比哈尔邦降水行为的长期评估(1901-2021):模式、趋势和观测变率

Manu Raj Sharma, Sukeshi Priya
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引用次数: 0

摘要

降雨是支配任何地区气候和水文条件的重要变量。在过去的一个世纪里,全球温室气体排放的增加导致了世界各地水文气象条件模式的变化。它导致了降雨模式和趋势的改变,造成了干旱和洪水的偶然发生。降雨变异性的增加引发并加剧了极端事件,在不同的气候变化情景下构成潜在的未来风险。这种预测的可变性可能会导致比哈尔邦等受洪水影响的邦发生剧烈变化,在那里,即使是降雨量的微小变化也可能影响水文循环和农业条件。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Long-term Assessment of Precipitation Behaviour in Bihar (1901-2021): Patterns, Trends and Observed Variability
Rainfall is an important variable that governs the climate and hydrological conditions of any region. During the past century, an increase in global emissions of greenhouse gases has caused changes in the patterns of hydro-meteorological conditions across the world. It has resulted in changed patterns and trends of rainfall, causing episodic occurrences of droughts and floods. This increasing variability of rainfall has triggered and intensified extreme events that pose potential future risks under different climate change scenarios. This projected variability may induce drastic changes in the flood affected states like Bihar where even a slightest change in rainfall variability may affect hydrological cycle and agriculture conditions.
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