geostrophic [,dʒi(:)əu'strɔfik]

geostrophic的基本解释

adj.

因地球自转而引起的, [气]地转风的

与geostrophic相关的网络例句 [注：此内容来源于网络，仅供参考]

The scale analysis on planetary scale motion in the tropical atmosphere shows that the equilibrium between the pressure gradient force and Coriolis force in the meridional direction is easily established, which is known as the zonally semi-geostrophic motion The semi-geostrophic adaptation process in which the inertial gravity waves play an important part is relatively quick The evolution process after the semi-geostrophic adaptation process is slow and controlled by the Kelvin waves and long Rossby waves

对热带大气行星尺度运动所做的尺度分析和物理分析表明：热带大气的行星尺度运动在y方向容易实现气压梯度力与Coriolis力的平衡，它称为纬圈的半地转运动。半地转平衡的建立过程，也就是半地转适应过程相对是很短暂的，它不需要考虑f=β0y随y的变化，因而主要依靠惯性重力波为频散；而半地转平衡建立后的演变过程相对是很缓慢的，它主要受Kelvin波和Rossby波控制。

It is shown from the analysis results that in order to meet the requirement that the calculated geostrophic flow results can reflect the practical current profile structure, it is practicable to select the 700 m level as level of no motion in case of water depth greater than 700 m and to select the bottom boundary as level of no motion in calculating the geostrophic flow.

结果表明，为使计算结果可以反映实际的流速剖面结构，当水深大于700 m和小于700 m时可分别选取700 m层和底边界作为地转流动力计算零流面。

It was shown that the velocity of the drifters is consistent with the geostrophic current derived from MSLA. Several regression models, with an independent variable of sea surface geostrophic current, were set up to simulate the real trajectories of drifters.

针对卫星跟踪漂流浮标运动的准地转性，建立了以海表地转流为主要回归自变量的几种回归模型，用以模拟浮标漂流轨迹，以期对浮标运动特性有进一步的认识。

与geostrophic相关的网络解释 [注：此内容来源于网络，仅供参考]

geostrophic：自转引起的

geostrategy 地缘政治学 | geostrophic 自转引起的 | geosychronous 地球同步的

geostrophic：因地球自转而引起的

geostrophic wind 地转风 | geostrophic 因地球自转而引起的 | German eye splice 顺绳索扭劲的眼环结

geostrophic：因地球自转的

geostrategy /地理战略学/ | geostrophic /因地球自转的/ | geostrophy /地砖/

geostrophic：地轉[的]

geostenography 地理速测 | geostrophic 地转的 | geostrophic-windlevel 地转风高度

geostrophic wind：地转风

此种指数系由此两纬度间之平均海平面气压差算出,而以相当地转风(Geostrophic wind)之东至西分量每秒分尺及十分数表示之. 乃因在D域(D-region)内,对高频(2至3mc) 无线电波之吸收突然显著增加,而使此一频率范围内之接收信号消失;