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Total solar irradiance since 1996: is there a long-term variation unrelated to solar surface magnetic phenomena?

机译:自1996年以来的总太阳辐照度:是否存在与太阳表面磁现象无关的长期变化?

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Context. Total solar irradiance (TSI) has been measured with space-based instruments since 1978. The TSI during the recent solar minimum in 2009 has been lower than the two former minima around the years 1986 and 1996, which points to a long-term decrease. Aims. In this study, we address the question of whether the observed decrease in the TSI is the result of evolving solar surface magnetism (sunspots and faculae). Methods. We use a TSI model that is solely based on solar surface magnetic phenomena (sunspots and faculae including network). The information needed for this model is derived from Carrington rotation magnetogram and photogram synoptic charts measured with the Michelson Doppler Imager (MDI) instrument on-board the Solar and Heliospheric Observatory (SOHO). By combining these data with solar atmosphere calculations, TSI is reconstructed. Results. The TSI is reconstructed from June 1996 to May 2010. From the solar minimum of 1996 to the solar maximum of 2004 the model reproduces the observations well, but it fails to explain the observed decrease in TSI in the solar minimum of 2009 and the very recent data of 2010. Conclusions. The difference between modeled and observed TSI might be the result of underrepresented weak magnetic fields in the Carrington rotation synoptic charts, an uncertainty in the TSI measurement, or a decline of the global temperature of the photosphere. If latter were true, this would have important implications for reconstructions of TSI in the past. In order to study if an underrepresentation of weak magnetic fields in the Carrington rotation synoptic charts is the explanation for the difference between our model and the observation, full-disk images with higher spatial and temporal resolution should be analyzed in future.
机译:上下文。自1978年以来,就已经使用太空仪器对太阳总辐照度(TSI)进行了测量。2009年最近的最低太阳辐照度(TSI)低于1986年和1996年的前两个最低值,这表明长期下降。目的在这项研究中,我们解决了这样一个问题,即所观察到的TSI下降是否是太阳表面磁性(太阳黑子和晶状体)发展的结果。方法。我们使用的TSI模型仅基于太阳表面的磁现象(包括网络的太阳黑子和微透镜)。该模型所需的信息来自卡林顿旋转磁磁图和用太阳和日球天文台(SOHO)上的迈克尔逊多普勒成像仪(MDI)仪器测量的摄影简图。通过将这些数据与太阳大气计算相结合,可以重建TSI。结果。从1996年6月至2010年5月对TSI进行了重建。从1996年的最低日照到2004年的最高日照,该模型很好地再现了观测结果,但无法解释在2009年和最近的最低日照中观测到的TSI的下降。 2010年的数据。结论。建模和观测到的TSI之间的差异可能是由于Carrington旋转天气图中弱磁场的表示不足,TSI测量的不确定性或光球整体温度下降的结果。如果后者是正确的话,这将对过去的TSI重建产生重要影响。为了研究卡林顿旋转天气图中弱磁场的不足表示是否可以解释我们的模型与观测值之间的差异,将来应分析具有更高时空分辨率的全盘图像。

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