Green Life Research Initiative Uganda Limited, Namulonge-Nabalanga, P.O. Box 1179, Wakiso, Uganda.
Directorate of Training and Research at Uganda National Meteorological Authority, Plot 21, 28 Port Bell Rd, P.O. Box 7025, Kampala, Uganda.
Environ Monit Assess. 2024 Sep 5;196(10):898. doi: 10.1007/s10661-024-12991-7.
Uganda in East Africa is experiencing highly variable rainfall which is exacerbated by temperatures warming at faster rates. This study analyzed rainfall and temperature patterns in comparison with the potential evaporation transpiration rates (PETs) for parts of Central, Western, Southern, and Southwestern Uganda for varying periods from 1981 to 2022. For rainfall onset date (OD), threshold of 0.85 mm for a rainy day, rainfall of 20 mm accumulated over 5 days with at least 3 rain days, and dry spell not exceeding 9 days in the next 30 days were used. The rainfall cessation dates (RCDs) are determined when water balance (WB) falls below 5 mm in 7 days in the last month of the expected season (May and December) for the first and second season, respectively. Standardized rainfall anomaly was utilized to show seasonal and annual rainfall variability. Pearson's correlation (r) coefficient was used to show the relationship between weather variables (rainfall, temperature) and PET at five rainfall stations. Results showed highly varied onset and cessation dates for March-May (MAM) seasonal rainfall compared to those of September-December (SOND). Results showed highly variable onset and cessation of rainfall over the region and statistically significantly increasing trends in both maximum and minimum temperatures across the region, with the highest rate of increase of maximum and minimum temperature of 0.70 and 0.65 °C per decade respectively. Moreover, the maximum temperature and PET showed strong positive correlation coefficient (r) that ranged from 0.76 to 0.90 across the regions, which likely contribute to excess evaporation from the surfaces, soil moisture deficits that negatively affect plant biomass production, low crop yields and food insecurity. PET and rainfall revealed insignificant statistical negative correlation as indicated by the correlation coefficient ranging from - 0.04 to - 0.22. We recommend water management and conservation practices such as mulching, zero tillage, agroforestry, planting drought-resistant crops, and using affordable irrigation systems during period of water deficit.
东非的乌干达经历着高度变化的降雨量,而气温变暖的速度则加剧了这一情况。本研究分析了 1981 年至 2022 年间乌干达中部、西部、南部和西南部部分地区的降雨和温度模式,并与潜在蒸散率(PET)进行了比较。对于降雨开始日期(OD),采用了 0.85 毫米的雨天阈值、5 天内累积 20 毫米的降雨、至少 3 天有雨的降雨、以及未来 30 天内不超过 9 天的干旱期。当预计季节(5 月和 12 月)最后一个月的 7 天内水平衡(WB)降至 5 毫米以下时,分别确定降雨结束日期(RCD)。利用标准化降雨异常来表示季节性和年际降雨变化。皮尔逊相关系数(r)用于表示五个降雨站的天气变量(降雨、温度)和 PET 之间的关系。结果表明,与 9 月至 12 月(SOND)的降雨相比,3 月至 5 月(MAM)季节性降雨的开始和结束日期变化较大。结果表明,该地区的降雨开始和结束高度变化,且整个地区的最高和最低温度都呈统计上显著的上升趋势,最高和最低温度的增长率分别为 0.70°C/十年和 0.65°C/十年。此外,最大温度和 PET 之间表现出很强的正相关系数(r),范围在 0.76 到 0.90 之间,这可能导致地表蒸发过多、土壤水分不足,从而对植物生物量生产产生负面影响、作物产量低和粮食不安全。PET 和降雨之间显示出统计学上无显著负相关,相关系数范围从-0.04 到-0.22。我们建议在水资源短缺期间采取水管理和保护措施,例如覆盖、免耕、农林复合、种植耐旱作物以及使用负担得起的灌溉系统。