ice of land origin
简明释义
陆源冰
英英释义
Ice of land origin refers to ice that forms on land surfaces, such as glaciers or ice sheets, as opposed to sea ice which forms from freezing seawater. | 陆源冰指的是在陆地表面形成的冰,如冰川或冰盖,与海冰相对,后者是由海水冻结而成的。 |
例句
1.The researchers found that the melting of ice of land origin 陆地来源的冰 contributed significantly to rising sea levels.
研究人员发现,陆地来源的冰 ice of land origin 的融化对海平面上升有显著贡献。
2.In climate models, it is crucial to account for ice of land origin 陆地来源的冰 when predicting future temperature changes.
在气候模型中,预测未来温度变化时考虑 陆地来源的冰 ice of land origin 是至关重要的。
3.The term ice of land origin 陆地来源的冰 refers to glaciers and ice sheets that form on land rather than in the ocean.
术语 陆地来源的冰 ice of land origin 指的是在陆地上形成的冰川和冰盖,而不是在海洋中形成的。
4.Scientists are studying the effects of ice of land origin 陆地来源的冰 on ocean currents and ecosystems.
科学家们正在研究 陆地来源的冰 ice of land origin 对海洋洋流和生态系统的影响。
5.The Antarctic ice sheet is primarily composed of ice of land origin 陆地来源的冰, which is at risk due to global warming.
南极冰盖主要由 陆地来源的冰 ice of land origin 组成,由于全球变暖而面临风险。
作文
The planet Earth is home to a variety of natural phenomena, one of which is ice. Ice can be found in many forms, but one particularly interesting type is the ice of land origin, which refers to ice that forms directly from the land rather than from the ocean or other bodies of water. This type of ice is primarily found in glaciers and ice sheets, which are essential components of our planet's climate system. Understanding the characteristics and implications of ice of land origin is crucial for appreciating its role in the environment and climate change. Glaciers are formed through the accumulation of snow over many years. As more snow falls, the lower layers become compacted and turn into ice. This process is slow and can take thousands of years. The ice of land origin found in glaciers is often very dense and can contain bubbles of air trapped from the atmosphere at the time of formation. These bubbles provide valuable information about past climate conditions, allowing scientists to study historical climate patterns and make predictions about future changes. In contrast to sea ice, which forms from freezing seawater, ice of land origin plays a significant role in regulating global sea levels. When glaciers melt due to rising temperatures, they contribute to an increase in sea levels, which can have devastating effects on coastal communities and ecosystems. The melting of ice of land origin is a clear indicator of climate change, as it directly correlates with rising global temperatures. Moreover, the presence of glaciers and their ice of land origin is vital for freshwater resources. Many rivers rely on glacial meltwater to maintain their flow during warmer months. In regions where glaciers are receding, such as the Himalayas or the Andes, there is growing concern about the long-term availability of freshwater for millions of people who depend on these rivers for drinking water and agriculture. The study of ice of land origin also extends to its impact on biodiversity. Glacial environments are unique ecosystems that host specialized flora and fauna adapted to cold conditions. As these ice masses retreat, the habitats for these species are threatened, leading to potential extinction and loss of biodiversity. Understanding how ice of land origin influences these ecosystems helps conservationists develop strategies to protect vulnerable species. In conclusion, the ice of land origin is not merely a frozen substance; it is a critical element of our planet’s environmental system. Its formation, melting, and effects on sea levels, freshwater resources, and biodiversity highlight the interconnectedness of Earth's systems. As we continue to confront the challenges posed by climate change, recognizing the importance of ice of land origin will be essential for developing effective solutions to mitigate its impacts and preserve our planet for future generations.
地球是许多自然现象的家园,其中之一就是冰。冰可以以多种形式存在,但有一种特别有趣的类型是陆源冰,指的是直接从陆地形成的冰,而不是来自海洋或其他水体。这种冰主要存在于冰川和冰盖中,它们是我们星球气候系统的重要组成部分。理解陆源冰的特征和影响对于欣赏其在环境和气候变化中的作用至关重要。冰川是通过多年积雪的积累而形成的。随着更多的雪降落,较低层的雪被压缩,变成冰。这个过程缓慢,可能需要数千年。冰川中发现的陆源冰通常非常致密,并且可以包含在形成时大气中捕获的空气泡。这些气泡提供了关于过去气候条件的宝贵信息,使科学家能够研究历史气候模式并对未来变化做出预测。与海冰不同,海冰是由海水冻结而成的,而陆源冰在调节全球海平面方面发挥着重要作用。当由于气温上升而导致冰川融化时,它们会导致海平面的上升,这可能对沿海社区和生态系统造成毁灭性的影响。陆源冰的融化是气候变化的明显指标,因为它与全球气温上升直接相关。此外,冰川及其陆源冰的存在对淡水资源至关重要。许多河流依赖冰川融水在温暖的月份维持流量。在冰川退缩的地区,如喜马拉雅山脉或安第斯山脉,人们对这些河流的长期淡水供应感到越来越担忧,因为数百万人依赖这些河流提供饮用水和农业用水。陆源冰的研究还扩展到其对生物多样性的影响。冰川环境是独特的生态系统,栖息着适应寒冷条件的特殊植物和动物。随着这些冰块的退缩,这些物种的栖息地受到威胁,可能导致灭绝和生物多样性的丧失。了解陆源冰如何影响这些生态系统有助于保护主义者制定保护易受威胁物种的策略。总之,陆源冰不仅仅是一种冰冻物质;它是我们星球环境系统的关键元素。它的形成、融化以及对海平面、淡水资源和生物多样性的影响突显了地球系统的相互联系。随着我们继续面对气候变化带来的挑战,认识到陆源冰的重要性将对制定有效的解决方案以减轻其影响和保护我们的星球至关重要。