The Coriolis force is much smaller in magnitude that the force of gravity.
In this case, Ώ is a small parameter.
We can writer
"z=h-\\frac {g\u00d7t\u00d7t}{2} (1)"
The particle hits the ground when
"t=\\sqrt {\\frac {2h}{g}} (2)"
The net eastward deflection of the particle as strikes the ground is
"d=\\frac {\u038f}{3} \u00d7 \\cos\u03bb\u00d7\\frac {8\u00d7h\u00d7h\u00d7h}{g}"
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