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<title>Doctoral</title>
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<description/>
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<rdf:li rdf:resource="http://197.159.135.214/jspui/handle/123456789/1088"/>
<rdf:li rdf:resource="http://197.159.135.214/jspui/handle/123456789/1087"/>
<rdf:li rdf:resource="http://197.159.135.214/jspui/handle/123456789/1086"/>
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<dc:date>2026-04-23T15:09:13Z</dc:date>
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<item rdf:about="http://197.159.135.214/jspui/handle/123456789/1088">
<title>Land Use Land Cover and Climate Change Impacts on Agro- Ecosystem Services Provisioning in Riverine Areas of Pendjari Reserve in Benin, West Africa</title>
<link>http://197.159.135.214/jspui/handle/123456789/1088</link>
<description>Land Use Land Cover and Climate Change Impacts on Agro- Ecosystem Services Provisioning in Riverine Areas of Pendjari Reserve in Benin, West Africa
Makponse, Dossa Armand
Examining the effects of land use and land cover change (LULCC) on biodiversity loss and human wellbeing in the Pendjari Reserve, a biodiversity hotspot in West Africa that has seen human disturbances for years, is the primary goal of this study. The study employed Landsat images and utilized the Random Forest classification software to analyze the dynamics of LULC for 1998, 2007, 2013, and 2020. The expected LULC for 2035 was projected using Terset 18.21. To learn more about household socio- economics characteristics and the advantages of trees in the townships from Tanguieta and Materi, information from 361 farmers was gathered. The influence of farm size, landholding, and district on tree diversity, tree species richness, and tree abundance, were examined as their combined impacts. The study unveiled notable alterations in LULC patterns, such as a reduced wooded savannah and a rise in shrub, cropland, and fallow land. Settlement areas experienced an increase in the studied period. The predicted results indicated an imminent slight decrease in wooded savannah, increase in shrub savannah, cropland, and fallow land, as well as a reduction of settlement areas in the future. Furthermore, farmers' preferences for tree and crop associations were assessed, with Parkia biglobosa identified as the tree species with the largest mean diameter at breast height (dbh) and height. At the same time, Vitellaria paradoxa had the highest height in Materi and Tanguieta. Tree benefits played a crucial role in selecting trees for agroforestry systems, with provisioning services followed by supporting services being the most common ecosystem benefits derived by local communities. Tree-crop associations varied among the farmers. The study examined the effects of tree conservation on agricultural output in agroforestry systems within the same study region as well as the impact of climate trends on critical crop yields. Findings revealed a substantial positive (warming) trend in temperature and a decrease in rainfall. There was a general positive warming trend observed between 1981 to 2020. Results showed that the lowest temperature positively and considerably impacted maize yields, while rainfall and relative humidity adversely affected respectively negatively and positively maize yields. The minimum temperature and relative humidity had a positive and substantial impact on sorghum. The maximum temperature and relative humidity negatively impacted cotton yield, but rainfall had affected positively cotton yields. Maximum and minimum temperature positively and significantly impacted cowpea yields. The Exponential regression model indicated that soil physicochemical characteristics and distance between tree and crop were the primary variables influencing crop yields in agroforestry systems. Furthermore, the study demonstrated that the maximum carbon stored by wooded savannah was projected to be 494,198.1 Mg C ha-1 in 2050, which decreased to 387,059.4 Mg C ha-1 in 2020 and 387,047.2 Mg C ha-1 in 2035. The lowest value of carbon is projected to be sequestered from 2020 to 2035, over a period of fifteen years. The highest gain and loss of projected carbon to sequestered for the period 2020 - 2050 is 108,947 Mg C ha-1 and -57, 996 Mg C ha-1 and the period 2035 -2050 is 108878 Mg C ha-1 and -57984.6 Mg C ha-1, respectively. Conversely, the lowest gain and loss were anticipated from 2020 to 2035, with value of 845.56 Mg ha-1 and -47.52 Mg C ha-1, respectively.
A Thesis submitted to the West African Science Service Centre on Climate Change and Adapted Land Use and the Kwame Nkrumah University of Science and Technology, Kumasi, Ghana, in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Climate Change and Land Use
</description>
<dc:date>2023-08-01T00:00:00Z</dc:date>
</item>
<item rdf:about="http://197.159.135.214/jspui/handle/123456789/1087">
<title>Adoption and Effects of Climate Change Adaptation, and Land Use Decision of Smallholders Farmers in the Saline Area of Sine-Saloum, Fimela Senegal</title>
<link>http://197.159.135.214/jspui/handle/123456789/1087</link>
<description>Adoption and Effects of Climate Change Adaptation, and Land Use Decision of Smallholders Farmers in the Saline Area of Sine-Saloum, Fimela Senegal
Thiam, Habibatou Ibrahima
Soil salinity expansion is one of the most severe land degradation issues confronting farmers in Senegal, particularly in coastal areas such as Fimela.&#13;
With sea level rise, temperature rise, and rainfall decrease, soil salinity is increasing significantly. It has a negative impact on crop yields and farmers' livelihoods. Farmers developed land use adaptation strategies to deal with soil salinity. Nonetheless, despite adaptations, some farmers continue to complain about the negative impact of soil salinity on their outcomes. Then, this study investigates farmers' adaptation, the different factors that influence it, its implications for smallholder farmers' livelihoods, and farmers' perception of soil salinity and its impact. Data from face-to-face interviews of 288 households using the Krejci and Morgan’s formula and GPS coordinates of households and each of their farms was collected. An agent-based model was used to understand land use adaptation to soil salinity expansion by considering farmers' perceptions of soil salinity expansion under climate change for simulation. A sub-model of household decisions, crop yield, and perception of soil salinity was developed and incorporated into the model. Three scenarios were considered to simulate the interaction between household agents and landscape agents over 25 years. Farmers' adoption is influenced by their assets and sociopsychological factors like threat assessment, coping assessment, and subjective norms. Farmers in Fimela do not have maladaptation thinking that may break their willingness to adopt strategies to cope with soil salinity. The ESR model shows that farmers' adoption of strategies to cope with soil salinity has a positive impact on groundnut yields and a negative influence on food security but has no significant effect on their millet yields. These findings have been validated by the simulation results, which show that the yield difference between farmers who perceive soil salinity expansion and those who do not is significant for groundnut but not millet over 25 years. As a result, it is critical to base policies in combating soil salinity effects on providing better methods of soil salinity adaptation strategies through scientific research. Policies should support a few pilot farmers in these precise and effective strategies to trigger other farmers to follow through the village and social influence by the farmer-to-farmer approach to enable farmers access and appropriation of these new methods.
A Thesis submitted to the West African Science Service Centre on Climate Change and Adapted Land Use and the Kwame Nkrumah University of Science and Technology, Kumasi, Ghana, in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Climate Change and Land Use
</description>
<dc:date>2023-07-01T00:00:00Z</dc:date>
</item>
<item rdf:about="http://197.159.135.214/jspui/handle/123456789/1086">
<title>Crops-Livestock Integration as a Resilience Strategy to Climate Change in Burkina Faso</title>
<link>http://197.159.135.214/jspui/handle/123456789/1086</link>
<description>Crops-Livestock Integration as a Resilience Strategy to Climate Change in Burkina Faso
Sanou, Charles Lamoussa
This study titled addressed a topical issue of climate change and its impacts on&#13;
farmers' livelihoods and the role that an integrated crop-livestock system can play in&#13;
building resilient farmers and agricultural systems. The research first of all analysed&#13;
historical climate (rainfall, minimum and maximum temperature) trends across three&#13;
climatic zones Sudan (Dano), Sudan-Sahel (Niou) and Sahel (Dori)) at annual,&#13;
seasonal and decadal scales. Climates indices computation was done using the&#13;
package ClimPACT2 GUI in R software. Annual and seasonal climate were&#13;
compared using the independent t-test. Decadal climate indices were subjected to a&#13;
Principal Component Analysis (PCA). The research also analysed the susceptibility&#13;
or sensibility of crop production and livestock health to climate change. Thirdly, the&#13;
research developed and/or updated measurement tool known as Crop-Livestock&#13;
Integration (CLI) indicators for a holistic characterisation of integrated croplivestock&#13;
system. These indicators were developed based on the information from&#13;
589 farmers’ households and secondary data. Above ground, data were collected&#13;
from 4,733 trees over a total land area of 243.2 ha (80.1 ha, 78.8 ha and 84.3 ha in&#13;
Sudan, Sudan-Sahel and Sahel zones, respectively). Due to the Sahel zone's&#13;
insecurity, soil data could be collected only within Sudan and Sudan-Sahel zones. In&#13;
total, 120 composite soil samples were collected for this purpose and 240 other&#13;
samples for soil bulk density determination. Results revealed changes in climate&#13;
conditions, more pronounced in temperature variations than in rainfall. In the&#13;
Sudan-Sahel and Sahel zones, a re-wetting trends was observed over the last decade&#13;
supporting the re-greening hypothesis of the Sahel. Despite some positive effects of&#13;
the climate indices, crop failure was the major impact of climate pejoration across zones. Similarly, livestock health was majorly negatively affected by climate&#13;
deterioration though the resurgence of diseases due to climate change. Climate&#13;
indices could explain 23.0 - 50.2 % of the variations in crop yield and an increased&#13;
cases of livestock diseases occurrence by 1-9.4 units due to the deterioration in&#13;
climate conditions across climatic zones. Changes in climatic conditions may also&#13;
induce microbial proliferation and host susceptibility to result in the emergence,&#13;
redistribution, and changes in the incidence and intensity of pest infestations. The&#13;
study concluded that crop-livestock integration is underperforming in Burkina Faso&#13;
and can be improved. Majority farmers (91.6 %) in the Sudan-Sahel zone are&#13;
practising full crop-livestock integration, unlike the Sahel (62.3%) and Sudan&#13;
(48.2%) zones. However, only 14.8%, 10.5% and 5.1 % showed the effectiveness of&#13;
integration in the Sudan-Sahel, Sahel and Sudan zones, respectively. CLI was&#13;
comparatively more effective in Sudan-Sahel (65.9±32.0 %) than Sahel (44.9±29.5&#13;
%) and Sudan zones (35.6±35.0 %). Integration indicators were significantly&#13;
associated with farm emissions, productivity, biodiversity and soils nutrients. CLI is&#13;
also a tree-based system with high sequestration potential that could significantly&#13;
counterbalance the whole system emissions. However, the coverage of fodder needs&#13;
is negatively associated with soils nutrients content indicating field nutrient mining if&#13;
an appropriate scheme of nutrient return to the soils as manure is not set. An&#13;
adequate combination of CLI components offers an opportunity to build resilient&#13;
farming systems in Burkina Faso to adapt to the changing climate.
A Thesis submitted to the West African Science Service Centre on Climate Change and Adapted Land Use and the Kwame Nkrumah University of Science and Technology, Kumasi, Ghana, in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Climate Change and Land Use
</description>
<dc:date>2023-07-01T00:00:00Z</dc:date>
</item>
<item rdf:about="http://197.159.135.214/jspui/handle/123456789/1085">
<title>Drought-Heatwaves’ Dynamics with Land Use Land Cover Types under the West African Monsoon System</title>
<link>http://197.159.135.214/jspui/handle/123456789/1085</link>
<description>Drought-Heatwaves’ Dynamics with Land Use Land Cover Types under the West African Monsoon System
Heatwaves are prolonged periods of abnormal heat that can adversely impact human&#13;
and animal well-being, public infrastructure, agriculture, wildfire occurrence and&#13;
severity, and workplace efficiency. With increasing global warming, heatwaves and&#13;
droughts are predicted to worsen. However, there are only a few documented cases of&#13;
heatwaves in Africa, and less research in West Africa has explored the&#13;
thermodynamics of heatwaves in the region. This study seeks to comprehensively&#13;
investigate the dynamics of heatwaves, particularly their interaction with landatmosphere&#13;
processes and droughts as compound events in three climate zones in&#13;
West Africa. The research compares heatwave and heat-stress occurrences and their&#13;
coincidental intensity with drought, using satellite, reanalysis, and in-situ datasets&#13;
from 1981 to 2020. The study uses Cumulative Heat (CumHeat or Heatcum) and&#13;
Universal Thermal Climate Index (UTCI) to measure heatwaves, Standardized&#13;
Precipitation (Evapotranspiration) Index (SPI or SPEI) for drought, and Normalized&#13;
CumHeat for temperature (Tmax and Tmin), UTCI, and Wet-Bulb Globe Temperature&#13;
(WBGT) to examine heatwave dynamics. The study employs the ECMWF Year of&#13;
Polar Prediction (YOPP) dataset to determine the main temperature advection and&#13;
tendency terms that contribute to heatwaves in selected cases (2018, 2019, and 2020)&#13;
covering different climate zones, from 1000 hPa, 925 hPa, to 850 hPa, and 700 hPa.&#13;
The study also uses validated coupled RegCM-CLM simulation outputs initialized&#13;
with soil moisture to compute SPEI and the normalized heatwave indices. The&#13;
Drought-heatwave (D-HW) events from observational data showed lower frequency&#13;
and intensity than the gridded dataset. The West African monsoon system is&#13;
experiencing an increase in the intensity and duration of UTCI and Tmax heatwaves,&#13;
mainly before or after the monsoon phase, with some occurrences during the&#13;
monsoon phase. An increasing trend in the intensity and duration of heatwaves, up to&#13;
40 days, has been observed in the gridded dataset, and there is a higher likelihood of&#13;
WBGT occurrence during the night. The study found that the differences in heatwave&#13;
indices are primarily due to the sensitivity to moisture and wind. The intensity of&#13;
heatwaves exhibits asymmetric statistical responses to moisture content deficits,&#13;
particularly in the Guinea zone and some parts of Sudan (Coast of Senegal). In the&#13;
Eastern part of West Africa, the opposite reaction to mid-latitudes is observed, where&#13;
there is an increase in moisture before and during a high heatwave. The impact of&#13;
soil moisture on heatwaves extends to the 6th level (8th level) about 0.492912 m&#13;
(1.38283 m) into the soil. These findings could help improve weather forecasting,&#13;
predict the impacts of heatwaves, and design adaptation strategies to reduce the&#13;
vulnerability of populations to heatwaves. Additionally, the results contribute to&#13;
developing more accurate and robust climate models that can better simulate the&#13;
behaviour of heatwaves and their interactions with other climate variables.
A Thesis submitted to the West African Science Service Centre on Climate Change and Adapted Land Use and the Kwame Nkrumah University of Science and Technology, Kumasi, Ghana, in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Climate Change and Land Use
</description>
<dc:date>2023-08-01T00:00:00Z</dc:date>
</item>
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