FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2612028467> ?p ?o ?g. }

• W2612028467 endingPage "6848" @default.
• W2612028467 startingPage "6812" @default.
• W2612028467 abstract "Abstract With a thermosphere‐ionosphere Fe/Fe + (TIFe) model developed from first principles at the University of Colorado, we present the first quantitative investigation of formation mechanisms of thermospheric Fe layers observed by lidar in Antarctica. These recently discovered neutral metal layers in the thermosphere between 100 and 200 km provide unique tracers for studies of fundamental processes in the space‐atmosphere interaction region. The TIFe model formulates and expands the TIFe theory originally proposed by Chu et al . that the thermospheric Fe layers are produced through the neutralization of converged Fe + layers. Through testing mechanisms and reproducing the 28 May 2011 event at McMurdo, we conceive the lifecycle of meteoric metals via deposition, transport, chemistry, and wave dynamics for thermospheric Fe layers with gravity wave signatures. While the meteor injection of iron species is negligible above 120 km, the polar electric field transports metallic ions Fe + upward from their main deposition region into the E ‐ F regions, providing the major source of Fe + (and accordingly Fe) in the thermosphere. Atmospheric wave‐induced vertical shears of vertical and horizontal winds converge Fe + to form dense Fe + layers. Direct electron‐Fe + recombination is the major channel to neutralize Fe + layers to form Fe above ~120 km. Fe layer shapes are determined by multiple factors of neutral winds, electric field, and aurora activity. Gravity‐wave‐induced vertical wind plays a key role in forming gravity‐wave‐shaped Fe layers. Aurora particle precipitation enhances Fe + neutralization by increasing electron density while accelerating Fe loss via charge transfer with enhanced NO + and O 2 + densities." @default.
• W2612028467 created "2017-05-19" @default.
• W2612028467 creator A5034398688 @default.
• W2612028467 creator A5076199902 @default.
• W2612028467 date "2017-06-01" @default.
• W2612028467 modified "2023-10-14" @default.
• W2612028467 title "Formation mechanisms of neutral Fe layers in the thermosphere at Antarctica studied with a thermosphere‐ionosphere Fe/Fe ⁺ (TIFe) model" @default.
• W2612028467 cites W1552476003 @default.
• W2612028467 cites W1554226731 @default.
• W2612028467 cites W1567272999 @default.
• W2612028467 cites W1604963949 @default.
• W2612028467 cites W1649510183 @default.
• W2612028467 cites W1672263216 @default.
• W2612028467 cites W1893470019 @default.
• W2612028467 cites W1921207839 @default.
• W2612028467 cites W1952959233 @default.
• W2612028467 cites W1966872696 @default.
• W2612028467 cites W1967896802 @default.
• W2612028467 cites W1969740830 @default.
• W2612028467 cites W1969956869 @default.
• W2612028467 cites W1970036327 @default.
• W2612028467 cites W1970269381 @default.
• W2612028467 cites W1974937226 @default.
• W2612028467 cites W1977780176 @default.
• W2612028467 cites W1981175511 @default.
• W2612028467 cites W1984928786 @default.
• W2612028467 cites W1991569834 @default.
• W2612028467 cites W1991886865 @default.
• W2612028467 cites W1992439707 @default.
• W2612028467 cites W1992763656 @default.
• W2612028467 cites W1996183262 @default.
• W2612028467 cites W1996753865 @default.
• W2612028467 cites W1996979150 @default.
• W2612028467 cites W1999014879 @default.
• W2612028467 cites W2000492550 @default.
• W2612028467 cites W2003699352 @default.
• W2612028467 cites W2004080731 @default.
• W2612028467 cites W2005736302 @default.
• W2612028467 cites W2007077282 @default.
• W2612028467 cites W2008465391 @default.
• W2612028467 cites W2010143950 @default.
• W2612028467 cites W2011466807 @default.
• W2612028467 cites W2014369658 @default.
• W2612028467 cites W2014507033 @default.
• W2612028467 cites W2017336802 @default.
• W2612028467 cites W2017345306 @default.
• W2612028467 cites W2020105551 @default.
• W2612028467 cites W2038183734 @default.
• W2612028467 cites W2038663227 @default.
• W2612028467 cites W2041482446 @default.
• W2612028467 cites W2044495826 @default.
• W2612028467 cites W2044987752 @default.
• W2612028467 cites W2045471756 @default.
• W2612028467 cites W2049161806 @default.
• W2612028467 cites W2051493915 @default.
• W2612028467 cites W2052004428 @default.
• W2612028467 cites W2052294817 @default.
• W2612028467 cites W2053810378 @default.
• W2612028467 cites W2054239947 @default.
• W2612028467 cites W2055814912 @default.
• W2612028467 cites W2057622447 @default.
• W2612028467 cites W2058425300 @default.
• W2612028467 cites W2062861935 @default.
• W2612028467 cites W2068133483 @default.
• W2612028467 cites W2071403173 @default.
• W2612028467 cites W2071475654 @default.
• W2612028467 cites W2072529579 @default.
• W2612028467 cites W2072884787 @default.
• W2612028467 cites W2073619393 @default.
• W2612028467 cites W2079328353 @default.
• W2612028467 cites W2079455703 @default.
• W2612028467 cites W2083641117 @default.
• W2612028467 cites W2086266800 @default.
• W2612028467 cites W2087326422 @default.
• W2612028467 cites W2091250644 @default.
• W2612028467 cites W2093021986 @default.
• W2612028467 cites W2094807461 @default.
• W2612028467 cites W2098184824 @default.
• W2612028467 cites W2103579203 @default.
• W2612028467 cites W2106711433 @default.
• W2612028467 cites W2108963537 @default.
• W2612028467 cites W2116334968 @default.
• W2612028467 cites W2124715982 @default.
• W2612028467 cites W2124942875 @default.
• W2612028467 cites W2131067066 @default.
• W2612028467 cites W2137797038 @default.
• W2612028467 cites W2142136705 @default.
• W2612028467 cites W2150420559 @default.
• W2612028467 cites W2158993832 @default.
• W2612028467 cites W2171650321 @default.
• W2612028467 cites W2303772024 @default.
• W2612028467 cites W2309100812 @default.
• W2612028467 cites W2316404615 @default.
• W2612028467 cites W2410013512 @default.
• W2612028467 cites W2491488721 @default.
• W2612028467 cites W2508330354 @default.
• W2612028467 cites W2749486094 @default.
• W2612028467 cites W2985646705 @default.

• next