Do Seismographs Reflect the Number and Size of Rock Cracks at Tectonic Plate Boundaries?
Modeling & PredictionIntroduction Tectonic plates are constantly moving and shifting, often causing earthquakes and other geological events. These movements are caused by the interaction of the plates at their boundaries, where they can either move apart, slide past each other, or collide. When the plates collide or slide past each other, the rocks at the boundary can
Modeling Extraterrestrial Radiation for High Latitudes: Estimation Techniques for 66.5° N/S
Energy & ResourcesIntroduction Estimation of extraterrestrial radiation (ETR) is an important aspect of Earth science that has received considerable attention in recent years. ETR is the amount of solar radiation that reaches the Earth’s surface from the Sun and is a critical factor in many areas, including agriculture, climate change, and solar energy. While ETR can be
The Impact of Vegetation on Suspended Sediment Yield in Earth Science
Wildlife & BiologyIntroduction Suspended sediment yield is the amount of sediment carried by water in a suspended state over a given period of time. It is an important parameter in geoscience because it provides insight into the erosion and sediment transport processes in a river system. Suspended sediment yield is influenced by a number of factors, including
Unlocking the Power of Single-Antenna-Single-Pass SAR Interferometry for High-Resolution Earth Science Radar Imaging
Safety & HazardsIntroduction Synthetic Aperture Radar (SAR) has revolutionised remote sensing applications by providing high resolution images of the Earth’s surface in all weather conditions. SAR interferometry (InSAR) is a technique that uses two SAR images of the same area to measure surface deformation. However, traditional InSAR algorithms require two antennas or passes to obtain the necessary
Unraveling the Mystery of Minuscule Grid Cell Weights in Earth Science
Modeling & PredictionIntroduction In earth science, grid cells are often used to represent a particular area of the earth’s surface. The size of the grid cell can vary depending on the application, but it is usually chosen to be small enough to capture the required level of detail. However, when using a method for weighting grid cells,