In the (non-inertial) rotating frame of reference bound to Phobos, with nadir/prograde directions setting the axis, the constant force towards Mars is the weight of Phobos.
Phobos semi-major axis (or orbital radius; it has very low eccentricity): 9376 km
Phobos mass: 1.06 x 10$^1$$^6$ kg,
Mars mass: 6.39 x 10$^2$$^3$ kg
The force of gravity: $F = G {{m_1 m_2}\over r^2}$
Result: 5.22 x 10$^1$$^5$ N, force equivalent to weight of 532 billion tonne on Earth.
That force, though, is constantly offset by the centrifugal force (remember: non-inertial frame of reference!) - that's why Phobos isn't falling down onto Mars immediately. So its speed towards Mars is pretty much zero - save for minuscule movement as tidal forces brake it and centrifugal force drops slightly - resulting in Phobos orbital radius dropping, orbital speed rising and equilibrium between weight and centrifugal force restored.
Accelerating towards Mars will achieve nothing, as the resulting reduced orbital radius immediately converts to increased orbital speed, and equivalent centrifugal force ejecting it back to prior orbit or even further as soon as your pushing force vanishes.
Due to tidal forces, Phobos loses altitude - moves towards Mars at 1.8 centimeters per year; but that's a pretty much constant speed - if there was an isolated, unbalanced force, it would be accelerating its descent, as per Newton's second law of motion. Meanwhile, it sticks to the same average altitude loss rate, meaning the forces inwards/outwards are perfectly balanced.