Albuquerque gives the heat back at night, and that swing is the whole personality of a house here. Afternoons on the valley floor and the West Mesa still bake stucco and flat roofs. After sunset the high desert lets go, and a shoulder-season day can demand cooling at four and heat before dawn. Winter adds light snow, hard mornings, and pipes that freeze on a clear night. Summer adds a monsoon that tests canales and grades. Spring adds wind. This is not Phoenix refusing to cool, and it is not a Wasatch winter buried in snow. It is a high-desert city with a daily temperature argument.
The roofs tell you the town. Parapets, flat membranes, and canales move water in short, rude bursts or fail and send it down the stucco. Pitched shingles show up in later neighborhoods and still take sun and wind. Evaporative coolers sit on the roof like a local landmark, because dry air and cold nights let them work. Furnaces sit inside for the mornings that are not optional. Adobe and thick stucco hide leaks. Frame houses in the Northeast Heights and tract edges hide more ordinary cavities and still freeze on the outside wall. Cottonwoods in the North Valley and along the bosque find sewer lines. The foothills take more wind and a sharper night than Nob Hill.
What people call about is practical. A pond on a flat roof. A cooler curb staining the ceiling. A west room that overheats and then a bedroom that is cold at midnight. Scale in the heater. Mice or pack rats when the nights turn. A yard that sends monsoon water at the foundation. Hail happens and is not the reason the city exists. Cold nights plus sun plus flat roofs are the reason.
Say the symptom and the roof shape. If a policy question is attached, have the deductible. The neighborhood matters only if it explains a parapet, a foothill lot, or a bosque tree.
Pick the trade that matches this swing, not a script from a lower desert or a snow city. Pick the trade and call.