The short answer is "to some extent". For instance, take a look at the abstract for
http://dx.doi.org/10.1119/1.14280
The long answer basically explains why its difficult to quantify this. Suppose you are stationary in space, near a large object. You can then measure the gravity of that object by measuring your acceleration with an accelerometer, the acceleration you need to "hold station" a constant distance away.
If you have a massive object whizzing by, though, it becomes very difficult to determine how to "hold station". It's easy to move in free-fall, but that's not what's wanted here. So, perhaps you try to look at distant stars, to triangulate your location, but you do so you find that gravity is warping the path of light in a manner that varies with time as the massive object whizzes by. So, the triangulation idea won't work either, unless you model how the light is being bent, but the whole idea is to measure the effect directly.
Another way of explaining the issue: it turns out the answer to "what is the field" depends on the specific details of the coordinate system you choose.
The easiest (and in long run the best) thing to do is to not attempt to make a direct measurement of the "gravitational field". This avoids all the measurement and coordinate dependence issues. The paper I quoted measures, instead, the velocity that someone picks up from the large mass while it whizzes by. This is an easy measuremnt to make, because it occurs in flat space-time. You measure the velocity before, and the velocity after, and that determines some sort of effective mass number. Howver, with this approach you get only a number, and not anything that describes how the field appears in space.
Another thing you can do, as I suggested, is to use a gravity gardiometer also called a forward mass detector to measure the gravity gradient. See the previous post for a reference to the details of how this device works. It measures not gravity, but how fast it changes, i.e. tidal forces. For a stationary object, and Newtonian gravity, the gravity gradient will be 2m/r^3 in a direction pointing towards the object (as opposed to m/r^2 for the gravitational force itself). So we can see that the gravity gradient gives us a mesurement of mass.
TThe second approach, using a gravity gradiometer, gives you a slightly better description of what the field "looks like" -as I said previously, the field is concentrated in the transverse direction, much like the electric field of a moving charge.
If you are not familiar with the electric field of a moving charge, take a look at http://www.phys.ufl.edu/~rfield/PHY2061/images/relativity_15.pdf.
I've got a post somewhere that gives the results of what the tidal force (gravity gradient) of a moving mass is, mathematically, if you really want the details. This is something that I had to work out for myself, BTW - the textbooks cover some special cases, which can be used to spot-check the results, but so far I haven't found one that works out the general problem.