Cosmic-ray intensity-time variations recorded in the lower atmosphere by one neutron detector (D-1, Climax, Colorado) and three ionization detectors (Freiburg, Germany; Cheltenham, Maryland; and Huancayo, Peru) are compared. Irregular intensity variations characterized by time parameters of 27 days and 24 hours are shown to occur in coincidence in the records of both types of detectors. It seems reasonable to ascribe correlated neutron and ionization intensity variations to a common origin.It has been shown that 27-day neutron intensity variations are produced by primary intensity variations. The magnitude of these variations must be greater for low energy primaries as 27-day neutron intensity variations at Climax are \ensuremath{\approx}5 times larger than corresponding ionization intensity variations at Freiburg, Cheltenham, and Huancayo. These variations must extend, however, to high energy primaries, as their effects are observed at the geomagnetic equator. From the \ensuremath{\approx}5:1 relative response (Climax neutron to northern sea level ionization detector) one parameter describing the energy dependence of 27-day primary intensity variations can be empirically evaluated. Assuming a power law similar to that describing the energy dependence of the time average primary intensity spectrum, it is found that the amplitude of 27-day primary intensity variations is required to decrease with increasing primary energy approximately one power of energy more rapidly than the time average primary spectrum itself. The electric field acceleration process hypothesis predicts primary intensity variations with approximately this energy dependence.Twenty-four-hour neutron (Climax) and ionization (Freiburg) intensity variations are correlated in local time. It is not certain that these variations are produced by primary intensity variations. Even if this were the case, the relative response (Climax to Freiburg) to such primary intensity variations cannot be accurately determined from the data studied here.