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arXiv 1907.09683astro-ph.EP
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金星快车、Akatsuki、MESSENGER和哈勃Space Telescope观测到的金星365 nm日冕的长期变化

Long-term variations of Venus' 365-nm albedo observed by Venus Express, Akatsuki, MESSENGER, and Hubble Space Telescope

Yeon Joo Lee, Kandis-Lea Jessup, Santiago Perez-Hoyos, Dmitrij V. Titov, Sebastien Lebonnois, Javier Peralta, Takeshi Horinouchi, Takeshi Imamura, Sanjay Limaye… 展开作者

Yeon Joo Lee, Kandis-Lea Jessup, Santiago Perez-Hoyos, Dmitrij V. Titov, Sebastien Lebonnois, Javier Peralta, Takeshi Horinouchi, Takeshi Imamura, Sanjay Limaye, Emmanuel Marcq, Masahiro Takagi, Atsushi Yamazaki, Manabu Yamada, Shigeto Watanabe, Shin-ya Murakami, Kazunori Ogohara, William M. McClintock, Gregory Holsclaw, Anthony Roman

摘要:

金星云顶附近的一个未知吸收体产生了从紫外线(UV)到可见光的广泛吸收特征,峰值约为360 nm,因此在太阳能吸收中起着关键作用。我们提出了一个定量研究的变化的云在365 nm和金星的太阳能加热率的基础上分析金星快车和晓的紫外图像,哈勃太空望远镜和信使号的紫外光谱数据,在此分析中的校准校正因子的紫外图像的金星快车(VMC)更新相对于哈勃和信使号的紫外测量。我们的研究结果表明,从2006年到2017年,整个地球上365 nm的太阳辐射量变化了2倍,根据我们的辐射转移计算,低纬度太阳加热率发生了25-40%的变化。因此,云顶大气层在这段时间内应该经历了相当大的太阳加热变化。我们的全球环流模式计算表明,这种可变的太阳加热率可以解释2006年至2017年观测到的纬向风变化。长期紫外线辐射和太阳活动变化的时间尺度重叠,这使得太阳极端紫外线强度和宇宙射线变化影响观测到的紫外线辐射趋势似乎是合理的。大气环流的变化也可能与高空SO2气体丰度的时间变化有关,后者影响H2SO 4-H2O气溶胶的形成。

英文摘要:

An unknown absorber near the cloud top level of Venus generates a broad absorption feature from the ultraviolet (UV) to visible, peaking around 360 nm, and therefore plays a critical role in the solar energy absorption. We present a quantitative study on the variability of the cloud albedo at 365 nm and its impact on Venus' solar heating rates based on an analysis of Venus Express and Akatsuki's UV images, and Hubble Space Telescope and MESSENGER's UV spectral data; in this analysis the calibration correction factor of the UV images of Venus Express (VMC) is updated relative to the Hubble and MESSENGER albedo measurements. Our results indicate that the 365-nm albedo varied by a factor of 2 from 2006 to 2017 over the entire planet, producing a 25-40% change in the low latitude solar heating rate according to our radiative transfer calculations. Thus, the cloud top level atmosphere should have experienced considerable solar heating variations over this period. Our global circulation model calculations show that this variable solar heating rate may explain the observed variations of zonal wind from 2006 to 2017. Overlaps in the timescale of the long-term UV albedo and the solar activity variations make it plausible that solar extreme UV intensity and cosmic-ray variations influenced the observed albedo trends. The albedo variations might also be linked with temporal variations of the upper cloud SO2 gas abundance, which affects the H2SO4-H2O aerosol formation.

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