thus more prominent than the positive SST anomaly in the Kuroshio region .

其中副极地海洋涡旋异常持续时间要比副热带海洋涡旋长，因此KOE区海温负异常持续时间长于黑潮及其东面区域的海温正异常，强度也要显著。

The temperature dependence of resistance presents a smooth metal - insulator transition far below the magnetic transition , and the MR monotonically increases with decreasing temperature under 8 kOe field , both of which are related to the structural defects in the films including grain boundaries and porosity .

薄膜的电阻－温度关系具有平缓的金属－绝缘体转变，转变温度远低于其居里温度；在8kOe磁场下，薄膜的磁电阻随温度下降而单调上升。

When the westerly wind stress anomaly is prescribed maintaining for a decade , the cooling of the KOE region induced by the subpolar gyre anomaly is subsequently able to influence the central North Pacific , accordingly maintaining the initial negative SST anomaly over there .

在西风应力异常持续10年的情况下，副极地海洋涡旋异常导致的KOE区负海温异常还可以影响到北太平洋中部，因而对北太平洋中部海温的负异常起着维持的作用。