首页> 外文期刊>Quarterly Journal of the Royal Meteorological Society >Spatial and vertical heterogeneities in aerosol properties over oceanic regions around India: Implications for radiative forcing
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Spatial and vertical heterogeneities in aerosol properties over oceanic regions around India: Implications for radiative forcing

机译:印度周围海洋区域气溶胶特性的空间和垂直异质性:对辐射强迫的影响

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The influence of atmospheric aerosols on Earth's radiation budget and hence climate, though well recognized and extensively investigated in recent years, remains largely uncertain mainly because of the large spatio-temporal heterogeneity and the lackof data with adequate resolution. To characterize this diversity, a major multi-platform field campaign ICARB (Integrated Campaign for Aerosols, gases and Radiation Budget) was carried out during the pre-monsoon period of 2006 over the Indian landmass and surrounding oceans, which was the biggest such campaign ever conducted over this region. Based on the extensive and concurrent measurements of the optical and physical properties of atmospheric aerosols during ICARB, the spatial distribution of aerosolradiative forcing was estimated over the entire Bay of Bengal (BoB), northern Indian Ocean and Arabian Sea (AS) as well as large spatial variations within these regions. Besides being considerably lower than the mean values reported earlier for this region, our studies have revealed large differences in the forcing components between the BoB and the AS. While the regionally averaged aerosol-induced atmospheric forcing efficiency was 31 +- 6 W m~(-2) tau~(-1) for the BoB, it was only approx 18 +- 7 W m~(-2) tau~(-1) for the AS. Airborne measurements revealed the presence of strong, elevated aerosol layers even over the oceans, leading to vertical structures in the atmospheric forcing, resulting in significant warming in the lower troposphere. These observations suggest serious climate implications and raise issues ranging from the impact of aerosols on vertical thermal structure of the atmospheric and hence cloud formation processes to monsoon circulation.
机译:大气气溶胶对地球辐射预算以及因此对气候的影响,尽管近年来得到了广泛认可和广泛研究,但很大程度上仍不确定,这主要是由于时空异质性大以及缺乏足够分辨率的数据所致。为了体现这种多样性,2006年季风前期在印度陆地和周围海洋地区进行了一次大型的多平台野外运动ICARB(气溶胶,气体和辐射预算综合运动),这是有史以来规模最大的运动在该地区进行。根据对ICARB期间大气气溶胶光学和物理特性的广泛且同时的测量,估计了整个孟加拉湾(BoB),印度洋北部和阿拉伯海(AS)以及大面积的气溶胶辐射强迫的空间分布这些区域内的空间变化。除了明显低于该地区早些时候报道的平均值外,我们的研究还显示出BoB和AS之间的强迫成分存在很大差异。虽然BoB的区域平均气溶胶诱发的大气强迫效率为31 +-6 W m〜(-2)tau〜(-1),但仅为18 +-7 W m〜(-2)tau〜( -1)。机载测量表明,甚至在整个海洋上,都存在强烈的升高的气溶胶层,从而导致大气强迫中的垂直结构,从而导致对流层下层明显升温。这些观测结果暗示了严重的气候影响,并提出了各种问题,从气溶胶对大气垂直热结构的影响到云形成过程再到季风环流。

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