City-states employed various methods to prevent flooding, such as constructing elaborate drainage systems, digging canals, and building levees and dikes to control the flow of water. Additionally, they strategically planned the layout of their cities to avoid settling in flood-prone areas. These engineering solutions helped minimize the impact of flooding on city-states.

The northwest coastal zone of Africa is influenced by the seasonal monsoon winds, particularly the northwest African monsoon, which brings moisture and rainfall to the region. Additionally, proximity to the Atlantic Ocean allows for moisture to be transported inland, supporting agricultural activities in the area. The combination of these factors helps to bring sufficient rainfall to the northwest coastal zone of Africa to support agriculture.

Areas prone to floods include those near rivers or lakes, in low-lying regions, coastal areas, and regions with poor drainage systems or heavy rainfall. Urban areas with extensive pavement or concrete surfaces can also experience flooding due to increased runoff.

"The Land of Little Rain" by Mary Austin was first published in 1903.

Monsoons often occur in South and Southeast Asia, including countries such as India, Bangladesh, Myanmar, Thailand, and Vietnam. These regions experience seasonal shifts in wind patterns that bring heavy rainfall during the monsoon season.

A floodplain is typically found next to a river and is the flat area on either side that gets flooded during periods of high water flow. It is an important natural feature that helps absorb excess water during flooding events.

The Somerset Levels flooded due to a combination of heavy rainfall, high tides, and insufficient drainage systems in the area. The flat topography of the region also contributed to the prolonged flooding.

The Atacama Desert in Chile is considered the driest place on Earth, receiving an average of less than 0.04 inches (1 mm) of rainfall per year. This extreme aridity is due to its location between the Andes Mountains and the Pacific Ocean, which create a rain shadow effect.

Rainwater will flow downhill, following the natural slope of the land. It will collect in rivers, streams, ponds, or lakes, eventually making its way to the ocean. Along the way, it may also be absorbed into the ground, recharging groundwater reserves.

A rainstorm can cause erosion of soil, leading to landslides and mudslides. It can also contribute to flooding, which can alter the shape of rivers and streams. Additionally, heavy rain can wash away vegetation and impact the local ecosystem.

Where people live can greatly impact their quality of life. Factors such as access to resources, job opportunities, environment, safety, and community amenities can all influence an individual's well-being and overall lifestyle. Different regions or neighborhoods may offer varying levels of support and opportunities for social, economic, and personal growth.

A desert region typically receives little rain due to its arid climate and lack of moisture in the atmosphere. The combination of high temperatures and low precipitation in desert areas contributes to their dry conditions.

Floods occur more frequently in some parts of the US due to factors such as heavy rainfall, proximity to rivers or coastlines, and topographical features that make areas more prone to flooding. Human activities like urbanization and deforestation can also increase the risk of flooding by disrupting natural drainage systems.

Regions near the equator tend to receive more rainfall due to the presence of the Intertropical Convergence Zone. Additionally, areas with large bodies of water, such as coastlines and islands, often receive higher levels of rainfall due to increased moisture in the air. Lastly, mountainous regions can also experience high levels of rainfall as air is forced to rise and cool, leading to condensation and precipitation.

The north coast may receive more rain due to prevailing wind patterns that bring moisture-laden air from the ocean, which then cools and releases rain as it meets the land. This phenomenon is known as orographic rainfall, where the elevation of the coastal mountains forces the air to rise and cool, facilitating condensation and precipitation. Additionally, the north coast's proximity to the equator may also contribute to higher rainfall rates due to the Intertropical Convergence Zone (ITCZ) shifting closer to the region.

The region likely receives the most rain due to its geographic location, such as being near large bodies of water or mountain ranges that contribute to higher levels of precipitation. Additionally, prevailing wind patterns and weather systems may play a role in bringing moisture to the area, resulting in increased rainfall compared to other regions.

Cities often have more impervious surfaces like concrete and asphalt, which don't absorb water. This leads to increased runoff, which can contribute to more frequent and intense rainfall events in cities. Additionally, the heat generated by urban areas can enhance the formation of rain clouds through a process called the urban heat island effect.

The flooding of the four towns to create the Quabbin Reservoir began in 1939 when the Kent, Dwinell, Dana, and Enfield were disincorporated. The construction of the reservoir was completed in 1946.

The southwest monsoon occurs in the summer months, typically from June to September in South and Southeast Asia.

The average annual rainfall in Tanzania varies depending on the region. In general, coastal areas receive around 1000-2000mm of rainfall per year, while inland areas receive between 500-1000mm of rainfall annually. Some regions in Tanzania, such as the highlands, can receive higher amounts of rainfall exceeding 2000mm per year.

Klerksdorp, South Africa has an average annual precipitation rate of around 400-500 millimeters per year.

Countries such as Egypt, Libya, and Saudi Arabia are known to receive very minimal rainfall throughout the year due to their arid climate and geographical location. These regions are characterized by desert landscapes and experience extremely low precipitation levels.

South America has diverse climates with varying rainfall patterns across different regions. The Amazon rainforest, for example, receives high annual rainfall levels, while coastal desert areas like the Atacama Desert in Chile are extremely dry. The overall rainfall in South America can range from very high in tropical regions to very low in desert areas.

The Great Plains region typically receives more rainfall than inland areas due to its proximity to moisture sources like the Gulf of Mexico and the Rocky Mountains. These geographical features contribute to favorable conditions for the formation of precipitation, leading to higher rainfall amounts in the Great Plains compared to more inland regions.