frontolysis

简明释义

英[frʌnˈtɒlɪsɪs]美[frʌnˈtɑːləsɪs]

n. 锋面减弱

英英释义

单词用法

同义词

反义词

例句

1.The continuous stage in the rainstorm, effects of divergence and deformation are equal in match or contest of strength, effect of tilting term is frontolysis.

在暴雨持续阶段，散度项锋生和形变项锋生作用旗鼓相当，倾斜项起锋消作用。

2.The continuous stage in the rainstorm, effects of divergence and deformation are equal in match or contest of strength, effect of tilting term is frontolysis.

在暴雨持续阶段，散度项锋生和形变项锋生作用旗鼓相当，倾斜项起锋消作用。

3.The horizontal advection term contribute little to the frontogenesis and frontolysis.

水平温度梯度的平流对锋生（消）的影响都很小。

4.At night, the frontolysis occurs due to the radiative cooling of dust.

晚上，沙尘辐射冷却导致大气低层锋消。

5.Frontogenesis and frontolysis have decisive effect on the precipitation near Meiyu front.

锋生锋消对于梅雨锋附近有无降水起到了重要的作用。

6.The frontogenesis (frontolysis) is a problem of significance in synoptic meteorology and climatology.

锋生(锋消)在天气学和气候学方面是一个重要问题。

7.Meteorologists observed a significant frontolysis 锋消散 over the region, leading to clearer skies.

气象学家观察到该地区出现了显著的frontolysis锋消散，导致天空变得更加清晰。

8.The frontolysis 锋消散 process can result in the weakening of storm systems.

在这个过程中，frontolysis锋消散可能导致风暴系统的减弱。

9.As the cold front moved through, a rapid frontolysis 锋消散 was noted by the team.

随着冷锋的移动，团队注意到了快速的frontolysis锋消散现象。

10.Understanding frontolysis 锋消散 helps meteorologists predict changes in weather patterns.

理解frontolysis锋消散有助于气象学家预测天气模式的变化。

11.During the weather briefing, the frontolysis 锋消散 was identified as a key factor in the forecast.

在天气简报中，frontolysis锋消散被确定为预测中的一个关键因素。

作文

In meteorology, understanding various weather phenomena is essential for predicting and analyzing atmospheric conditions. One such phenomenon is frontolysis, which refers to the weakening or dissipation of a weather front. Weather fronts are boundaries between different air masses, and they play a crucial role in determining local weather patterns. When a front undergoes frontolysis, it indicates that the forces maintaining the front are diminishing, leading to a change in weather conditions. This process can result in the reduction of precipitation, a rise in temperatures, and a general stabilization of the atmosphere. The study of frontolysis is particularly important for meteorologists as it helps them forecast changes in weather more accurately. For instance, when a cold front begins to weaken, it may signal the end of a period of stormy weather, allowing meteorologists to inform the public about improving conditions. Conversely, understanding frontolysis can also indicate potential shifts towards more severe weather if the front is dissipating in a manner that allows for other atmospheric disturbances to take place. One practical example of frontolysis can be seen in the transition from winter to spring. During this time, many regions experience a variety of weather fronts as warmer air begins to push northward. As these fronts interact with lingering cold air, they can create complex weather patterns. However, as the season progresses, frontolysis often occurs, leading to fewer cold fronts and a more stable warm air mass dominating the region. This transition is vital for agriculture, as farmers must understand when to plant crops based on expected weather patterns. Moreover, frontolysis is not just an isolated event; it often interacts with other meteorological processes. For example, when a front weakens, it can lead to the development of high-pressure systems, which are associated with clear skies and calm weather. Understanding the implications of frontolysis allows meteorologists to provide better forecasts and warnings. In conclusion, frontolysis is a significant concept in meteorology that describes the weakening of weather fronts. It plays a crucial role in understanding and predicting weather patterns and has practical implications for various sectors, including agriculture and disaster preparedness. As our climate continues to change, the study of processes like frontolysis becomes even more important for ensuring that we can adapt to and anticipate the impacts of shifting weather patterns. By comprehensively studying frontolysis, meteorologists can enhance their forecasting abilities, ultimately benefiting society as a whole.

在气象学中，理解各种天气现象对于预测和分析大气条件至关重要。其中一个现象是frontolysis，它指的是天气前线的减弱或消散。天气前线是不同气团之间的边界，它们在决定局部天气模式方面发挥着关键作用。当一条前线经历frontolysis时，这表明维持该前线的力量正在减弱，导致天气条件的变化。这个过程可能导致降水量减少、温度上升以及大气的整体稳定。对于气象学家来说，研究frontolysis尤为重要，因为它有助于他们更准确地预测天气变化。例如，当一条冷锋开始减弱时，这可能意味着暴风雨天气时期的结束，使气象学家能够向公众通报改善的天气条件。相反，理解frontolysis也可以指示潜在的严重天气变化，如果前线以一种允许其他大气扰动发生的方式消散。frontolysis的一个实际例子可以在冬季转春季的过渡中看到。在这个时候，许多地区经历多种天气前线，因为温暖的空气开始向北推进。当这些前线与残留的冷空气相互作用时，它们可以形成复杂的天气模式。然而，随着季节的推移，frontolysis通常会发生，导致较少的冷前线和一个更稳定的暖气团主导该地区。这一过渡对农业至关重要，因为农民必须根据预期的天气模式了解何时播种作物。此外，frontolysis并不是一个孤立的事件；它通常与其他气象过程相互作用。例如，当一条前线减弱时，它可以导致高压系统的发展，而高压系统通常与晴朗的天空和宁静的天气相关。理解frontolysis的影响使气象学家能够提供更好的天气预报和警告。总之，frontolysis是气象学中的一个重要概念，描述了天气前线的减弱。它在理解和预测天气模式方面发挥着至关重要的作用，并对农业和灾害准备等各个领域具有实际意义。随着我们的气候不断变化，像frontolysis这样的过程的研究变得更加重要，以确保我们能够适应和预见天气模式变化的影响。通过全面研究frontolysis，气象学家可以增强他们的预测能力，最终使整个社会受益。