Department of Geography, Kurukshetra University, Kurukshetra, 136119, India.
Department of Geography, Government College, Bahu, Jhajjar, 124142, India.
Environ Monit Assess. 2021 Oct 21;193(11):743. doi: 10.1007/s10661-021-09539-4.
Rajasthan state of India is prone to recurrent droughts; hence, exploring drought severities over the semi-arid Sahibi river basin is crucial for drought management. To investigate drought severity, the Rainfall Anomaly Index (RAI) was applied at two time spans, such as annual (January to December) and the monsoon season (June to September), using long-term daily rainfall data (1961-2017) for nine rain gauge stations. Similarly, for the examination of various drought characteristics like magnitude, duration and intensity, run theory analysis was used. Trends in rainfall, drought severity, magnitude, duration and intensity were computed by employing both parametric (simple linear regression) and non-parametric (Mann-Kendall and Sen's slope) tests, while spatial pattern maps of rainfall and drought characteristics were prepared using geographical information system. The analysis of rainfall records revealed a declining trend in eastern and central parts, whereas remaining areas of the basin witnessed an increasing trend during two time spans. During the study period, drought occurrence varied both geographically and temporally. The extreme, severe and moderate drought events were more common during monsoon season. Amongst the stations, Tapukara, Bairath and Mundawar rain gauge stations experienced the largest number of drought events compared to other stations. At both time scales, the most extreme droughts in the Sahibi basin occurred in 1979, 1986, 1987, 1989 and 2002. At the annual time span, the basin had the longest drought duration of 300 days, with a drought magnitude of - 758.3 mm. Likewise, the Tapukara rain gauge station had the longest dry spell of 310 days, followed by Behrod and Kotkasim (306 days each), Kotputli and Tijara (305 days each) and Mundawar (303 days). Finally, the findings of this study are expected to be useful to agricultural scientists, policymakers and water resource managers.
印度拉贾斯坦邦经常发生干旱;因此,探索半干旱的萨希比河流域的干旱严重程度对于干旱管理至关重要。为了研究干旱严重程度,在两个时间段应用了降雨异常指数(RAI),例如年(1 月至 12 月)和季风季节(6 月至 9 月),使用九个雨量站的长期每日降雨数据(1961-2017 年)。同样,为了检查各种干旱特征,如规模、持续时间和强度,使用了运行理论分析。通过使用参数(简单线性回归)和非参数(曼恩-肯德尔和森的斜率)检验计算了降雨、干旱严重程度、规模、持续时间和强度的趋势,同时使用地理信息系统编制了降雨和干旱特征的空间格局图。对降雨记录的分析表明,在两个时间段内,东部和中部地区的降雨呈下降趋势,而流域的其余地区则呈上升趋势。在研究期间,干旱的发生在地理和时间上都有所不同。极端、严重和中度干旱事件在季风季节更为常见。在各站中,Tapukara、Bairath 和 Mundawar 雨量站比其他站经历了更多的干旱事件。在两个时间尺度上,Sahibi 流域最极端的干旱发生在 1979 年、1986 年、1987 年、1989 年和 2002 年。在年时间跨度内,流域的干旱持续时间最长为 300 天,干旱规模为-758.3mm。同样,Tapukara 雨量站的干旱期最长,为 310 天,其次是 Behrod 和 Kotkasim(各 306 天)、Kotputli 和 Tijara(各 305 天)和 Mundawar(303 天)。最后,预计本研究的结果将对农业科学家、政策制定者和水资源管理者有用。