基于机载传感器和实地测量的西非气溶胶光学特性的气候分析:以萨赫勒地区为例

Nébon Bado, A. Ouedraogo, H. Guengane, T. S. M. Ky, S. D. Bazyomo, B. Korgo, M. Drame, S. Sall, F. Kiéno, D. Bathiébo
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引用次数: 3

摘要

本文基于2001年至2016年间的卫星和现场测量,研究了西非气溶胶的气候学,涵盖了萨赫勒地区的四个地点。尼日尔、马里、塞内加尔和布基纳法索分别有巴尼祖姆布(13.541°N,02.665°E)、辛扎纳(13.278°N,05.934°W)、达喀尔(14.394°N,16.959°W)和瓦加杜古(12.20°N,1.40°W)。因此,卫星观测和现场测量之间的相互比较显示,MODIS和AERONET之间具有良好的相关性,Cinzana的相关系数R=0.86,Banizounbou的相关系数R=0.85,瓦加杜古的相关系数P=0.84,达喀尔现场计算的相关系数低,R=0.66。与MODIS一样,SeaWiFS与地面光度计的测量结果显示出非常好的一致性,尤其是Banizoumbou(R=0.89),Cinzana(R=0.88)和Dakar(R=0.75),然后在瓦加杜古现场计算出低相关系数(R=0.64)。这些机载传感器的性能也通过均方根误差(RMSE)和平均绝对误差(MAE)的计算得到证实。在此验证之后,基于气溶胶光学深度(AOD)的气候分析显示,西非气溶胶的季节性受到MERRA模型再分析所示气候动力学的强烈影响。气溶胶的这种季节性空间分布证明了在萨赫勒地区不同地点观测到的颗粒物的时间变异性。此外,AOD和Angstrom系数的综合分析表明,萨赫勒地区春季(3月至4月至5月)和夏季(6月至7月至8月)的气溶胶期。然而,这些气溶胶主要由沙漠尘埃主导,其主要来源位于撒哈拉以北和萨赫勒地区。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Climatological Analysis of Aerosols Optical Properties by Airborne Sensors and in Situ Measurements in West Africa: Case of the Sahelian Zone
This paper deals with the climatology of aerosols in West Africa based on satellite and in situ measurements between 2001 and 2016 and covers four sites in the Sahelian zone. There are indeed Banizoumbou (13.541°N, 02.665°E), Cinzana (13.278°N, 05.934°W), Dakar (14.394°N, 16.959°W) and Ouagadougou (12.20°N, 1.40°W) located respectively in Niger, Mali, Senegal and Burkina Faso. Thus, an intercomparison between the satellite observations and the in situ measurements shows a good correlation between MODIS and AERONET with a correlation coefficient R = 0.86 at Cinzana, R = 0.85 at Banizounbou, R = 0.84 at Ouagadougou and a low correlation coefficient R = 0.66 calculated on the Dakar site. Like MODIS, SeaWiFS shows a very good correspondence with measurements of the ground photometer especially for Banizoumbou (R = 0.89), Cinzana (R = 0.88) and Dakar (R = 0.75) followed by a low correlation coefficient calculated on the Ouagadougou site (R = 0.64). The performance of these airborne sensors is also corroborated by the calculation of root mean square error (RMSE) and the mean absolute error (MAE). Following this validation, a climatological analysis based on aerosol optical depth (AOD) shows the seasonality of aerosols in West Africa strongly influenced by the climate dynamics illustrated by the MERRA model reanalysis. This seasonal spatial distribution of aerosols justifies the temporal variability of the particles observed at the different sites in the Sahel. In addition, a combined analysis of AOD and Angstrom coefficient indicates the aerosol period in the Sahel in spring (March-April-May) and summer (June-July-August). However, these aerosols are strongly dominated by desert dust whose main sources are located north in the Sahara and Sahel.
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