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On the steady‐state assumption for the energy distribution function of the nonthermal N( 4 S) atoms and the efficiency of NO production by these atoms in the terrestrial thermosphere
Author(s) -
Dothe H.,
Sharma R. D.,
Duff J. W.
Publication year - 1997
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/97gl03258
Subject(s) - thermosphere , boltzmann equation , physics , steady state (chemistry) , distribution function , atomic physics , boltzmann constant , maxwell–boltzmann distribution , mesosphere , ionosphere , distribution (mathematics) , function (biology) , production (economics) , thermodynamics , atmospheric sciences , quantum mechanics , plasma , chemistry , mathematics , stratosphere , mathematical analysis , macroeconomics , astronomy , evolutionary biology , biology , economics
The time dependent energy distribution functions (EDF) of N( 4 S) atoms for altitudes greater than 100 km at 1400 hr local time are calculated by solving the time dependent Boltzmann equation. At time t=0 the time dependent sources and sinks are switched on into a Maxwell‐Boltzmann distribution of N( 4 S) atoms and the time dependence of the EDF is followed by solving the Boltzmann equation. It is found that the non‐Maxwellian tail of the EDF reaches a steady‐state in 0.01 s giving the fraction of nascent N( 4 S) atoms that react with O 2 before the establishment of steady‐state to be less than 1%. The number of NO molecules produced per second, after the establishment of steady‐state, by the non‐Maxwellian tail of the EDF is at most about 3% of the number of N( 4 S) atoms in the sources. The last fraction, often referred to as “NO reaction efficiency”, is about an order of magnitude smaller than that given in recent literature. An important consequence of this study is that the models still calculate less NO in the mesosphere and lower thermosphere than is measured.