Key Laboratory of Water Cycle & Related Land Surface Processes/Institute of Geographic Science and Natural Resources Research, Chinese Academy of Sciences, Beijing, 100101, China.
Qinghai Key Laboratory of Basin Water Cycle and Ecology, Qinghai Institute of Water Resources and Hydropower, Xining, China.
Sci Rep. 2019 Apr 19;9(1):6317. doi: 10.1038/s41598-019-42811-9.
An understanding of climate variability, trends, and prediction for better water resource management and planning in a basin is very important. Since the water resources of the Lake Chad basin (LCB) are highly vulnerable to changing climate, in the present study, a combination of trend analysis methods was used to examine the climate variability and trends for the period of 1951-2015 using observed and Climate Research Unit (CRU) data, and a combination of spectral analysis techniques was used for the prediction of temperature and precipitation using CRU data. Eighty-four percent of the temperature time series indicated extremely strong signals of increasing trends (α = 0.001) and 25-38% of the precipitation time series indicated strong decreasing trends (α = 0.05). Temperature is expected to increase and precipitation is expected to decrease in the future. However, surprisingly, in some regions located in the South, the temperature was predicted to decrease slightly in 2021-2030 relative to 2006-2015. This decrease might occur because these regions are highly protected natural resource areas and forests are frequently present. On the whole, the temperature was predicted to increase by 0.65-1.6 °C and precipitation was predicted to decrease by 13-11% in the next two decades (i.e., 2016-2025 and 2026-2035) relative to 1961-1990. Periodic analysis showed a 20- to 25-year cycle in precipitation in all basins and a 40- to 45-year cycle in temperature but only in the Chari-Logone basin.
了解气候变化的规律和趋势,对于更好地进行流域水资源管理和规划非常重要。由于乍得湖流域的水资源极易受到气候变化的影响,因此本研究采用趋势分析方法,利用观测数据和气候研究单位(CRU)数据,对 1951-2015 年期间的气候变化规律和趋势进行了研究,同时还利用 CRU 数据的谱分析技术对温度和降水进行了预测。84%的温度时间序列显示出极强的上升趋势信号(α=0.001),25-38%的降水时间序列显示出较强的下降趋势(α=0.05)。未来,温度预计将上升,降水预计将减少。然而,令人惊讶的是,在南部的一些地区,预计在 2021-2030 年与 2006-2015 年相比,温度将略有下降。这种下降可能是因为这些地区是高度保护的自然资源区,森林经常存在。总的来说,预计在未来二十年(即 2016-2025 年和 2026-2035 年)内,温度将上升 0.65-1.6°C,降水将减少 13-11%,与 1961-1990 年相比。周期性分析表明,所有流域的降水都存在 20-25 年的周期,温度存在 40-45 年的周期,但只有在乍得湖-洛贡流域存在这种周期。