Table 2
Summary of the different possible theoretical scenarios described in Section 3 to visualise the relative signs of the parameters at play.
μ0 = δ0 − ζ0ξ |
|||||||
---|---|---|---|---|---|---|---|
ξ | μ0 | tacc,0 − M* | ζ0 | Rd − M* | δ0 | Md − M* (a) and ![]() |
⇒ |
< 0 | tacc,0 ↓ M* ↑ | Any | < 0 | (a) shallower than (b) | = | ||
0 | 0 | tacc,0 ↔ M* ↑ | Any | 0 | (a) as steep as (b) | = | |
> 0 | tacc,0 ↑ M* ↑ | Any | > 0 | (a) steeper than (b) | = | ||
≤ 0 | Rd ↓ ↔ M* ↑ | ≤ 0 | (a) shallower or as steep as (b) | = | |||
<0 | tacc,0 ↓ M* ↑ | > 0 | Rd ↑ M* ↑ | (−∞, ζ0ξ) | (a) shallower or steeper than (b)(a) | ≠ | |
≤ 0 | Rd ↓ ↔ M* ↑ | ≤ 0 | (a) shallower or as steep as (b) | ○ | |||
(0, 1) | 0 | tacc,0 ↔ M* ↑ | > 0 | Rd ↑ M* ↑ | ≥ 0 | (a) steeper or as steep as (b) | = |
> 0 | tacc,0 ↑ M* ↑ | ≤ 0 | Rd ↓ ↔ M* ↑ | (ζ0ξ, +∞) | (a) shallower or steeper than (b)(b) | ○ | |
> 0 | Rd ↑ M* ↑ | (ζ0ξ, +∞) | (a) steeper than (b) | = |
δevo = ξ(ζ0 − μ0), ξ ≠ 0 | |||||||
---|---|---|---|---|---|---|---|
δevo | Md − M* (a) and ![]() |
||||||
< 0 | (a) shallower than (b) | ||||||
0 | (a) as steep as (b) | ||||||
> 0 | (a) steeper than (b) |
Notes. From left to right in the top table, the columns show (i) ξ, a proxy for the evolutionary model (viscous if ξ = 0, hybrid or wind-driven otherwise); (ii) μ0, the slope of the tacc,0 − M* correlation and its implication on the correlation itself; (iii) ζ0, the slope of the Rd − M* correlation, and its implication on the correlation itself; (iv) δ0 = λm,0 − λacc,0, the difference between the initial slopes of the Md − M* and correlations and its implication on their relative steepness. The final column summarises whether the signs of μ0 and δ0 are ‘necessarily the same’ (=), ‘necessarily opposite’ (≠) or ‘can be either’ (○). When discussing the implications on correlations, up(down)wards arrows represent an in(de)crease of the parameters, while horizontal arrows describes the lack of correlation. The different cell colours are purely meant to guide the eye. The top table links the initial conditions, while the bottom table summarises the implications of the evolved difference in the slopes. (α)ζ0ξ is positive, therefore δ0 can either be negative (implying (a) shallower than (b)) or positive (implying (a) steeper than (b)). (b)ζ0ξ is negative, therefore the same argument as in a holds.
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