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The scaling factors are derived from the ozonesonde profiles up to the balloon burst height (at least 26 km) and MLS monthly mean climatology above the burst height (red circles).
Each ozonesonde profile with the new correction factor applied was complemented by the O3 climatology profile above the balloon burst height.
The O3 concentrations above the balloon burst height were provided by linearly interpolating in time the daytime climatology profiles arranged at the middle of each month.
This equation is a reduced form of the general burst equation: where kcat = (k2 k3)/(k2 + k3), the burst height = k2/ k2 + k3), and the rate of burst formation = k2 + k3, which results from making the assumption that k2 ≫ k3.
The S/N ratios, which were calculated as the average burst height of 3551 nanoparticles detected in 1 min divided by the standard deviation of the background signal (noise), were found to be 486 and 561 for SS and FL detection, respectively.
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OR.1177 specified 50, 100, 200 and 300-kt yields, assuming a circular error probable of 1200 feet and a damage probability of 0.8, and laydown delivery capability, with burst heights for targets from 0 to 10000 feet above sea level.
These bursts indicate the height of shock formation in the corona as evidenced by EUV shocks and Moreton waves (see e.g., Asai et al. 2012a, 2012b).
The circatidal clock would suppress this general activity, leading to activity bursts (of different height) every 12.4 hours.
We then use large-scale three-dimensional simulations to construct numerically generated Height of Burst maps that are appropriate at the higher energy levels associated with the entry of asteroids with diameters of hundreds of meters.
In particular, these tools rely upon the powerful yield scaling laws developed for point-source blasts that are used in conjunction with a Height of Burst (HOB) map to predict ground damage for an airburst of a specific energy at a given altitude.
To minimize internal fragmentation, BCO expands the burst by one slot height in steps.
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