As days are longer in the summer (the Sun spends more time above the horizon) AND the Sun gets higher in the sky during summer days (meaning it deposits more energy per square metre of the surface of the Earth in the hemisphere), temperatures in the summer are hotter than they are in the winter and more solar generation is possible in the summer than the winter. These have not yet . During the spring and summer months, and part of autumn it corresponds to 1 PM Central Daylight Time. Asia Pacific; EMEA; Latin America; UK Solicitors; UK Bar; United States If a media asset is downloadable, a download button appears in the corner of the media viewer. The June solstice is the summer solstice in the Northern Hemisphere and the winter solstice in the Southern Hemisphere. Saturnalia was a wild carnival, as well as a time to mark the passing of the seasons. Text on this page is printable and can be used according to our Terms of Service. Noon Sun Angle Equation Noon Sun Angle = 90 - Zenith Angle Zenith Angle: Subsolar point & your location are in the same hemisphere, subtract! Animation showing how the tilt angle changes from the summer solstice in the northern hemisphere (or winter in the southern hemisphere) to the northern hemisphere winter solstice (summer in the south). Mid-latitudesEarths solstices are largely marked by the transition of the subsolar point across the tropics. The timing and extent of solstices are largely determined by the planets axial tilt, orbital eccentricity, and distance from the sun. Th. The declination angle can be calculated by the equation 1: = - 23. It varies due to the inclination of the earth's polar axis and its revolution around the sun.