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The high population pressure induced higher risk to the urban residents as well as constrained urban growth over higher vulnerable zones.
High population pressure in the central highlands of Kenya has led to continuous cultivation of land with minimal additional inputs leading to soil nutrient depletion.
Research on such challenges must adopt an inclusive approach based on local knowledge supported by science-based analyses of the socio-ecological systems in the face of high population pressure and climate change.
The land is a scarce resource in the sub-watershed due to high population pressure and degradation.
This is due to the result that these areas were characterized by high population pressure and cultivated for long period of time (Kindu et al. 2013).
These are, particularly, common in areas where high population pressure exists whose livelihoods directly depend on the exploitation of natural resources in rural areas (Woldeamlak and Sterk 2005).
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However, higher herbicide and equipment costs penalized the no-till technology and it was only preferred under conditions of higher population pressure, which penalizes alternative fallow systems.
There is high population and grazing pressure in the KGR due to the increasing levels of immigration.
Global risks were projected to increase both from a changing climate and from socio-economic factors where population pressure is high or there is a high incidence of poverty.
While natural factors such as intermittent droughts and limited freshwater reserves can cause scarcity, high population growth imposes additional pressures.
The magnitude of interrill and rill erosion was determined on the northern slopes of the Uluguru Mountains, Tanzania which is representative for larger areas of East African Arch Mountains, where population pressure is high and land degradation is severe.
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