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A Model for the Total Solar Irradiance Based on Active Region Decay

机译:基于有源区衰减的总太阳辐照度模型

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We present a model for the total solar irradiance. The model takes the observed location, timing, and area of emerging active regions as input and produces a time-evolving size distribution of magnetic structures over the solar surface. We assume that the bright magnetic structures (faculae), which counteract the irradiance deficit caused by sunspots, consist of the products of active region decay. We simulate the decay process as a combination of fragmentation and boundary erosion of large-scale magnetic structures. The model has several adjustable parameters that control the decay processes and the irradiance contribution from the quiet Sun and the small-scale magnetic elements that are produced during the decay process. We use a genetic algorithm to estimate these parameters by fitting to the observed irradiance and daily sunspot area time series over the 1978-2007 time interval. Given the simplifications associated with the model, the resultant parameter values are well constrained within the imposed ranges. In addition, the irradiance and daily sunspot area time series produced by the best-fit models agree very well with the observations, although the sunspot area fits tend to perform better than the irradiance fits. However, it is evident that the model is neglecting a significant source of excess brightness, which manifests itself in two ways. First, the optimal values for the lifetime and intensity contrast of the bright, small-scale flux elements are both larger than expected. Second, the synthetic irradiance consistently underestimates the observations during the ascending phase of a cycle, despite the daily sunspot area fitting the observations quite well during these times. We also show that this genetic forward modeling approach can be used to detect a long-term trend of decadal timescale in the quiet-Sun irradiance. Assuming a constant quiet-Sun irradiance, we reconstruct the total solar irradiance over the 1874-1978 time interval, for which observational data of emerging active regions are available.
机译:我们提出了总太阳辐照度的模型。该模型将观测到的活动区域的位置,时间和面积作为输入,并在太阳能表面上产生磁性结构随时间变化的尺寸分布。我们假设抵消了由黑子引起的辐照度不足的明亮的磁性结构(晶簇)由活动区域衰减的产物组成。我们将衰变过程模拟为大型磁性结构的碎片化和边界腐蚀的组合。该模型具有几个可调整的参数,用于控制衰变过程以及安静的太阳和衰变过程中产生的小规模磁性元素的辐照度贡献。我们使用一种遗传算法通过拟合1978-2007年时间间隔内观察到的辐照度和太阳黑子区域的时间序列来估计这些参数。给定与模型相关的简化,结果参数值被很好地限制在施加的范围内。此外,尽管太阳黑子面积拟合的性能往往好于辐照度拟合,但最佳拟合模型产生的辐照度和每日黑子面积时间序列与观测值非常吻合。但是,很明显,该模型忽略了多余亮度的重要来源,这以两种方式体现出来。首先,明亮的小型助焊剂的寿命和强度对比度的最佳值均大于预期值。其次,尽管日照黑子面积在这些时间段与观测值非常吻合,但合成辐照度在一个周期的上升阶段始终低估了观测值。我们还表明,这种遗传正向建模方法可用于检测静太阳辐照下十年时间尺度的长期趋势。假设恒定的安静太阳辐照度,我们重建1874-1978年时间间隔内的总太阳辐照度,为此可获得新兴活动区域的观测数据。

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