| dc.description.abstract |
Different observations of the Sun provide a vast array of measures of solar activity, including
solar irradiance, which has been used in this thesis. The Sun’s irradiance, total
solar irradiance (TSI) and spectral solar irradiance (SSI), incident at the top of the Earth’s
atmosphere and normalized to one astronomical unit, have been measured with spaceborne
instruments continuously since 1978. The irradiance varies on several timescales,
ranging from minutes up to decades, and likely lasting even longer. This temporal variability
of SSI significantly alters the Earth’s atmospheric density distribution and temperature,
which drive variations in many upper atmospheric processes including satellite
drag, ground-space communications, and GPS precision. Long-term TSI variability is essential
in understanding past and future global climate changes. Direct measurements of
the solar irradiance are available over the last four decades and are too short to derive
conclusions about any possible long-term changes in solar irradiance and their possible
influence on climate. It is, therefore, necessary to use models of solar output to deduce
variations at earlier dates. One type of solar irradiance model is an empirical model, frequently
called a proxy model, that is derived using linear relationships between a proxy
of solar activity and direct observations of the solar irradiance.
The main driver of the irradiance variations on time-scales of days to decades, and
possibly longer, is believed to be associated with solar magnetic activity located in the
active photospheric regions of sunspots and faculae. Empirical models incorporating the
effects of magnetic features (both sunspots and faculae) are sufficient to account for most
of the observed changes in TSI. However, proxy based empirical model outputs and observed
TSI comparison do not support this conclusion; the model fails to explain the depletion
that was observed in TSI since 2005. Conventional regression approach does not
have the features that can address this kind of temporal variations. Therefore, a method
aligning the empirical model with the observation in an adaptable manner is needed. This
means that in order to accurately estimate the detailed characteristics of TSI, including TSI
variability before 1947, an adaptive and more robust model is essential. In this thesis, a
data-driven method of solar irradiance modeling from magnetic features is presented.
The thesis employs a neural network (NN) modeling approach to reconstruct both total
and spectral irradiance temporal dynamics using the solar proxy as the input drivers
for the variations. The physical basis of this model is that all variations in solar irradiance
are caused by changes in surface magnetic activity. To find the nonlinear mapping between
solar magnetic features and solar irradiance, feed-forward neural networks were
used due to their simplicity, flexibility, and ease of use. To determine the critical combination
of magnetic features, we explored the influence of magnetic features on the solar
irradiance variations by means of network-based empirical modeling. To train the neural
network, the photometric sunspot index (PSI) and the magnesium II core-to-wing ratio
(Mg II index) were used in the input space while the Physikalisch-Meteorologisches
Observatorium Davos (PMOD) composite used as a target of the network. In order to facilitate
the learning process, two training algorithms have been implemented: Levenberg-
Marquardt and Bayesian approach. Using these approaches, we separately developed
two TSI models. The performance of the network was estimated quantitatively by means
of cross-validation and learning curve analysis on the data from the PMOD composite.
The ability of the networks to model the TSI variations was also independently tested
by comparing its performance with TSI data obtained from semi-empirical and linear
regression models. The results indicate that the NN TSI model proposed has a good
performance in representing TSI variations compared to the linear regression model. To
deduce solar output variation prior to the satellite era, first, we estimated the Mg II index
variation from F10.7 cm solar flux back to 1947 using NN modeling approach. By
incorporating the PSI and the modeled Mg II index effects, we extend the TSI estimation
back to 1947. The extrapolated TSI result indicates that the amplitudes of Solar Cycles 19
and 21 are closely comparable to each other, and Solar Cycle 20 appears to be of lower
irradiance during its maximum. |
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