An empirical model of height-integrated Pedersen and Hall conductance inferred from the TIROS-NOAA satellite dare are introduced and reviewed.The contours of both Pedersen and Hall conductance are drawn with the magnetic latitude-magnetic local time coordinates between 45°-90°GM and 0-24 MLT for discrete levels of particle precipitation. Similar contours of conductance controlled by solar irradiation in different seasons are also shown with same coordinates but for 9°-90°GM and 0-24 MLT. The internal relationship between the magnetosphere-ionosphere coupling and conductance model is investigated too.