Flyjack, Let's start over.
First, a hypothetical illustration. Assume an aircraft flying two miles above sea level, no surface winds or winds aloft, and a ground speed of 240 MPH (four miles per minute). Let's add a further simplification, there is NO ATMOSPHERE as well (repeat, this is a HYPOTHETICAL illustration).
An object (any object) that is dropped from this aircraft under these conditions will, with respect to the aircraft, stay directly under the aircraft until it strikes the earth. While descending from the aircraft, this object is only subjected to the laws of gravity which are explained in elementary physics textbooks, Wikipedia, and other online Internet sources. Using the relatively simple equations for a body falling from rest in a vacuum, the time of the fall of the object from the aircraft to the ground can be calculated. Then the distance that the aircraft travelled in that time can also be calculated.
The weight vector (as used here, vector means a force acting in a specified direction) of any body, including the one described above, is ALWAYS pointing towards the center of the earth.
Now let's revisit the above problem and remove the no atmosphere assumption. Before considering horizontal motion, let's assume that an object is dropped from a stationary balloon. We now have to consider the atmosphere's impact (or air resistance) on the falling body. For purely vertical motion, this is also relatively simple and problems along this line are considered in elementary physics books and such. Other things being the same, it would take the same object, falling from the same height, longer to reach the ground with air resistance than if it was in a vacuum.
If the falling object has sufficient altitude, it will reach a speed where the air resistance is equal to the weight of the object. The air resistance, or drag force, in this instance is the same magnitude and pointing in the opposite direction of the weight. In addition, the drag force is ALWAYS parallel to and pointing in the opposite direction of the free-stream velocity vector. And in this example, the free-stream velocity vector also points straight down or towards the center of the earth.
When we add horizontal motion in an atmosphere to our problem, the situation goes from relatively simple to intractable. The equations governing this horizontal motion become about fourth-order quadratic non-linear equations and require something on the order of a Cray supercomputer to solve. That is why we don't see tables of actual computations. Instead we have estimates and guesses about the horizontal motion of the falling body.
Incidentally, the term "throw forward" is not an aerodynamics term but a term used by skydivers. Page 233, The Skydiver's Handbook, 10th Revised Edition, by Dan Poynter and Mike Turoff, contains a discussion on forward throw and includes a chart of speeds and distances. The last thing before the chart is the phrase "we're not going to delve into the physics of deceleration resistance here". That says it all.
How about taking a look at the online information concerning free falling bodies and see if that can explain things a bit better than me. If it doesn't, feel free to ask more questions.
Robert99