Precipitation and Elevation
What usually happens is that moisture laden air is blown toward mountains and forced to climb higher. As it rises, it tends to  become colder and less dense, so can hold less moisture. The surplus moisture is often precipitated in the hills or mountains, so when the air passes beyond the mountains there is much less rainfall. This is known as rain shadow. Here in Hereford UK we have plenty of rain, but not nearly as much as some places in the Welsh hills which lie 20 miles to the west of us, so I think we benefit a little from rain shadow. It was my experience in Borneo that there was more rain in the hills than at lower altitudes, but whether this holds true for the summit if Mount Kinabalu, which is over 12,000 feet high, I am not so sure. Probably not. More likely the rain is precipitated on the lower slopes.