Book — 1 online resource (xvi, 263 pages) : illustrations (some color) Digital: text file.
The purpose of the conference is to bring together leading researchers from the adaptive hardware and systems community to exchange experiences and share new ideas in the field While the focus of this conference is on communications and space applications, we welcome original contributions in other application areas such as consumer, medical, defense and security, as the techniques employed in these areas can be disseminated across the board.
This guide contains more than a dozen home or classroom activities for youngsters of all ages, including step-by-step instructions, materials lists, and background information on eclipses and our solar system.
Washington, D.C. : United States. Dept. of Energy. Office of Science ; Oak Ridge, Tenn. : distributed by the Office of Scientific and Technical Information, U.S. Dept. of Energy, 2016
Book — p. 5853-5866 : digital, PDF file.
<p>The Specified Dynamics version of the Whole Atmosphere Community Climate Model (SD-WACCM) and the Goddard Space Flight Center two-dimensional (GSFC 2-D) models are used to investigate the effect of galactic cosmic rays (GCRs) on the atmosphere over the 1960–2010 time period. The Nowcast of Atmospheric Ionizing Radiation for Aviation Safety (NAIRAS) computation of the GCR-caused ionization rates are used in these simulations. GCR-caused maximum NO<sub><i>x</i></sub> increases of 4–15 % are computed in the Southern polar troposphere with associated ozone increases of 1–2 %. NO<sub><i>x</i></sub> increases of ~1–6 % are calculated for the lower stratosphere with associated ozone decreases of 0.2–1 %. The primary impact of GCRs on ozone was due to their production of NO<sub><i>x</i></sub>. The impact of GCRs varies with the atmospheric chlorine loading, sulfate aerosol loading, and solar cycle variation. Because of the interference between the NO<sub><i>x</i></sub> and ClO<sub><i>x</i></sub> ozone loss cycles (e.g., the ClO + NO<sub>2</sub>+ M → ClONO<sub>2</sub>+ M reaction) and the change in the importance of ClO<sub><i>x</i></sub> in the ozone budget, GCRs cause larger atmospheric impacts with less chlorine loading. GCRs also cause larger atmospheric impacts with less sulfate aerosol loading and for years closer to solar minimum. GCR-caused decreases of annual average global total ozone (AAGTO) were computed to be 0.2 % or less with GCR-caused column ozone increases between 1000 and 100 hPa of 0.08 % or less and GCR-caused column ozone decreases between 100 and 1 hPa of 0.23 % or less. Although these computed ozone impacts are small, GCRs provide a natural influence on ozone and need to be quantified over long time periods. This result serves as a lower limit because of the use of the ionization model NAIRAS/HZETRN which underestimates the ion production by neglecting electromagnetic and muon branches of the cosmic ray induced cascade. Furthermore, this will be corrected in future works.</p>