ABSTRACT
Kenya is a drought, famine and hunger prone country,
with considerable impact on agriculture, human health and livestock due to its
eco-climatic conditions. It contains only a few regions of high and regular
rainfall where arid and semi-arid lands cover 80% of the territory, therefore
periodical droughts are part of the climate system. Some
drought studies undertaken in Kenya used Standardized Precipitation Index (SPI)
which could not fully account for drought severity status as the role of
temperature increase on drought conditions was not taken into account. This study has tried to fill the gap by using Standardized Precipitation Evapotranspiration Index (SPEI), which includes precipitation, a temperature
component and evapotranspiration in its computations. SPEI and the Normalized Difference
Vegetation Index Anomaly (NDVI) were applied to characterize drought in Kenya
from 1987 to 2016, investigate the drought
severity and duration in the same period, assess drought trends together with
mapping of spatial distribution of drought in identified months, assessment of
Agricultural, meteorological and socio-economic activities. Correlation analysis was done to understand the response of climate and
satellite based drought monitoring indices results and the crop yield data. The
results and analysis obtained from the study showed that the years 1987, 1998, 2000, 2001, 2005, 2006, 2008,
2009, 2010, 2011 and 2015 were considered as drought years based on their SPEI
and NDVI anomaly results. They were classified as extremely dry, very dry and
moderately dry for meteorological drought and slight, moderate, severe and very
severe for Agricultural drought. SPEI results can be rated as being superior as
the element of temperature variation is taken into consideration.