Quote Originally Posted by Facubaci View Post
Oh, how complicated. Well, I have to say that there is a large island at the southwest of this great continent. It's far, and measures a third the size of this map. I can not draw a picture now, tomorrow yes. I don't think that island cares, it's like Australia, that it's far than Asia and in the other way (in the southwest).
Ok then I will suppose the impact of the ITCZ is minimal during winter, meaning it sits more or less on the equator or little to the south.
Quote Originally Posted by Facubaci View Post

My map has a middle-low pressure almost entirely. In the southern hemisphere there is no another landmass. And the areas from Ecuador to the parallel 30 or 35 ° would be tropical climate, wet tropical, warm steppe, desert, some Mediterranean climate at the west of the mountains between 30 ° and 45 ° and in the east would be like Manchuria (Dwa?).
yes it will look like this on the west coast. The east coast is different and I don't think there is a Manchurian climate. The north east is always wet and cannot be Dwa. More like Dfa/Dfb.


Quote Originally Posted by Facubaci View Post
The mid-continent area is bisected by a mountain, so in that zone would be mountain climate. And the other areas are relatively close to the coast.
I'm making a plan and I won't include mountain climate. Following the Koppen classification, alpine climate does not exist. It would cover a wide range of possibilities anyway. I will just ingrone that part for the moment.

Quote Originally Posted by Facubaci View Post
Thanks for the the pictures of the polar front. But i thought that in summer the polar front can be retired near to the pole. Why it can reached to latitude 30? I thought that in winter the polar front should be very wide and narrower in summer.
Your right, I contradicted my own sources. It goes south during the winter like the ITCZ.