Thats a unique idea.You should consider the following idea to enhance your idea so that it would impact uniquely: For a water content over 8%, the transmitted component of a SAR beam becomes negligible. The electromagnetic wave interaction with the interface discontinuity is then determined by the scattering efficiency of surface roughness rms and correlation height. It is illustrated by the difference of contrast observed on images acquired from a same scene one late in the afternoon after a warm day and the development of a t interface, and the other, early in the morning after a cool night and growth of frost flor in place of the t interface. The increased the rms height of newly formed crystals reduce the angle dependence of the backscattered signal and therefore the contrast on the scene, hover, the increased volume scattering in snow covered areas seems to be the main factor causing a resolution difference on the ridge network beten images recorded on morning and at the end of the afternoon. A detailed survey of the air-snow or air-ice interface of the snow cover and ice blocks surfaces. Surface tness, snow tness content and surface roughness are documented. Radar data measured on a variety of snow and ice interfaces are presented and analyzed.  show that the presence of a t film on snow and ice surfaces produces an increased forward scattering whereas interfaces covered with newly crystallized ice display an enhanced backscattering.
['Eric Hudier', 'J. Gosselin', 'Deborah Febres']
I am writing a research paper on a idea Diurnal SAR variability due to ice and snow air interface wetness overnight changes.
[{"from": "human", "value": "I am writing a research paper on a idea Diurnal SAR variability due to ice and snow air interface wetness overnight changes."}, {"from": "gpt", "value": "Thats a unique idea.You should consider the following idea to enhance your idea so that it would impact uniquely: For a water content over 8%, the transmitted component of a SAR beam becomes negligible. The electromagnetic wave interaction with the interface discontinuity is then determined by the scattering efficiency of surface roughness rms and correlation height. It is illustrated by the difference of contrast observed on images acquired from a same scene one late in the afternoon after a warm day and the development of a t interface, and the other, early in the morning after a cool night and growth of frost flor in place of the t interface. The increased the rms height of newly formed crystals reduce the angle dependence of the backscattered signal and therefore the contrast on the scene, hover, the increased volume scattering in snow covered areas seems to be the main factor causing a resolution difference on the ridge network beten images recorded on morning and at the end of the afternoon. A detailed survey of the air-snow or air-ice interface of the snow cover and ice blocks surfaces. Surface tness, snow tness content and surface roughness are documented. Radar data measured on a variety of snow and ice interfaces are presented and analyzed.  show that the presence of a t film on snow and ice surfaces produces an increased forward scattering whereas interfaces covered with newly crystallized ice display an enhanced backscattering."}]