They are the superposition of a background field and the effects of
the upper atmospheric wave pattern.
Not exact matches
Instead, a new study suggests, the phenomena occur when four types of slow - moving, high - altitude
atmospheric waves merge over a small region and, in turn, temporarily drive a 10 - fold - or - stronger brightening of an ever - present glow in the
upper atmosphere (green layer in the image above).
The ambiance of
upper -
atmospheric diffusion is especially palpable in such installations from the 1990s as St. Elmo's Breath (1992), and in a recent series of wide and tall glass panels animated with dissolving
waves of color.
Long - term trends in the
upper atmosphere - ionosphere are a complex problem due to simultaneous presence of several drivers of trends, which behave in a different way: increasing
atmospheric concentration of greenhouse gases, mainly CO2, long - term changes of geomagnetic and solar activity, secular change of the Earth's main magnetic field, remarkable long - term changes of stratospheric ozone concentration, and very probably long - term changes of
atmospheric dynamics, particularly of
atmospheric wave activity (Lastovicka 2009; Qian et al. 2011; Lastovicka et al. 2012).
By using an idealized heating to force a comprehensive
atmospheric model, the large negative anomalous latent heating associated with the observed deficit in central tropical Pacific rainfall is shown to be mainly responsible for the global quasi-stationary
waves in the
upper troposphere.