Lake Tanganyika is located on the east of central Africa, and is shared by four developing countries: Democratic Republic of the Congo, Burundi, Tanzania and Zambia. It lies between 3◦20 ′ to 8◦45 ′ S and 29◦05 ′ to 31◦15′ E. It is about 650 km long and 50 km wide on average. The mean depth o
We study the fluctuations of the horizontal wind speed and of both the ambient air temperature and t...
International audienceNew intermediate-resolution, normal-incidence seismic reflection profiles from...
Lake Kivu in East Africa has gained notoriety for its prodigious amounts of dissolved methane and da...
[1] Intraseasonal thermocline oscillations in Lake Tanganyika are analysed using observations near M...
<p>White circles with black outlines indicate locations of in situ temperature measurement. The size...
The biggest reservoir of fresh water in Africa, second deepest lake in the world, and major reservoi...
It is generally believed that the Earth's rotation has negligible impact on the water circulation in...
Climate warming over the 20th century has increased the density stratification and stability of Lake...
An analysis is presented of the wind-induced thermocline oscillations of Lake Tanganyika, East Afric...
Lake Tanganyika is one of the largest lakes of Africa and second biggest Lake Considering the area a...
Lake Tanganyika, the deepest and most voluminous lake in Africa, has warmed over the last century in...
peer reviewedTen variables were measured at least twice per month at three locations of Lake Tangany...
The Lake Tanganyika trough derives from the distension of a late precambrian stabilized craton. The ...
Thermal structure, light attenuation, and chlorophyll- a dynamics within the upper 100 m at the nort...
Lake Kivu in East Africa has gained notoriety for its prodigious amounts of dissolved methane and da...
We study the fluctuations of the horizontal wind speed and of both the ambient air temperature and t...
International audienceNew intermediate-resolution, normal-incidence seismic reflection profiles from...
Lake Kivu in East Africa has gained notoriety for its prodigious amounts of dissolved methane and da...
[1] Intraseasonal thermocline oscillations in Lake Tanganyika are analysed using observations near M...
<p>White circles with black outlines indicate locations of in situ temperature measurement. The size...
The biggest reservoir of fresh water in Africa, second deepest lake in the world, and major reservoi...
It is generally believed that the Earth's rotation has negligible impact on the water circulation in...
Climate warming over the 20th century has increased the density stratification and stability of Lake...
An analysis is presented of the wind-induced thermocline oscillations of Lake Tanganyika, East Afric...
Lake Tanganyika is one of the largest lakes of Africa and second biggest Lake Considering the area a...
Lake Tanganyika, the deepest and most voluminous lake in Africa, has warmed over the last century in...
peer reviewedTen variables were measured at least twice per month at three locations of Lake Tangany...
The Lake Tanganyika trough derives from the distension of a late precambrian stabilized craton. The ...
Thermal structure, light attenuation, and chlorophyll- a dynamics within the upper 100 m at the nort...
Lake Kivu in East Africa has gained notoriety for its prodigious amounts of dissolved methane and da...
We study the fluctuations of the horizontal wind speed and of both the ambient air temperature and t...
International audienceNew intermediate-resolution, normal-incidence seismic reflection profiles from...
Lake Kivu in East Africa has gained notoriety for its prodigious amounts of dissolved methane and da...