Global observations of nitric oxide in the thermosphere

By C. Barth, K. Mankoff, S. Bailey, S. Solomon. 2003

168 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Atmospheric Science

View Paper: https://www.semanticscholar.org/paper/b77bff5c6226e95169d74dcebdba15df426b0026

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Astronomy and Astrophysics

1. J. Oberheide
2. Liying Qian
3. Jeff Forbes
4. S. Solomon
5. Sean Bruinsma
6. D. Marsh
7. R. Garcia
8. J. Russell

In Atmospheric Science

1. R. Garcia
2. Liying Qian
3. S. Solomon
4. F. Sassi
5. D. Marsh
6. Douglas E. Kinnison
7. J. Oberheide
8. J. Russell

Citations in the corpus

• Tropospheric tides from 80 to 400 km: Propagation, interannual variability, and solar cycle effects (2009, methodology): “Lower thermospheric nitric oxide densities from the Student Nitric Oxide Explorer (SNOE) [Barth et al., 2003] show a pronounced ‘‘wave-4’’ signature at low latitudes that could be attributed to DE3 density variations [Oberheide and Forbes, 2008b].”
• Energetic Particle Influence on the Earth’s Atmosphere (2015, background): “Their penetration depth is rather small and the energy deposition occurs mainly in the lower thermosphere (above 90 km) and confines to the auroral ovals located over 60–75◦ geomagnetic latitude band (Baker 2000; Barth et al. 2003).”
• Influence of the Precipitating Energetic Particles on Atmospheric Chemistry and Climate (2012, background): “Their energy is mostly deposited in the lower thermosphere (above 90 km) inside the auroral ovals located over the 60 –75 geomagnetic latitude band (Baker et al. 2001; Barth et al. 2003).”
• Simulation of secular trends in the middle atmosphere, 1950–2003 (2007, methodology): “NO is specified using data from the Student Nitric Oxide Explorer (SNOE) satellite [Barth et al., 2003], which has been parameterized as a function of latitude, season, and phase of the solar cycle inMarsh et al.’s [2004] Nitric Oxide Empirical Model (NOEM).”
• Energetic particle precipitation effects on the Southern Hemisphere stratosphere in 1992–2005 (2007, methodology): “These include SH hemispheric auroral and medium energy electron (MEE) power data derived from NOAA POES satellites (http://www.sec.noaa.gov/pmap/PoesSem.html), and thermospheric NO measurements from the Student Nitric Oxide Explorer (SNOE) [Barth et al., 2003].”
• Solar extreme‐ultraviolet irradiance for general circulation models (2005, result): “This is again in better agreement with recent observations [e.g., Russell et al., 1993; Barth et al., 1999; Solomon et al., 1999; Barth et al., 2003; Marsh et al., 2004].”