Results 61 to 70 of about 33,721 (170)
Chorus Wave–Driven Electron Dynamics in the Van Allen Belts: From Coherence to Diffusion
Abstract The Van Allen radiation belts contain relativistic electrons trapped by Earth's magnetic field, posing serious risks to spacecraft. Chorus waves are known to accelerate these electrons via resonant interactions, but these interactions are inherently nonlinear and coherent.
Xin Tao +4 more
wiley +1 more source
Numerical simulations of multi-scale astrophysical problems: The example of Type Ia supernovae
Vastly different time and length scales are a common problem in numerical simulations of astrophysical phenomena. Here, we present an approach to numerical modeling of such objects on the example of Type Ia supernova simulations.
Roepke, F. K.
core +1 more source
Abstract NASA scientists and engineers, in collaboration with university researchers, have developed low‐cost lightweight remote sensing instruments that anyone can build and use to bring remote sensing science to communities beyond traditional professional scientists. Built from commercially available components, these Science and Technology Education
Paul Mirel +6 more
wiley +1 more source
Efficient Sampling of Geophysical Sensor Arrays on the Seafloor
Abstract The great expense of deploying dense arrays of seafloor sensors for continuous collection of geophysical data inhibits the proliferation of measurement systems to the majority of the planet's surface. Advancing geophysical coverage offshore will require technologies different from conventional methods applied onshore where electrical power and
M. A. Zumberge, D. Horwitt
wiley +1 more source
Abstract X‐band Phased array radars are characterized by high spatial and temporal resolution, but suffer from a range of data quality problems, such as echo voids after the filtering of ground clutter, abnormal radials, radial obstructions and irregular missing radar echoes. This paper proposes a radar echo image restoration model (GCD) based on color
Jinyan Xu +6 more
wiley +1 more source
Analysis of South Atlantic Anomaly Influence on Low‐Earth Orbit Lightning Observations
Abstract The low‐Earth orbit Optical Transient Detector (OTD) and Lightning Imaging Sensor (LIS) instruments, spanning 1995–2023, have spatiotemporal patterns within their metadata that are consistent with the South Atlantic Anomaly (SAA). While the SAA had a known influence on these instruments, this study details new variability and impacts.
A. G. Clark +5 more
wiley +1 more source
Abstract Earth's radiation belts are the regions where highly energetic charged particles are trapped by Earth's magnetic field, posing significant risks to the satellites and other space‐based technologies. Understanding the dynamics of the radiation belts is critical not only for advancing fundamental plasma physics but also for predicting and ...
Hong Zhao +3 more
wiley +1 more source
Methods for Cleaning Apollo Passive Seismic Data
Abstract Apollo passive seismic data provide a unique resource for studying the lunar interior structure. However, the raw data are frequently contaminated by various artifacts, either related to the seismic sensors and the acquisition system or to issues during data transmission to the Earth.
Xiang Zhang +8 more
wiley +1 more source
Abstract Fe‐oxidizing microorganisms in deep‐sea hydrothermal vent environments are often used as analogs for primordial life on Earth. In fact, Earth's oldest purported microfossils are preserved as hematite filaments in a jasper rock dated between 4,160 and 4,280 million years and are thought to have originated in a seafloor hydrothermal environment.
Dominic Papineau +8 more
wiley +1 more source
Abstract Due to the properties of sound propagation underwater, including the existence of the SOFAR channel, sounds in the ocean can propagate over large distances with little attenuation. This makes passive acoustics a relevant method for monitoring natural events such as ice calving, earthquakes, and underwater volcanic eruptions.
Pierre‐Yves Raumer +4 more
wiley +1 more source

