accumulation area ratio

简明释义

积累区比值;

英英释义

The accumulation area ratio is a measure that compares the area of a glacier or snowfield where accumulation occurs (typically at higher elevations) to the total area of the glacier or snowfield.

积累区比率是一个度量,用于比较冰川或雪场中发生积累的区域(通常位于较高海拔)与冰川或雪场的总面积。

例句

1.The accumulation area ratio indicates the proportion of the glacier that contributes to ice accumulation.

积累区域比率表示对冰雪积累有贡献的冰川比例。

2.Researchers found that the accumulation area ratio is crucial for understanding glacier dynamics.

研究人员发现,积累区域比率对于理解冰川动态至关重要。

3.In this study, we calculated the accumulation area ratio over several years.

在这项研究中,我们计算了几年的积累区域比率

4.Monitoring the accumulation area ratio can help predict future sea level rise.

监测积累区域比率可以帮助预测未来的海平面上升。

5.A higher accumulation area ratio suggests a healthier glacier system.

较高的积累区域比率表明冰川系统更健康。

作文

The concept of accumulation area ratio plays a crucial role in understanding the dynamics of glacial systems and their impact on climate change. This term refers to the ratio of the area of a glacier that accumulates snow and ice to the total area of the glacier itself. In simpler terms, it measures how much of the glacier's surface is contributing to its growth versus how much is subject to melting or ablation. Understanding this ratio is essential for scientists as they study glacier mass balance, which is a key indicator of climate health.Glaciers are vital components of the Earth's hydrological cycle and serve as significant freshwater reservoirs. The accumulation area ratio can vary greatly depending on several factors, including geographical location, altitude, and climatic conditions. For instance, glaciers located in polar regions typically have higher accumulation area ratios compared to those in temperate zones, where warmer temperatures lead to increased melting.Monitoring changes in the accumulation area ratio over time allows researchers to predict future trends in glacier behavior and their contribution to sea-level rise. As global temperatures continue to increase, many glaciers are experiencing a decline in their accumulation areas. This reduction not only affects the accumulation area ratio but also poses risks to ecosystems and communities that rely on glacial meltwater for drinking, irrigation, and hydroelectric power.In addition to its implications for water resources, the accumulation area ratio also provides insights into the broader impacts of climate change. By studying how this ratio shifts, scientists can better understand the feedback mechanisms within the climate system. For instance, as glaciers shrink, they expose darker land surfaces that absorb more sunlight, further accelerating warming and melting—a phenomenon known as the albedo effect.Moreover, the accumulation area ratio is not just a static measure; it can be influenced by human activities such as urban development and deforestation, which can alter local climates and precipitation patterns. As we continue to grapple with the challenges posed by climate change, understanding the nuances of the accumulation area ratio becomes increasingly important for developing effective mitigation and adaptation strategies.In conclusion, the accumulation area ratio is a critical metric in the study of glaciers and their response to climate change. It encapsulates the delicate balance between accumulation and ablation, providing valuable information about the health of our planet's cryosphere. As we strive to address the pressing issues of climate change, a deeper understanding of such concepts will empower us to make informed decisions that protect our environment for future generations.

“积累区比率”这一概念在理解冰川系统的动态及其对气候变化的影响中发挥着至关重要的作用。这个术语指的是冰川积累雪和冰的区域与冰川总面积的比率。简单来说,它衡量了冰川表面有多少部分在促进其生长,与有多少部分处于融化或消融状态。理解这个比率对于科学家们研究冰川质量平衡至关重要,冰川质量平衡是气候健康的一个关键指标。冰川是地球水文循环的重要组成部分,是重要的淡水储存库。“积累区比率”可以因多个因素而大相径庭,包括地理位置、海拔和气候条件。例如,位于极地地区的冰川通常具有较高的积累区比率,而温带地区的冰川由于气温较高,导致融化增加,积累区比率较低。监测“积累区比率”随时间的变化使研究人员能够预测冰川行为的未来趋势及其对海平面上升的贡献。随着全球温度的持续上升,许多冰川的积累区正在减少。这种减少不仅影响“积累区比率”,还对依赖冰川融水进行饮用、灌溉和水电发电的生态系统和社区构成风险。除了对水资源的影响外,“积累区比率”还提供了气候变化更广泛影响的见解。通过研究这一比率的变化,科学家们可以更好地理解气候系统中的反馈机制。例如,随着冰川的缩小,它们暴露出较暗的土地表面,吸收更多的阳光,进一步加速变暖和融化,这一现象被称为反照率效应。此外,“积累区比率”并不是一个静态的度量;它可能受到人类活动的影响,例如城市发展和森林砍伐,这些活动可以改变当地气候和降水模式。随着我们继续应对气候变化带来的挑战,理解“积累区比率”的细微差别变得愈发重要,以便制定有效的缓解和适应策略。总之,“积累区比率”是研究冰川及其对气候变化响应的关键指标。它概括了积累与消融之间的微妙平衡,为我们提供了有关地球冰冻圈健康的重要信息。在我们努力解决气候变化的紧迫问题时,对这些概念的深入理解将使我们能够做出明智的决策,以保护我们的环境,造福未来几代人。

相关单词

accumulation

accumulation详解:怎么读、什么意思、用法

ratio

ratio详解:怎么读、什么意思、用法