The human body heats itself at some rate, because of this, I'm trying to add a forcing function to the differential equation known as Newtons law of cooling: $Q = hA(T-T_{env}) + f$, which I suspect accurate models a very simplified situation.
We have veins and capillaries that almost-evenly distributes heat over ever cubic centimeter of our bodies. Let's assume it's completely even.
Let's say a person presses the entire palm and closed (not spread apart) fingers of their hand on a piece of dry ice, which we'll pretend is a cross-sectional rectangle of surface area, with room temperature air. This coldness will spread throughout the hand.
Then, what forcing function must I add to model the temperature of the hand over time? At what rate does the human body heat its volume to implore Newton's law of cooling?