气候变化背景下越南海东省干旱变化研究

Q4 Engineering
N. T. Ha, D. N. Hung, Cù Thị Phương
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引用次数: 0

摘要

海阳是越南北部红河三角洲的一个省,GDP为3020美元/年。它的经济主要依靠自然条件,特别是农业。在气候变化的背景下,干旱将是一种严重影响经济的自然灾害,农业也不例外。利用Pearson相关系数评价方法,建立多元线性回归方程,发现总蒸发量与月总降雨量、月平均气温、月最高气温和月最低气温具有良好的相关性。这是根据气候变化情景计算未来潜在蒸发量的基础。利用越南气候变化情景的输入数据,计算干旱指数K,计算了2021- 2050年海阳省最干旱的三个月(12、1、2)的干旱演变。结果表明:在RCP 4.5和RCP 8.5两种情景下,干旱指数K均处于干旱和极高干旱水平;rcp8.5的干旱程度高于rcp4.5,而芝林气象站的干旱程度是海阳气象站的1.4 ~ 1.5倍。结果表明,干旱具有明显的周期性,干旱情景rcp8.5每9-10年达到一次最大值。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A study on changes in drought in Haiduong provinces of Vietnam in the context of climate change
Hai Duong is a province in the Red River Delta of northern Vietnam, with a GDP of 3020 USD/year. Its economy depends mainly on natural conditions, especially agriculture. In the context of climate change, drought will be a natural disaster that greatly affects the economy and agriculture is no exception. Using the Pearson correlation coefficient evaluation method and building multi-linear regression equations, a good correlation was found between total evaporation and total monthly rainfall, monthly mean temperature, monthly maximum temperature and monthly minimum temperature. This is the basis for calculating potential future evaporation based on climate change scenarios. Calculating the drought index K with the input data of climate change scenarios for Vietnam, this analysis has calculated the drought evolution for the three driest months of the year (12, first, 2) for the period 2021- 2050 in Hai Duong province. Results show that with both scenarios (RCP 4.5 and RCP 8.5), the drought index K is at drought and very high drought levels. The drought level in RCP 8.5 is higher than in RCP 4.5 while the drought level at Chi Linh meteorological station is 1.4-1.5 times higher than that at Hai Duong meteorological station. It emerges that drought is clearly cyclical with the drought scenario RCP 8.5 which reaches its maximum every 9-10 years.
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来源期刊
Disaster Advances
Disaster Advances 地学-地球科学综合
CiteScore
0.70
自引率
0.00%
发文量
57
审稿时长
3.5 months
期刊介绍: Information not localized
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