A major wind system is blowing perpendicular to a 4 km highmountain range. The moist air arrives at the upwind side at atemperature of 2°C then ascends from sea level. At the top of themountains it has lost all its moisture. It then descends back tosea level on the lee side of the mountain range. What temperaturewould be expected at sea level on the lee side? What is this effectcalled and what would you expect to see looking from the lee sideto the top of the mountains? What might the consequences be forecosystems of this effect?