In summer at noon the sun should be high enough to give rated power to ... I'd say at LEAST 70º latitude.
You overlook the length of the light's path through the atmosphere.
I did not. I
EXPLICITLY considered path length, which is why I specified that the sun should be at least 45º above the horizon — which is true at midsummer noon everywhere at less than around 70º latitude (as I specified) — at which point the path length is quite minimal at only 1.4x longer than if the sun is directly overhead.
The effective depth of the atmosphere (i.e. the actual depth if the same mass of air was all at sea level density) is around 28000 ft or 8.5 km.
At a 45º slope the effective path length is only about 3.5 km longer.
When the sun is low the light can have to travel many tens of km through the atmosphere — and has a far higher chance of meeting a cloud. That's why I think it's just about useless to point panels east and west to catch the low sun ... unless you have no more space to put ones facing the equator.
If you like we can forget about 70º latitude. Very few people live more than 55º from the equator (Glasgow, Edinburgh, Copenhagen, Moscow, all the Siberian cities, Edmonton) where the midsummer noon sun gets 58.5º high, for about 1.5km extra path length compared to the zenith. And almost no one at all more than 60º (Oslo, Stockholm, Helsinki, St Petersburg, Yakutsk, Magadan, Anchorage) where the midsummer noon sun gets 53.5º high for about 2km extra effective path length compared to the zenith.
The summer sun in Oslo / Stockholm / Anchorage is more than 20º higher than the winter sun here in northern NZ (31.1º in June 17-26), but I get near maximum power from my MPPT if the sky is clear with just a 10% over-panelling so even at that low elevation the path length attenuation is not a huge thing.
Sure, having the sun at the zenith is optimal, but 30º or 35º or even 45º from the zenith is no big deal in terms of attenuation of the sun.