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Some remarks about lidar data preprocessing and different implementations of the gradient method for determining the aerosol layers
Lidar Aerosol Wavelet Preprocessing
2015/8/17
The determination of atmospheric aerosol layers from lidar returns is possible through automated algorithms. This product is useful, for example, in monitoring the Boundary Layer Height (BLH) as well ...
Remarks on the parallel propagation of small-amplitude dispersive Alfvénic waves
parallel propagation small-amplitude dispersive Alfvénic waves
2009/11/13
The envelope formalism for the description of a small-amplitude parallel-propagating Alfvén wave train is tested against direct numerical simulations of the Hall-MHD equations in one space dimension w...
Remarks on nonlinear relation among phases and frequencies in modulational instabilities of parallel propagating Alfvén waves
nonlinear relation modulational instabilities parallel propagating Alfvén waves
2009/11/9
Nonlinear relations among frequencies and phases in modulational instability of circularly polarized Alfvén waves are discussed, within the context of one dimensional, dissipation-less, unforced fluid...
Remarks on the Magnitude Determination for Nurmijärvi, Kajaani and Kevo Seismograph Stations Based on the Rayleigh Waves
Remarks Magnitude Determination Nurmijä rvi Kajaani Kevo Seismograph Stations Rayleigh Waves
2009/6/15
Remarks on the Magnitude Determination for Nurmijärvi, Kajaani and Kevo Seismograph Stations Based on the Rayleigh Waves
Some Remarks on the Semi-Classical Limit of Quantum Gravity
the Semi-Classical Limit Quantum Gravity
2010/10/13
One of the most important issues in quantum gravity is to identify its semi-classical regime. First the issue is to define for we mean by a semi-classical theory of quantum gravity, then we would like...