Charged colloidal monolayers at the interface between water and air (or oil) are used in a large number of chemical, physical, and biological applications. Although considerable experimental and theoretical effort has been devoted in the past few decades to the investigation of such monolayers, some of their fundamental properties are not yet fully understood. In this article, we model charged colloidal monolayers as a continuum layer of finite thickness, with a separate charge distribution on the water and air sides. The electrostatic surface free energy and surface pressure are calculated via the charging method and within the Debye-Hiickel approximation. We obtain the dependence of surface pressure on several system parameters: the monolayer thickness, its distinct dielectric permittivity, and the ionic strength of the aqueous subphase. The surface pressure scaling with the area per particle, a, is found to be between a(-2) in the close-packing limit and a(-5/2) in the loose-packing limit. In general, it is found that the surface pressure is strongly influenced by charges on the air side of the colloids. However, when the larger charge resides on the water side, a more subtle dependence on salt concentration emerges. This corrects a common assumption that the charges on the water side can always be neglected due to screening. Finally, using a single fit parameter, our theory is found to fit the experimental data well for strong- to intermediate-strength electrolytes. We postulate that an anomalous scaling of a(-3/2), recently observed in low ionic concentrations, cannot be accounted for within a linear theory, and its explanation requires a fully nonlinear analysis.