Did you find this paper?
http://onlinelibrary.wiley.com/doi/10.4319/lo.2012.57.5.1453/pdf. It uses both terms:
"Absorbance corrected for offset was then converted to Napierian absorption coefficient, a
g(λ) (m
-1). The dependence of a
g(λ) on λ is typically described using Eq. 1:
a
g(λ) = a
g(λ
0)e
-S(λ-λ0) (1)
where λ
0 < λ and S is the spectral slope coefficient in the λ
0–λ-nm spectral range. Spectral slope coefficients were estimated using a linear fit of the log-linearized a
g(λ) spectrum over their respective spectral range and are reported here with units of nm
-1. Measurements of DOC and a
g(350) were used to calculate DOC-normalized absorption coefficients (a
g(350) : DOC), expressed here in units of L mol
-1 cm
-1."
From this I take it that Napierian absorption coefficient is the absorbance per unit length of the sample. (Napierian means using natural logs rather than log
10.) Thus A = ln(I
0/I
t) and a = A/l, where l is the path length.
Spectral slope coefficient is a measure of how the absorption coefficient changes with wavelength. In appropriate circumstances, over a relatively narrow wavelength range, it can be described by Eq. 1, i.e. it varies exponentially with wavelength.