Mouchet J, Manguin S, Sircoulon J, Laventure S, Faye O, Onapa A W, Carnevale P, Julvez J, Fontenille D
ORSTOM, Paris, France.
J Am Mosq Control Assoc. 1998 Jun;14(2):121-30.
Different malarial situations in Africa within the past 40 years are discussed in order to evaluate the impact of climatic and human factors on the disease. North of the equator, more droughts and lower rainfall have been recorded since 1972; and in eastern and southern Africa, there have been alternating dry and wet periods in relation to El Niño. Since 1955, the increase in human population from 125 to 450 million has resulted in both expansion of land cultivation and urbanization. In stable malaria areas of West and Central Africa and on the Madagascar coasts, the endemic situation has not changed since 1955. However, in unstable malaria areas such as the highlands and Sahel significant changes have occurred. In Madagascar, cessation of malaria control programs resulted in the deadly epidemic of 1987-88. The same situation was observed in Swaziland in 1984-85. In Uganda, malaria incidence has increased more than 30 times in the highlands (1,500-1,800 m), but its altitudinal limit has not overcome that of the beginning of the century. Cultivation of valley bottoms and extension of settlements are in large part responsible for this increase, along with abnormally heavy rainfall that favored the severe epidemic of 1994. A similar increase in malaria was observed in neighboring highlands of Rwanda and Burundi, and epidemics have been recorded in Ethiopia since 1958. In contrast, in the Sahel (Niayes region, Senegal), stricken by droughts since 1972, endemic malaria decreased drastically after the disappearance of the main vector, Anopheles funestus, due to the destruction of its larval sites by cultivation. Even during the very wet year of 1995. An funestus did not reinvade the region and malaria did not increase. The same situation was observed in the Sahelian zone of Niger. Therefore, the temperature increase of 0.5 degree C during the last 2 decades cannot be incriminated as a major cause for these malaria changes, which are mainly due to the combination of climatic, human, and operational factors.
本文讨论了过去40年非洲不同的疟疾情况,以评估气候和人为因素对该疾病的影响。自1972年以来,赤道以北地区记录到更多干旱和更少降雨;在东非和南非,与厄尔尼诺现象相关的干湿期交替出现。自1955年以来,人口从1.25亿增加到4.5亿,导致了耕地扩张和城市化。在西非和中非以及马达加斯加海岸的稳定疟疾区,自1955年以来地方病情况没有变化。然而,在不稳定的疟疾区,如高地和萨赫勒地区,发生了重大变化。在马达加斯加,疟疾控制项目的停止导致了1987 - 1988年的致命疫情。1984 - 1985年在斯威士兰也观察到了同样的情况。在乌干达,高地(1500 - 1800米)的疟疾发病率增加了30多倍,但其海拔界限尚未突破本世纪初的水平。谷底耕种和定居点扩展在很大程度上导致了这种增加,同时异常大量的降雨助长了1994年的严重疫情。在卢旺达和布隆迪的邻近高地也观察到疟疾有类似增加,自1958年以来埃塞俄比亚也记录到了疫情。相比之下,在自1972年以来遭受干旱的萨赫勒地区(塞内加尔尼亚耶斯地区),由于主要病媒冈比亚按蚊的幼虫栖息地因耕种而遭到破坏,该地区的地方疟疾在主要病媒消失后急剧下降。即使在1995年非常湿润的年份,冈比亚按蚊也没有重新侵入该地区且疟疾没有增加。在尼日尔的萨赫勒地区也观察到了同样的情况。因此,过去20年0.5摄氏度的温度升高不能被归咎为这些疟疾变化的主要原因,这些变化主要是气候、人类和操作因素共同作用的结果。