Open AccessTrends and variability in pan evaporation and other climatic variables at Ibadan, Nigeria, 1973–2008
Author(s) -
Oguntunde Philip G.,
Abiodun Babatunde J.,
Olukunle Olawale J.,
Olufayo Ayorinde A.
Publication year - 2012
Publication title -
meteorological applications
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.672
H-Index - 59
eISSN - 1469-8080
pISSN - 1350-4827
DOI - 10.1002/met.281
Subject(s) - pan evaporation , environmental science , monsoon , relative humidity , climatology , geography , wind speed , vapour pressure deficit , atmospheric sciences , evaporation , meteorology , chemistry , biochemistry , photosynthesis , transpiration , geology
Understanding changes in evaporation rates is expected to be of great importance for water resource planning and management. This paper examines pan evaporation data as an example of the detection and attribution of trends in climate variables. Records of pan evaporation ( E pan ), rainfall ( R ), radiation ( S R ), wind speed ( W S ), temperature ( T a ) and humidity ( R H ) for the period 1973–2008 were collected from the International Institute of Tropical Agriculture (IITA) in Ibadan, Nigeria. Mann–Kendall trend and Sen's slope tests were performed on the respective meteorological variables and a variability index (VI) was also computed for these. The results showed that annually E pan , S R and W S significantly decrease ( P < 0.001) while R , T a , and R H showed insignificant increasing trends in the last four decades. E pan and S R decrease at the rate of 8.3 mm year −2 and 37.8 MJ m −2 year −1 , respectively. Similar to E pan , S R decreased significantly in all the months ( P < 0.01) and the reduction ranged from 5.1% per decade in March to 9.3% per decade in August. The result of VI showed that the decrease in E pan and other explanatory variables is rather recent. Regression between E pan and other variables indicates that about 30, 15 and 6% of its variance can be explained by S R , W S and VPD (vapour pressure deficit), respectively. The possible roles of dust‐haze known as ‘harmattan’ winds and monsoon clouds in attenuating S R and hence reducing E pan are discussed. Copyright © 2011 Royal Meteorological Society