You know the importance and significance of the Green's function. However, what Green's functions have you ever heard about or used? There are actually only a very small set of geometries where closed form expressions of the Green's function are available, namely, the free-space Green's function, the layered medium Green's function, the Green's function of a rectangular or circular waveguide / cavity, or maybe, even the Green's function of a sphere or a cylinder expressed in special Bessel functions; Green's function is also known for an empty periodic lattice, typically called the lattice Green's function.
But!!! Here we're looking at Green's functions of all geometries. -------- Green's function in terms of modes, and relatively few number of modes. As modes themselves are independent of frequencies, such representations can be readily calculated in a wide range of frequencies, earning it the name, the Broadband Green's Function.
Check this paper for this concept and its demonstration in a photonic crystal.
Just see how funny the Green's function looks like in the crystal at different frequencies.
The construction of the Broadband Green's Function requires efficient characterization of the band structure for periodic structures, such as metamaterials and photonic crystals.
Here is how we calculate it: a quite interesting idea that makes use of the broadband representation of the lattice Green's function to convert a non-linear root searching problem into a linear eigenvalue problem of small size.
The broadband Green's function empowers us to do a lot. It is a combination of analytical modeling and numerical computations. It offers us new insights into the physical scattering process.
Check this first demonstration of the application of the Broadband Green's Function in calculating the scattering from a half-sapce of photonic crystals.
Snow quenches our thirst, and snow cools our planet. ------ iSWGR
Snow is a dense volumetric random media. At microwave frequencies, the ice grains interact actively with electromagnetic waves, creating unique microwave signatures that can be utilized to observe the global snow coverage / amount remotely, preferably on-board a satellite.
We're especially interested in modeling the physical scattering and emission process of electromagnetic waves inside the snowpack. We use both analytical approaches and numerical approaches. The numerical approach solves Maxwell's equation directly on the Monte Carlo realizations of the random media. It predicts the most fundamental physical solution of wave interactions without any approximation. It usually involves high-performance parallel computing (HPC) techniques to attack problems of unprecedented scales. We're also thrilled in developing operational algorithms for snow retrieval using radar and radiometer measurements.
Check out these papers for improved understanding of the topic.
UWBRAD, the Ultra-Wideband Software Defined Radiometer, is a radiometer operating at 0.5~2.0 GHz, designed to derive the polar ice sheet internal / intraglacial temperature profiles using wideband low frequency radiometry.
Check these several papers on the scientific concepts / campaigns, the technical implementations, and the electromagnetic scattering and emission processes, behind this endeavor to improve our knowledge of the polar ice sheet, and our mother planet.
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