论文标题
维多利斯在金星快递上获得的金星夜间夜间平均红外热排放的全球地图
Global maps of Venus nightside mean infrared thermal emissions obtained by VIRTIS on Venus Express
论文作者
论文摘要
关于金星气氛的惊人特征之一是其时间变异性和动力学,具有混乱的极性涡流,大规模的大气波,剪切特征和可变风,依赖于当地时间和可能的地形特征。这项研究的目的是结合数年来积累的数据,并使用云不透明度和上层云温度获得重点放在云的全球大气结构的全球平均状态。我们首先使用集成的辐射度通过以1.74μm和2.25μm为中心的红外大气窗来生成全局图,这表明下部云中云不透明度的空间变化在44-48 km的高度左右,还提供了可能粒径的间接估计。我们还使用在3.8μm和5.0μm的热区域中看到的亮度温度产生了相似的全局图,这些温度在60-70 km海拔约60-70 km的云层顶部直接指示。这些图是使用Venus Express上的可见和红外热成像光谱仪映射通道(Virtis-M)的完整数据集生成的,从2006年5月到2008年10月,在2006年5月至2008年10月的时期内具有广泛的空间和长时间的覆盖范围。我们的结果提供了全球范围的视野,对云的不透明,粒度和上半范围的云云温度的全球视图,显示了两个不同的范围,显示了不同的平面环境。获得的轮廓还提供了详细的依赖性,局部时间和经度,诊断到各种高度层的全局循环流和动力学的诊断,从大约44至70 km的表面上。
One of the striking features about Venus atmosphere is its temporal variability and dynamics, with a chaotic polar vortex, large-scale atmospheric waves, sheared features, and variable winds that depend on local time and possibly orographic features. The aim of this research is to combine data accumulated over several years and obtain a global mean state of the atmosphere focusing in the global structure of the clouds using the cloud opacity and upper cloud temperatures. We have first produced global maps using the integrated radiance through the infrared atmospheric windows centred around 1.74μm and 2.25μm, that show the spatial variations of the cloud opacity in the lower clouds around 44-48 km altitude and also provide an indirect estimation of the possible particle size. We have also produced similar global maps using the brightness temperatures seen in the thermal region at 3.8μm and 5.0μm, which provide direct indication of the temperatures at the top of the clouds around 60-70 km altitude. These maps have been generated using the complete dataset of the Visible and InfraRed Thermal Imaging Spectrometer mapping channel (VIRTIS-M) on board Venus Express, with a wide spatial and long temporal coverage in the period from May 2006 until October 2008. Our results provide a global view of the cloud opacity, particle size and upper cloud temperatures at both hemispheres, showing the main different dynamical regions of the planet. The profiles obtained also provide the detailed dependencies with latitude, local time and longitude, diagnostic of the global circulation flow and dynamics at various altitude layers, from about 44 up to 70 km over the surface.