What initial mass function results from successful streaming instability dominance?
A top-heavy initial mass function.
The streaming instability is proposed as a leading theoretical solution to allow dust to bypass the fragmentation and radial drift barriers by causing rapid, localized gravitational clumping of dust, leading directly to planetesimal formation. While it offers a faster path, the outcome of this process is specific. Simulations indicate that when the streaming instability successfully causes this rapid gravitational collapse, it produces a mass distribution that is skewed heavily toward the larger end of the scale. This is described as a 'top-heavy' initial mass function, meaning a large proportion of the available mass is concentrated into very large planetesimals, sometimes hundreds of kilometers in size, very early in the formation process.
