The humidity created by the boiling wort just above the kettle will be much greater than the ambient humidity. This layer just above the kettle reduces the evaporation rate effectively creating a buffer between the cooler air and the hot wort. If your humid summer days also have a slight breeze, this diffuses the layer and increases the rate the wort evaporates. If your cold winter brew days have little breeze, the layer stays close to the wort slowing the evaporation rate. As heat also affects evaporation rate, hot summer days have a higher evaporation rate than cold winter days due to greater excitement of molecules as the heat rises.