Same as the previous question, but specifically for over steep mountainous terrain. Discuss. Finite-difference equations are approximations to the full, differential equations that describe the real atmosphere. However, such finite-difference equations can also be thought of as exact representations of a numerical atmosphere that behaves according to different physics. How is this numerical atmosphere different from the real atmosphere? How would physical laws differ for this numerical atmosphere, if at all? When the NWP model runs for a long time, if it approaches steady state, is this state equal to the real climate or to the “model” climate?
Same as the previous question, but specifically for over steep mountainous terrain. Discuss….
Same as the previous question, but specifically for over steep mountainous terrain. Discuss. Finite-difference equations are approximations to the full, differential equations...
