geostrophic

geostrophic的音标是[ˌdʒiːəˈstrəʊfɪk]；基本翻译是地转风；速记技巧是注意中间的r不发音。

Geostrophic的词源：

词根“geostrophic”来源于希腊语，意为“地球的”。

变化形式：

复数形式为“geostrophic”，意为“地球的”。

相关单词：

1. Geostrophic current：地转流，一种在地球表面流动的流体，由于地球自转而产生的科里奥利力对其有影响。

2. Geostrophic speed：地转速度，描述地转流中流体运动的速度。

3. Geostrophic wind：地转风，描述在地球表面流动的风，由于地球自转而产生的科里奥利力对其有影响。

4. Geostrophy：地转平衡，指在地球表面流动的流体系统，受到的科里奥利力与惯性力相等。

5. Equatorial geostrophic current：赤道地转流，指在赤道地区流动的流体，由于地球自转而产生的科里奥利力对其有影响。

6. Shear geostrophy：剪切地转平衡，指在垂直方向上流动的流体系统，受到的科里奥利力和惯性力相等。

7. Geostrophic velocity field：地转速度场，描述流体运动的速度场，其中流体的速度与地转速度相等。

8. Geostrophic wind shear：地转风剪切，指在垂直方向上流动的风速随高度的变化。

9. Geostrophic wind stress：地转风应力，描述风对流体的作用力，与地转风速度成正比。

10. Non-geostrophic flow：非地转流，指流体运动不受地球自转影响或影响较小的流动系统。

常用短语：

1. geostrophic wind

2. geostrophic current

3. geostrophic balance

4. geostrophic flow

5. geostrophic adjustment

6. geostrophic velocity

7. geostrophic circulation

双语例句：

1. The wind speed in the region is mainly determined by the geostrophic wind.

该地区的风速主要由地转风决定。

2. The geostrophic current flows from the northern to the southern hemisphere.

地转流从北半球流向南半球。

3. Geostrophic adjustment is necessary to maintain the balance of the ocean current system.

为了维持洋流系统的平衡，需要进行地转调整。

4. The geostrophic velocity determines the speed at which water flows in a given direction.

地转速度决定了水在某一方向上的流动速度。

5. The geostrophic circulation plays an important role in global climate regulation.

地转环流在全球气候调节中发挥着重要作用。

6. The ocean current system is influenced by various factors, including the geostrophic current and wind stress.

海洋环流系统受到多种因素的影响，包括地转流和风应力。

7. The ocean current system is constantly undergoing geostrophic adjustment to maintain balance.

海洋环流系统不断进行地转调整以维持平衡。

英文小作文：

Title: The Mystery of the Geostrophic Current

The ocean current system is a complex network of currents and flows that plays a crucial role in the global climate system. Among these currents, the geostrophic current has always fascinated scientists and researchers for its mysterious behavior and influence on the oceanic environment.

The geostrophic current flows in a straight line at a constant speed, independent of the local topography and other factors. It is driven by the balance between the Coriolis force and the pressure gradient force, resulting in a constant flow of water from one region to another. This constant flow creates a dynamic balance in the oceanic environment, maintaining a certain level of circulation and exchange of materials between different regions.

However, the geostrophic current is not without its challenges. It is influenced by various factors, including wind stress, temperature differences, and local topography, which can affect its speed and direction. Understanding these factors and their interactions with the geostrophic current is crucial for predicting and managing oceanic environments and their impact on climate change.

The geostrophic current is an ongoing mystery that continues to captivate scientists and researchers, opening new avenues for exploration and discovery in the oceanic environment. Understanding its role and influence on the global climate system is essential for maintaining a sustainable environment for future generations.