Situma Silvia, Nyakarahuka Luke, Omondi Evans, Mureithi Marianne, Mweu Marshal, Muturi Matthew, Mwatondo Athman, Dawa Jeanette, Konongoi Limbaso, Khamadi Samoel, Clancey Erin, Lofgren Eric, Osoro Eric, Ngere Isaac, Breiman Robert F, Bakamutumaho Barnabas, Muruta Allan, Gachohi John, Oyola Samuel O, Njenga M Kariuki, Singh Deepti
medRxiv. 2024 May 17:2024.05.17.24307534. doi: 10.1101/2024.05.17.24307534.
Recent epidemiology of Rift Valley fever (RVF) disease in Africa suggests growing frequency and expanding geographic range of small disease clusters in regions that previously had not reported the disease. We investigated factors associated with the phenomenon by characterizing recent RVF disease events in East Africa.
Data on 100 disease events (2008 - 2022) from Kenya, Uganda, and Tanzania were obtained from public databases and institutions, and modeled against possible geo-ecological risk factors of occurrence including altitude, soil type, rainfall/precipitation, temperature, normalized difference vegetation index (NDVI), livestock production system, land-use change, and long-term climatic variations. Decadal climatic variations between 1980-2022 were evaluated for association with the changing disease pattern.
Of 100 events, 91% were small RVF clusters with a median of one human (IQR, 1-3) and 3 livestock cases (IQR, 2-7). These clusters exhibited minimal human mortality (IQR 0-1), and occurred primarily in highlands (67%), with 35% reported in areas that had never reported RVF disease. Multivariate regression analysis of geo-ecological variables showed a positive correlation between occurrence and increasing temperature and rainfall. A 1oC increase in temperature and 1-unit increase in NDVI, 1-3 months prior were associated with increased RVF incidence rate ratios (IRR) of 1.20 (95% CI 1.1,1.2) and 9.88 (95% CI 0.85, 119.52), respectively. Long-term climatic trends showed significant decadal increase in annual mean temperature (0.12 to 0.3oC/decade, P<0.05), associated with decreasing rainfall in arid and semi-arid lowlands but increasing rainfall trends in highlands (P<0.05). These hotter and wetter highlands showed increasing frequency of RVF clusters, accounting for 76% and 43% in Uganda and Kenya, respectively.
These findings demonstrate the changing epidemiology of RVF disease. The widening geographic range of disease is associated with climatic variations, with the likely impact of wider dispersal of virus to new areas of endemicity and future epidemics.
Rift Valley fever is recognized for its association with heavy rainfall, flooding, and El Niño rains in the East African region. A growing body of recent studies has highlighted a shifting landscape of the disease, marked by an expanding geographic range and an increasing number of small RVF clusters. This study challenges previous beliefs about RVF, revealing that it predominantly occurs in small clusters rather than large outbreaks, and its association with El Niño is not as pronounced as previously thought. Over 65% of these clusters are concentrated in the highlands of Kenya and Uganda, with 35% occurring in previously unaffected regions, accompanied by an increase in temperature and total rainfall between 1980 and 2022, along with a rise in the annual number of rainy days. Notably, the observed rainfall increases are particularly significant during the short-rains season (October-December), aligning with a secondary peak in RVF incidence. In contrast, the lowlands of East Africa, where typical RVF epidemics occur, display smaller and more varied trends in annual rainfall. The worldwide consequence of the expanding RVF cluster is the broader dispersion of the virus, leading to the establishment of new regions with virus endemicity. This escalation heightens the risk of more extensive extreme-weather-associated RVF epidemics in the future. Global public health institutions must persist in developing preparedness and response strategies for such scenarios. This involves the creation and approval of human RVF vaccines and therapeutics, coupled with a rapid distribution plan through regional banks.
非洲裂谷热(RVF)疾病的最新流行病学研究表明,在以前未报告过该疾病的地区,小规模疾病聚集的频率不断增加,地理范围不断扩大。我们通过描述东非最近的裂谷热疾病事件,调查了与这一现象相关的因素。
从公共数据库和机构获取了2008 - 2022年来自肯尼亚、乌干达和坦桑尼亚的100起疾病事件的数据,并针对可能的发生地地理生态风险因素进行建模,这些因素包括海拔、土壤类型、降雨/降水量、温度、归一化植被指数(NDVI)、畜牧生产系统、土地利用变化和长期气候变化。评估了1980 - 2022年十年间的气候变化与不断变化的疾病模式之间的关联。
在100起事件中,91%是小规模裂谷热聚集,其中位值为1例人类病例(四分位距,1 - 3)和3例牲畜病例(四分位距,2 - 7)。这些聚集导致的人类死亡率极低(四分位距0 - 1),主要发生在高地(67%),35%的事件报告发生在从未报告过裂谷热疾病的地区。对地理生态变量的多变量回归分析显示,疾病发生与温度升高和降雨增加呈正相关。温度每升高1℃以及事件发生前1 - 3个月NDVI每增加1个单位,裂谷热发病率比值(IRR)分别增加1.20(95%置信区间1.1, 1.2)和9.88(95%置信区间0.85, 119.52)。长期气候趋势显示年平均温度有显著的十年期升高(0.12至0.3℃/十年,P<0.05),这与干旱和半干旱低地降雨量减少相关,但高地降雨量呈增加趋势(P<0.05)。这些更炎热且更湿润的高地裂谷热聚集频率增加,分别占乌干达和肯尼亚的76%和43%。
这些发现表明裂谷热疾病的流行病学正在发生变化。疾病地理范围的扩大与气候变化相关,可能会使病毒更广泛地传播到新的流行地区并引发未来的疫情。
裂谷热在东非地区因与暴雨、洪水和厄尔尼诺降雨有关而为人所知。最近越来越多的研究强调了该疾病格局的变化,其特点是地理范围不断扩大以及小规模裂谷热聚集数量不断增加。这项研究挑战了以往对裂谷热的认知,揭示出它主要以小规模聚集而非大规模爆发的形式出现,并且其与厄尔尼诺的关联并不像之前认为的那么明显。这些聚集中超过65%集中在肯尼亚和乌干达的高地,35%发生在以前未受影响的地区,同时1980年至2022年间温度和总降雨量增加,雨日数量也有所上升。值得注意的是,观察到的降雨增加在短雨季节(10月至12月)尤为显著,与裂谷热发病率的第二个高峰一致。相比之下,东非典型裂谷热疫情发生的低地,年降雨量变化较小且趋势多样。裂谷热聚集范围扩大在全球范围内的后果是病毒更广泛地传播,导致新的病毒流行地区出现。这种情况的升级增加了未来与极端天气相关的更广泛裂谷热疫情的风险。全球公共卫生机构必须持续制定针对此类情况的防范和应对策略。这包括研发和批准人类裂谷热疫苗及治疗方法,并通过区域储备库制定快速分发计划。