The latitude-temperature graph reflects significant variations in temperature due to a combination of factors, including measurement methods and site locations over fifty years of data collection. Higher latitudes experience greater temperature increases primarily because their climate is influenced by energy transported from lower latitudes, rather than direct solar radiation. This energy transfer occurs through water vapor and ocean currents, where water evaporates in warmer regions, moves north, and releases heat upon condensation. Consequently, increased atmospheric water vapor during warming periods enhances this heat transfer, resulting in more pronounced warming at high latitudes. Additionally, the northern hemisphere exhibits more significant temperature changes due to its lower heat capacity, allowing for quicker thermal adjustments compared to the southern hemisphere.