ice tongue afloat

简明释义

浮冰舌

英英释义

An ice tongue afloat refers to a large, elongated mass of floating ice that extends from a glacier into a body of water, typically characterized by its flat or gently sloping surface.

漂浮的冰舌是指从冰川延伸到水体中的一大块细长的漂浮冰块,通常具有平坦或轻微倾斜的表面。

例句

1.The ice tongue afloat was a stunning sight, glistening under the Arctic sun.

这个漂浮冰舌在北极阳光下闪闪发光,令人惊叹。

2.The researchers observed the ice tongue afloat at the edge of the glacier, indicating significant melting.

研究人员观察到冰川边缘的漂浮冰舌,这表明融化显著。

3.The large ice tongue afloat posed a risk to nearby shipping routes.

大型的漂浮冰舌对附近的航运路线构成了风险。

4.Scientists are studying the movement of the ice tongue afloat to understand climate change effects.

科学家们正在研究漂浮冰舌的运动,以了解气候变化的影响。

5.During the expedition, we encountered an ice tongue afloat that had broken off from the main glacier.

在探险过程中,我们遇到了一个从主冰川断裂的漂浮冰舌

作文

The phenomenon of glaciers and icebergs has always fascinated scientists and nature enthusiasts alike. One particular term that often arises in discussions about glacial formations is ice tongue afloat. This term refers to a large, floating extension of a glacier that protrudes into the sea. These ice tongues can be found in various polar regions, where they play a crucial role in understanding climate change and its impact on our planet. ice tongue afloat (浮冰舌)不仅是冰川的一部分,它们还为我们提供了重要的气候数据。 When we think about glaciers, we often picture massive, solid structures of ice that are firmly grounded on land. However, the reality is that many glaciers extend into the ocean, creating these dynamic and fascinating formations known as ice tongues. An ice tongue afloat can vary significantly in size, with some stretching for miles and others being relatively small. These extensions are formed when the glacier flows over the edge of a landmass and into the water, where the ice begins to float. The presence of an ice tongue afloat is critical for several reasons. Firstly, it acts as a barrier, slowing down the flow of the glacier behind it. This phenomenon can help stabilize the glacier and prevent it from calving—breaking off chunks of ice into the ocean. However, as global temperatures rise, these ice tongues are becoming increasingly vulnerable. Scientists have observed that many ice tongue afloat formations are retreating at alarming rates, which contributes to rising sea levels. Moreover, ice tongue afloat structures are essential indicators of environmental changes. By studying their movement and melting patterns, researchers can gather valuable data about the health of polar ecosystems and the overall effects of climate change. For instance, as these ice tongues melt, they release freshwater into the ocean, which can disrupt local marine life and alter ocean currents. In addition to their scientific significance, ice tongue afloat formations also hold aesthetic value. They create stunning landscapes that attract tourists and photographers from around the world. The sight of a massive ice tongue extending into the deep blue sea is both breathtaking and humbling. It serves as a reminder of the beauty and fragility of our planet's natural wonders. In conclusion, understanding the concept of ice tongue afloat is vital for appreciating the complexities of our planet's glacial systems. These floating extensions not only contribute to the dynamics of glaciers but also serve as critical indicators of climate change. As we continue to study and monitor these magnificent structures, we gain insight into the health of our environment and the urgent need for action to combat climate change. Protecting these natural formations is essential for preserving the delicate balance of our ecosystems and ensuring a sustainable future for generations to come.

冰川和冰山的现象一直吸引着科学家和自然爱好者。一个常常在讨论冰川形成时出现的术语是ice tongue afloat(浮冰舌)。这个术语指的是一个大型的、漂浮的冰川延伸部分,突入海洋。这些冰舌可以在各种极地地区找到,它们在理解气候变化及其对我们星球的影响方面发挥着至关重要的作用。ice tongue afloat不仅是冰川的一部分,它们还为我们提供了重要的气候数据。当我们想到冰川时,常常会想象出坚固的冰块,稳稳地扎根于陆地。然而,现实是许多冰川向海洋延伸,形成这些动态而迷人的结构,称为冰舌。ice tongue afloat的大小差异很大,有些延伸数英里,而其他则相对较小。这些延伸部分的形成是因为冰川流过陆地边缘,进入水中,冰开始漂浮。ice tongue afloat的存在对于几个原因至关重要。首先,它充当了一种屏障,减缓了冰川后方冰体的流动。这种现象有助于稳定冰川,防止其崩裂——将冰块断裂并掉入海洋。然而,随着全球气温上升,这些冰舌变得越来越脆弱。科学家观察到,许多ice tongue afloat的形成正在以惊人的速度退缩,这导致海平面上升。此外,ice tongue afloat结构是环境变化的重要指标。通过研究它们的移动和融化模式,研究人员可以收集有关极地生态系统健康和气候变化整体影响的宝贵数据。例如,随着这些冰舌的融化,它们将淡水释放到海洋中,这可能会干扰当地海洋生物并改变洋流。除了科学意义外,ice tongue afloat的形成也具有美学价值。它们创造出令人惊叹的景观,吸引来自世界各地的游客和摄影师。看到一条巨大的冰舌延伸到深蓝色的海洋中,既令人叹为观止又令人谦卑。这提醒我们我们星球自然奇观的美丽与脆弱。总之,理解ice tongue afloat的概念对于欣赏我们星球冰川系统的复杂性至关重要。这些漂浮的延伸不仅有助于冰川的动态,还作为气候变化的重要指标。随着我们继续研究和监测这些壮丽的结构,我们获得了对我们环境健康的洞察,以及应对气候变化的紧迫需求。保护这些自然结构对于保持生态系统的微妙平衡和确保未来几代人的可持续发展至关重要。

相关单词

afloat

afloat详解:怎么读、什么意思、用法