Socio economic characteristics of cricket farmers in Lake Victoria region of Kenya

Author(s):  
Jackline A. Oloo ◽  
Afton Halloran ◽  
Maina J. Nyongesah
2008 ◽  
Vol 2 (4) ◽  
pp. e222 ◽  
Author(s):  
Michelle L. Steinauer ◽  
Ibrahim N. Mwangi ◽  
Geoffrey M. Maina ◽  
Joseph M. Kinuthia ◽  
Martin W. Mutuku ◽  
...  

2021 ◽  
pp. 002234332110384 ◽  
Author(s):  
Colleen Devlin ◽  
Sarah M Glaser ◽  
Joshua E Lambert ◽  
Ciera Villegas

Fisheries conflict is an underappreciated threat to the stability and health of communities. Declining fish populations, rising demand for seafood, and efforts to reduce illegal fishing are increasing the risk that conflict over fisheries resources will undermine stability and peace. Here, we investigate the frequency, causes, and consequences of fisheries conflict in six countries around the Horn of Africa and East Africa (Tanzania, Kenya, Somalia, Djibouti, Eritrea, and Yemen) between 1990 and 2017. Fisheries conflict events were cataloged from news reports, and events were characterized by the date, location, actors, consequences, and drivers of the conflict. We found the rate of fisheries conflict is gradually increasing in the region, with spikes in conflict driven by the arrival of foreign fishing boats or international naval vessels. Conflict was caused primarily by illegal fishing, foreign fishing, weak governance, limits on access to fishing grounds, and criminal activities including piracy. Two-thirds of all conflict events occurred in Kenyan and Somali waters, with areas of high conflict intensity in the Lake Victoria region, near the Somali coastline, and in the southern Red Sea. During this period, 684 fisheries conflict events in the region resulted in over 400 fatalities, nearly 500 injuries, and over 4,000 arrests.


2019 ◽  
Vol 147 (9) ◽  
pp. 3365-3390 ◽  
Author(s):  
Beth J. Woodhams ◽  
Cathryn E. Birch ◽  
John H. Marsham ◽  
Todd P. Lane ◽  
Caroline L. Bain ◽  
...  

Abstract The Lake Victoria region in East Africa is a hot spot for intense convective storms that are responsible for the deaths of thousands of fishermen each year. The processes responsible for the initiation, development, and propagation of the storms are poorly understood and forecast skill is limited. Key processes for the life cycle of two storms are investigated using Met Office Unified Model convection-permitting simulations with 1.5 km horizontal grid spacing. The two cases are analyzed alongside a simulation of a period with no storms to assess the roles of the lake–land breeze, downslope mountain winds, prevailing large-scale winds, and moisture availability. While seasonal changes in large-scale moisture availability play a key role in storm development, the lake–land-breeze circulation is a major control on the initiation location, timing, and propagation of convection. In the dry season, opposing offshore winds form a bulge of moist air above the lake surface overnight that extends from the surface to ~1.5 km and may trigger storms in high CAPE/low CIN environments. Such a feature has not been explicitly observed or modeled in previous literature. Storms over land on the preceding day are shown to alter the local atmospheric moisture and circulation to promote storm formation over the lake. The variety of initiation processes and differing characteristics of just two storms analyzed here show that the mean diurnal cycle over Lake Victoria alone is inadequate to fully understand storm formation. Knowledge of daily changes in local-scale moisture variability and circulations are keys for skillful forecasts over the lake.


Antiquity ◽  
1967 ◽  
Vol 41 (162) ◽  
pp. 146-147
Author(s):  
J. H. Chaplin

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