How does the distribution of land and water affect average temperatures in cities?

The distribution of land and water plays a crucial role in influencing average temperatures in cities, particularly through its effects on seasonal temperature variations. Water has a high heat capacity, meaning it can absorb and retain heat more effectively than land. This property results in a moderating effect on temperature, leading to cooler summers and warmer winters in coastal areas compared to inland regions.

During summer, land heats up quickly, resulting in higher temperatures, while water bodies remain cooler. Conversely, in winter, land cools down rapidly, while the water retains heat, thus keeping nearby areas warmer. This differential heating leads to more pronounced seasonal variations in temperature in areas dominated by land compared to those located near large bodies of water.

By influencing patterns of heat distribution, the land-water distribution ultimately impacts local climate and temperature trends within cities, making this answer particularly relevant to understanding climate change and geographical differences. The other options do not accurately capture the intricate relationship between land and water distribution and temperature dynamics in urban settings.