Results 231 to 240 of about 4,448,337 (335)

Influence of the Earthward and Tailward Ion Flows on the Lunar Surface Water in the Magnetotail

open access: yesJournal of Geophysical Research: Planets, Volume 130, Issue 12, December 2025.
Abstract Earth wind, namely the particles from the Earth's magnetotail, is an important source of lunar water. Besides tailward flow incident on the lunar nearside when the Moon is in the magnetotail, there exists earthward flow bombarding the farside, affecting the distribution and preservation of lunar water.
H. Z. Wang   +21 more
wiley   +1 more source

Cosmic-Ray Bursts under Thick Shields [PDF]

open access: bronze, 1949
Y. Fujimoto, S. Hayakawa, Y. Yamaguchi
openalex   +1 more source

The cosmic ray detector for the NICA collider [PDF]

open access: diamond, 2020
Martin Bielewicz   +30 more
openalex   +1 more source

Radar Polarimetry in Glaciology: Theory, Measurement Techniques, and Scientific Applications for Investigating the Anisotropy of Ice Masses

open access: yesReviews of Geophysics, Volume 63, Issue 4, December 2025.
Abstract Dielectric anisotropy in ice alters the propagation of polarized radio waves, so polarimetric radar sounding can be used to survey anisotropic properties of ice masses. Ice anisotropy is either intrinsic, associated with ice‐crystal orientation fabric (COF), or extrinsic, associated with material heterogeneity, such as bubbles, fractures, and ...
Benjamin H. Hills   +30 more
wiley   +1 more source

The Pierre Auger Cosmic Ray Observatory [PDF]

open access: yes, 2015
A. Aab   +499 more
semanticscholar   +1 more source

Oxychlorine Species on Mars: A Review

open access: yesReviews of Geophysics, Volume 63, Issue 4, December 2025.
Abstract Oxychlorine species (mainly perchlorate and chlorate) have been identified at multiple locations on the surface of Mars by both orbiter and in situ rovers. They have also been found in martian meteorites. Cl‐isotopes in meteoritic minerals suggest that an oxychlorine cycle has been operating on the martian surface for the last ∼4 billion years.
Kaushik Mitra
wiley   +1 more source

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