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斯威士兰王国干旱的全国时间变化:1981 - 2018年

Nationwide temporal variability of droughts in the Kingdom of Eswatini: 1981-2018.

作者信息

Tfwala C M, Mengistu A G, Seyama E, Mosia M S, van Rensburg L D, Mvubu B, Mbingo M, Dlamini P

机构信息

Department of Soil, Crop and Climate Sciences, University of the Free State, P.O. Box 339, 9300 Bloemfontein, South Africa.

Department of Agricultural Research and Specialists Services, Ministry of Agriculture, P.O. Box 4, M204 Malkerns, Swaziland.

出版信息

Heliyon. 2020 Dec 13;6(12):e05707. doi: 10.1016/j.heliyon.2020.e05707. eCollection 2020 Dec.

Abstract

For adequate mitigation and adaptation measures, it is essential to have detailed analysis of droughts patterns. This study determined the i) occurrence and severity of droughts ii) drought recurrence frequencies and iii) drought trends across different agro-ecological zones in the Kingdom of Eswatini for the period 1981 to 2018. A Standardised Precipitation Index (SPI) computed from long-term precipitation data measured from six meteorological stations was used to determine drought occurrence and severity. Python software (Version 3.6) was applied on the SPI values to predict the recurrence of drought events over time in years. The SPI showed that in the Highveld, 42% of the droughts were moderate, 32% were severe and the remaining 26%, which all occurred post 1980 were extreme (SPI -2.34 to -2.82). The Middleveld had an even proportion of drought categories (29-35%). The Lowveld recorded 62% of moderate, 8% severe and 30% extreme droughts of which 70% occurred post 2000. Moderate droughts were found to recur every 4-5 years while extreme droughts are expected every 13-21 years. These findings are essential for mitigation and adaptation measures geared towards the adverse effects of droughts.

摘要

为了采取充分的缓解和适应措施,对干旱模式进行详细分析至关重要。本研究确定了:i)斯威士兰王国1981年至2018年期间不同农业生态区干旱的发生情况和严重程度;ii)干旱重现频率;iii)干旱趋势。利用从六个气象站测量的长期降水数据计算得出的标准化降水指数(SPI)来确定干旱的发生情况和严重程度。运用Python软件(版本3.6)对SPI值进行分析,以预测多年来干旱事件随时间的重现情况。SPI显示,在高地,42%的干旱为中度,32%为重度,其余26%(均发生在1980年之后)为极端干旱(SPI为-2.34至-2.82)。中地的干旱类别比例较为均衡(29%-35%)。低地记录的中度干旱占62%,重度干旱占8%,极端干旱占30%,其中70%发生在2000年之后。发现中度干旱每4至5年重现一次,而极端干旱预计每13至21年出现一次。这些发现对于针对干旱不利影响的缓解和适应措施至关重要。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8abf/7744714/cb57016c018b/gr1.jpg

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