My research area of interest is renewable energy. Since energy is the engine of everything that does many works. For my research specifically on Organic Solar Cells’ power conversion performance using Plasmonic Nanoparticles at different layers of inverted Organic solar cells, I am studying the title “Unraveling Plasmon-Coupled Power Conversion Efficiency Enhancement in Wide-Band Gap Polymers-Based Organic Solar Cells: Both Experimental and Computational Approaches” at Addis Ababa University under the supervisors of Prof. Newayemedihin Aberra Tegegn and Dr. Nika Bekri Abdullah from Ethiopia. This study aims to solve the world’s energy problem and the Horn of Africa, which will contribute to the future of the rift specifically Ethiopia because Ethiopia is found in the Horn of Africa and is one of the parts of the rift.

Based on the field trip experience, I observed the people were faced with a lot of climate uncertainties ” extreme weather events” leading to the occurrence of drought and flood interchangeable over years. The decline of natural resources within rift could be as a result of climate and environmental change which have been intensify by human activities. Other identify problems were as follows;

1. The Maasai pastoralist lived with their cattle’s within the rift which gave room for water contamination and other related sanitation issues resulting to water related illness among the populace which could affect their productivities (output).
2. The increasing population (human and animals) over the years could cause conflict between the farmers and pastoralist due to shrinking land for farming (rain fed agriculture) and grazing over the years.
3. There evidence of sheet and rill erosion process which could affect the fertility and condition of arable land for rain fed agriculture.
4. Depreciation of the ecological services within the Maasai conservation area of the rift was observe and needs urgent attention.
5. Drought and flood have affected the livelihood, health and well begin of the Massai people of the rift.
6. The people are living in hamlet and in dispersed form of settlement which could be difficult for the Narok government to provide preventive measures against diseases like malaria and water relate problems to the people.
7. There is need to understand the past climate before the development of the rift, present micro climate and predict what the future micro climate will be within the rift system. These will give more light on the implications

Quaternary studies in the field of animal communities with integrated approaches of paleontology, zooarchaeology and taphonomy. Actualist and (paleo)eco-ethological studies, especially on human and animal predation. Reconstruction of paleoenvironments and climatic context in the Plio-Pleistocene.

Research themes: Late Pleistocene and early Holocene hunter-gatherer societies in Africa. I am interested in the organization of hunter-gatherer lithic technology, especially stone procurement. My research explores how technological organization can be studied to understand the major evolutionary and demographic changes of the last hundred-thousand years in Africa.

Christine Adongo is currently an early stage researcher doing PhD at l’Ecole des Hautes Etudes en Sciences Sociales (EHESS – Paris), and a member of Institut Interdisciplinaire d’Anthropologie du Contemporaire (IIAC). She attained both her bachelors and Masters degrees in Environmental science at Kenyatta University in Nairobi, Kenya. Broadly, her research interests encompass environment, natural resources, local landscapes, pastoral socio-ecological transition and livelihoods. More specifically, she has worked on natural resources conservation and livelihoods, focusing on the Kenya coastal sacred Kaya forests, and pastoral futures in northern Kenya in so far as climate change adaptation and WASH management at the local level in concerned. Her most work focuses on ‘green’ projects’ implementation (geothermal energy project in Kenya) and their socio-ecological and livelihood implications on the resilience of local pastoral landscape. Christine will use the mobility funds from GDR as a post-doctoral undertaking, to advance her fieldwork and facilitate the dissemination of her work on the contested futures of geothermal in the greater Olkaria geothermal area in Kenya’s rift valley.

My PhD research is about finding and dating cryptotephras in marine sediment cores around the Horn of Africa, over the last million years. The aims are : to provide a tephrostratigraphic framework, and to correlate these tephras with tuffs from the East African Rift (e.g. Silver Tuff from Konso, Ethiopia) using glass shard geochemistry. The outcomes are : the age of hominin fossils, palaeoclimatology of the area, and volcanic history of the East African Rift System.

I study fossil pollen and phytoliths as paleobotanical markers of past vegetation in order to reconstruct paleovegetations associated with Mio-Pliocene and Pleistocene hominins in Central and East Africa.

I am interested in the interactions between plants, vegetation and present-day climate in the tropics, and the influence of these three factors on botanical markers for tracing climatic and plant community changes in the past. Since 2018, I have been participating in the OGRE paleontological mission in the Shungura Formation, Omo Valley, Ethiopia.

I am a limnogeologist based at the Institut National de Recherches Archéologiques Preventives (National Institute of Preventative Archaeological Research, or INRAP) in Lyon, France. Prior to joining the WTAP in 2010 and refocusing my work on the East African Rift System (EARS) I worked at Lake Baikal in central Asia.

Limnogeology is the study of sediments formed by inland waters (e.g. lakes, ponds, rivers, wetlands), and in West Turkana my specific research interest is the sedimentary cyclicity and temporal evolution of lake deposits, which I use to reconstruct past climatic, tectonic, and environmental changes and how they influenced hominin evolution during the Plio-Pleistocene. My approach involves identifying sequences of ancient lake sediments where they are exposed in the Nachukui Formation and performing detailed sediment analyses to determine the processes and contexts (deep, shallow, endorheic etc) that led to their deposition. As the largest endorheic water body in a desert on earth, Lake Turkana has undergone remarkable changes in size, shape, and hydrology over time, and has played a key role in affecting the environments and locations that were available for hominins to exploit.