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        <dc:title>Ghana</dc:title>
        <dc:creator>Nutsukpo, D K</dc:creator>
        <dc:creator>Jalloh, A</dc:creator>
        <dc:creator>Zougmore, R B</dc:creator>
        <dc:creator>Nelson, G C</dc:creator>
        <dc:creator>Thomas, T S</dc:creator>
        <dc:subject>Ghana</dc:subject>
        <dc:subject>Climate Change</dc:subject>
        <dc:subject>African Agriculture</dc:subject>
        <dc:subject>West Africa</dc:subject>
        <dc:description>Including inland water bodies, Ghana covers 238,539 square kilometers and&#13;
is located on the south central coast of West Africa. The country shares borders&#13;
in the east with Togo, in the north with Burkina Faso, and in the west&#13;
with Côte d’Ivoire. The topography of Ghana is mainly undulating, with most&#13;
slopes less than 5 percent and many not exceeding 1 percent. The topography&#13;
of the high rainforest is, however, mainly strongly rolling. The uplifted edges&#13;
of the Voltarian basin give rise to narrow plateaus between 300 and 600 meters&#13;
in elevation (Boateng 1998). Moving from the rainforest zone in the south to&#13;
the Sahara Desert in the north, rainfall generally decreases and temperature&#13;
increases. Rainfall is the most important climatic factor influencing vegetation&#13;
in Ghana. The wettest area is in the extreme southwest, where the rainfall is&#13;
over 2,000 millimeters per year. In the extreme north, the annual rainfall is less&#13;
than 1,100 millimeters. The driest area is at the southeastern coastal tip, where&#13;
the rainfall is about 750 millimeters. Much of the rain falls in intense storms&#13;
of short duration, especially at the beginning of the season, resulting in heavy&#13;
runoff and erosion. The annual mean relative humidity is about 80 percent in&#13;
the south and 44 percent in the north (Dickson and Benneh 1988). The mean&#13;
monthly temperature for the entire country is 25°C. Although temperatures&#13;
are uniformly moderate, there are important variations over different parts of&#13;
the country, reflecting altitude and distance from the sea...</dc:description>
        <dc:publisher>International Food Policy Research Institute</dc:publisher>
        <dc:contributor>Jalloh, A</dc:contributor>
        <dc:contributor>Nelson, G C</dc:contributor>
        <dc:contributor>Thomas, T S</dc:contributor>
        <dc:contributor>Zougmore, R B</dc:contributor>
        <dc:contributor>Roy-Macauley, H</dc:contributor>
        <dc:date>2013</dc:date>
        <dc:type>Book Section</dc:type>
        <dc:type>PeerReviewed</dc:type>
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        <dc:language>en</dc:language>
        <dc:identifier>http://oar.icrisat.org/10797/1/CHAPTER%206.pdf</dc:identifier>
        <dc:identifier>  Nutsukpo, D K and Jalloh, A and Zougmore, R B and Nelson, G C and Thomas, T S  (2013) Ghana.   In:  West African agriculture and climate change: A comprehensive analysis.   IFPRI’s climate change in Africa series .  International Food Policy Research Institute, Washington, pp. 141-172.  ISBN 978-0-89629-204-8     </dc:identifier></oai_dc:dc>
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