Climate Variability in the Sudano-Guinean Transition Area and Its Impact on Vegetation: The Case of the Lamto Region in Côte D’Ivoire
Figure 6
(a) Mean atmospheric depth of the monsoon flow at Lamto calculated from the difference between 1000 hPa and the atmospheric level reached by the monsoon flow coming from the ocean. (b) Standardized anomalies of the atmospheric depth of the monsoon calculated from (a). Linear regression fits (red) of the five decades (1962–1971, 1972–1981, 1982–1991, 1992–2001 and 2002–2011) are plotted.
