摘要
This paper highlights the global warming of the lower atmosphere of West African tropical area using <em>in-situ</em> data. The study is based on the analysis of 500-m interval vertical profiles of radiosonde temperature above Niamey (13.47<span style="white-space:nowrap;">°</span>N;2.16<span style="white-space:nowrap;">°</span>E) a sub-Saharan meteorological station. The annual cycle of surface temperatures shows seasonally two peaks located in April/May and in October and two minimum in December/January and August respectively. In the mid-troposphere (between 5 km and 10 km height), time series of monthly mean temperatures from January 2001 to December 2018, shows an annual variability with a slight downward trend of -0.036<span style="white-space:nowrap;">°</span>C per decade. In the lower stratosphere (25 - 30 km altitude) a cooling of -0.64<span style="white-space:nowrap;">°</span>C/decade is observed. Temperatures time series also highlight the presence of two breaking points associated with the El Ni<span style="white-space:nowrap;">ñ</span>o-Southern Oscillation (ENSO) events. When performing a separation regarding Southern Oscillation Index (SOI) time series, model parameters of the linear regression indicate a tropospheric warming during the neutral and La Ni<span style="white-space:nowrap;">ñ</span>a phases and a stratospheric cooling. The analysis of the lower stratosphere zonal wind highlights different behaviours of the quasi-biennial oscillation (QBO) during the neutral and La Ni<span style="white-space:nowrap;">ñ</span>a phases.
This paper highlights the global warming of the lower atmosphere of West African tropical area using <em>in-situ</em> data. The study is based on the analysis of 500-m interval vertical profiles of radiosonde temperature above Niamey (13.47<span style="white-space:nowrap;">°</span>N;2.16<span style="white-space:nowrap;">°</span>E) a sub-Saharan meteorological station. The annual cycle of surface temperatures shows seasonally two peaks located in April/May and in October and two minimum in December/January and August respectively. In the mid-troposphere (between 5 km and 10 km height), time series of monthly mean temperatures from January 2001 to December 2018, shows an annual variability with a slight downward trend of -0.036<span style="white-space:nowrap;">°</span>C per decade. In the lower stratosphere (25 - 30 km altitude) a cooling of -0.64<span style="white-space:nowrap;">°</span>C/decade is observed. Temperatures time series also highlight the presence of two breaking points associated with the El Ni<span style="white-space:nowrap;">ñ</span>o-Southern Oscillation (ENSO) events. When performing a separation regarding Southern Oscillation Index (SOI) time series, model parameters of the linear regression indicate a tropospheric warming during the neutral and La Ni<span style="white-space:nowrap;">ñ</span>a phases and a stratospheric cooling. The analysis of the lower stratosphere zonal wind highlights different behaviours of the quasi-biennial oscillation (QBO) during the neutral and La Ni<span style="white-space:nowrap;">ñ</span>a phases.
作者
Pétronille Kafando
Bruno Korgo
Madé Fodé
Pétronille Kafando;Bruno Korgo;Madé Fodé(Laboratoire de Physique et de Chimie de l’Environnement, Université Joseph Ki-Zerbo, Ouagadougou, Burkina Faso;Laboratoire d’Energie Thermique et Renouvelable, Université Joseph Ki-Zerbo, Ouagadougou, Burkina Faso;Département de Physique, Faculté des Sciences et Techniques, Université Abdou Moumoumi, Niamey, Niger)