which can run from several weeks to four months. Despite this vulnerability, the history of drought and famine in the Sahel do not perfectly correlate. While modern scientific climate and rainfall studies have been able to identify trends and even specific periods of drought in the region, oral and written records over the last millennium do not record famine in all places at all times of drought. One 1997 study, in attempting to map long scale rainfall records to historical accounts of famine in Northern Nigeria, concluded that “the most disruptive historical famines occurred when the cumulative deficit of rainfall fell below 1.3 times the standard deviation of long-term mean annual rainfall for a particular place.” The 1982 to 1984 period, for instance, was particularly destructive to the pastoral Fula people of Senegal, Mali and Niger, and the Tuareg of northern Mali and Niger. The populations had not only suffered in the 1968 to 1974 period, but the inability of many to rebuild herds destroyed a decade earlier, along with factors as various as the shift of political power to settled populations with independence in the 1960s, Senegalese-Mauritanian border relations, and Niger's dependence upon falling world uranium prices coinciding in a destructive famine. 600–700 AD Surviving contemporary records of climate in the Sahel begin with early Muslim travellers in the early Medieval Warm Period. These suggest that Sahel rainfall was relatively low in the 7th and 8th centuries and then increased substantially from about 800 AD. There was a decline in rainfall from about 1300 AD, but an increase again around 200 years later. "Little Ice Age" droughts According to a study of West African drought based on Ghanaian lake sediments (not eyewitness historical accounts) published in the journal Science in April 2009: The most recent of these [multicentury droughts] occurred between 1400 and 1750 CE (550 to 200 yr B.P.), similar in timing to the Little Ice Age (LIA, 1400 to 1850 CE), a well-known interval when Northern Hemisphere temperatures were cooler than at present. In contrast with earlier studies, which reconstructed wetter conditions in East Africa during this period, evidence from Lake Bosumtwi supports more recent studies suggesting that this interval was dry. Evidence for LIA drought is not restricted to Africa, however. Records from throughout the tropics, including the western Pacific warm pool, the Arabian Sea, continental Asia, and tropical South America all show evidence for dry