geostrophic的音標是[?d?i???str??f?k]；基本翻譯是地轉風；速記技巧是注意中間的r不發音。

Geostrophic的詞源：

詞根“geostrophic”來源于希臘語，意為“地球的”。

變化形式：

復數形式為“geostrophic”，意為“地球的”。

相關單詞：

1. Geostrophic current：地轉流，一種在地球表面流動的流體，由于地球自轉而產生的科里奧利力對其有影響。

2. Geostrophic speed：地轉速度，描述地轉流中流體運動的速度。

3. Geostrophic wind：地轉風，描述在地球表面流動的風，由于地球自轉而產生的科里奧利力對其有影響。

4. Geostrophy：地轉平衡，指在地球表面流動的流體系統，受到的科里奧利力與慣性力相等。

5. Equatorial geostrophic current：赤道地轉流，指在赤道地區流動的流體，由于地球自轉而產生的科里奧利力對其有影響。

6. Shear geostrophy：剪切地轉平衡，指在垂直方向上流動的流體系統，受到的科里奧利力和慣性力相等。

7. Geostrophic velocity field：地轉速度場，描述流體運動的速度場，其中流體的速度與地轉速度相等。

8. Geostrophic wind shear：地轉風剪切，指在垂直方向上流動的風速隨高度的變化。

9. Geostrophic wind stress：地轉風應力，描述風對流體的作用力，與地轉風速度成正比。

10. Non-geostrophic flow：非地轉流，指流體運動不受地球自轉影響或影響較小的流動系統。

常用短語：

1. geostrophic wind

2. geostrophic current

3. geostrophic balance

4. geostrophic flow

5. geostrophic adjustment

6. geostrophic velocity

7. geostrophic circulation

雙語例句：

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

該地區的風速主要由地轉風決定。

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

地轉流從北半球流向南半球。

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

為了維持洋流系統的平衡，需要進行地轉調整。

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

地轉速度決定了水在某一方向上的流動速度。

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

地轉環流在全球氣候調節中發揮著重要作用。

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

海洋環流系統受到多種因素的影響，包括地轉流和風應力。

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

海洋環流系統不斷進行地轉調整以維持平衡。

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.