outlet glacier
简明释义
从陆冰流出的流冰
英英释义
An outlet glacier is a glacier that flows out from an ice cap or ice sheet and drains into the sea or a lake. | 出流冰川是指从冰盖或冰原流出,并排入海洋或湖泊的冰川。 |
例句
1.The melting of the outlet glacier contributes significantly to rising sea levels.
这个出流冰川的融化对海平面上升有显著贡献。
2.The outlet glacier is a critical component of the ice cap, allowing for the flow of ice into the ocean.
这个出流冰川是冰盖的重要组成部分,允许冰流入海洋。
3.The outlet glacier feeds into a large fjord, creating stunning landscapes.
这个出流冰川注入一个大型峡湾,创造出令人惊叹的风景。
4.Hiking near the outlet glacier provides breathtaking views of the surrounding mountains.
在出流冰川附近徒步旅行可以欣赏到周围山脉的壮丽景色。
5.Scientists are studying the retreat of the outlet glacier to understand climate change effects.
科学家们正在研究出流冰川的后退,以了解气候变化的影响。
作文
An outlet glacier is a type of glacier that flows out from an ice cap or ice sheet, typically into the ocean or a lake. These glaciers play a crucial role in the dynamics of ice movement and are significant contributors to sea-level rise. Understanding outlet glaciers is essential for climate science, as they are sensitive indicators of climate change. As global temperatures rise, these glaciers may accelerate their flow, leading to increased calving and melting. One of the most studied outlet glaciers is the Jakobshavn Glacier in Greenland. This glacier has been observed to flow faster than ever before, contributing significantly to the melting of the Greenland ice sheet. The rapid retreat of Jakobshavn has raised concerns among scientists about the stability of the ice sheet as a whole. The melting of outlet glaciers like Jakobshavn is not only a local issue but has global repercussions, as it contributes to rising sea levels that threaten coastal communities worldwide.The mechanisms behind the flow of outlet glaciers are complex. They are influenced by factors such as the topography of the underlying bedrock, the temperature of the ice, and the presence of meltwater. Meltwater can lubricate the base of the glacier, allowing it to slide more easily over the bedrock. This phenomenon has been observed in various studies, where increased meltwater during warmer months leads to enhanced glacier flow. Moreover, the calving process, where chunks of ice break off from the front of a glacier, is a significant aspect of how outlet glaciers contribute to sea-level rise. When these large ice blocks break off and fall into the ocean, they displace water, leading to an increase in sea level. The rate of calving can be influenced by ocean temperatures, which have been rising due to climate change.To monitor the changes in outlet glaciers, scientists use a combination of satellite imagery, aerial surveys, and ground-based measurements. These methods allow researchers to track the speed of glacier flow, the extent of melting, and the overall health of these critical ice formations. Understanding these changes is vital for predicting future sea-level rise and its impacts on human populations and ecosystems.In conclusion, outlet glaciers are vital components of our planet's cryosphere and play an essential role in global sea-level dynamics. Their response to climate change serves as a warning sign for the broader implications of warming temperatures. As we continue to study and monitor these glaciers, it is imperative to consider the interconnectedness of climate systems and the urgent need for action to mitigate climate change effects. The future of our coastlines and the millions who inhabit them may depend on our understanding and management of outlet glaciers and their contributions to rising sea levels.
出流冰川是一种从冰帽或冰原流出的冰川,通常流入海洋或湖泊。这些冰川在冰的运动动态中发挥着至关重要的作用,是海平面上升的重要贡献者。理解出流冰川对于气候科学至关重要,因为它们是气候变化的敏感指示器。随着全球气温的上升,这些冰川可能加速流动,导致更多的冰崩和融化。最受研究的出流冰川之一是格林兰的雅各布哈文冰川。观察到该冰川的流动速度比以往任何时候都快,对格林兰冰盖的融化贡献显著。雅各布哈文的快速退缩让科学家们对整个冰盖的稳定性产生了担忧。出流冰川的融化不仅是一个地方性问题,而且具有全球影响,因为它导致海平面上升,威胁到世界各地的沿海社区。出流冰川的流动机制复杂。它们受到底层基岩地形、冰温和融水存在等因素的影响。融水可以润滑冰川的底部,使其更容易在基岩上滑动。在各种研究中观察到这一现象,即在温暖的月份,融水增加会导致冰川流动增强。此外,冰川的崩裂过程,即大块冰从冰川前缘断裂,是出流冰川如何贡献海平面上升的重要方面。当这些大冰块断裂并落入海洋时,它们会排开水,从而导致海平面上升。崩裂的速度可能受到海洋温度的影响,而海洋温度因气候变化而上升。为了监测出流冰川的变化,科学家使用卫星图像、空中调查和地面测量相结合的方法。这些方法使研究人员能够跟踪冰川流动的速度、融化的程度以及这些关键冰体的整体健康状况。理解这些变化对于预测未来海平面上升及其对人类和生态系统的影响至关重要。总之,出流冰川是我们星球冰冻圈的重要组成部分,在全球海平面动态中发挥着关键作用。它们对气候变化的反应是温暖气温更广泛影响的警示信号。随着我们继续研究和监测这些冰川,必须考虑气候系统之间的相互联系以及采取紧急行动以减轻气候变化影响的迫切需要。我们沿海地区和数百万居民的未来可能取决于我们对出流冰川及其对海平面上升贡献的理解和管理。
相关单词