Rain and Flooding

Yes. If the water moisture in the atmosphere is just right, you can see a rainbow anytime of the day. It is possible to see full circular rainbows or halos around the sun in the daytime, or even multiple ones.

The 2011 Japan earthquake and tsunami resulted in over 15,000 confirmed deaths, with many others reported missing and presumed dead. Some of the hardest-hit areas included Miyagi, Iwate, and Fukushima prefectures. The victims were from various backgrounds and included residents, tourists, and rescue workers.

Cold air is needed for snow because it keeps the water vapor in the air frozen as ice crystals. When the temperature is above freezing, the ice crystals melt and turn into rain instead of snow. Additionally, colder air has a lower capacity to hold moisture, which causes the water vapor to condense and form snowflakes.

A rainbow is a trick of the light and has no physical properties. The water drops that cause the light to show up as a rainbow can come down and touch the ground, so a rainbow can look like it is touching the ground around waterfalls and similar water features, and is so high up in the air that it appears to touch the horizon. But the rainbow will move as the observer's eyes move, so you can never get to the rainbow, but it may appear to someone else that you have reached the end of the rainbow.
If you were in a plane looking down on a rainbow you would see a complete circle. From below we only see part of it because of the Earth's curve etc. And as described above only you can see the particular rainbow that you are seeing. It looks different to anyone else because of the way the millions of raindrops reflect light individually and so differ even to someone next to you.

Relief rainfall is most likely to occur during the rainy season or monsoon season, which varies depending on the region. In tropical regions, relief rainfall is common during the summer months when warm, moist air is forced to rise over mountains, leading to cooling, condensation, and precipitation.

The funnel increases the area of catchment and makes the reading more accurate by increasing the volume of rain collected. Rainfall statistics must be standardised by specifying the mouth diameter of the funnel if the reading is to have any value.

Forms when a soluble substance separates and settles out from a solution due to a chemical reaction.

The monsoon season can bring relief from hot and dry conditions, replenishing water sources and supporting agriculture. It may also bring challenges such as flooding, transportation disruptions, and increased risk of diseases. Families may need to adjust their activities and routines to adapt to the changes in weather and conditions during the monsoon.

Rain is formed when water vapor in the atmosphere cools and condenses into liquid water droplets. These droplets continue to grow until they are heavy enough to fall to the ground as rain. This process is known as the water cycle.

Rain gauges should be placed on level ground in an open area where there are no buildings, trees, or other obstacles to block the rain. This is to prevent the water collected on the roofs of buildings or the leaves of trees from dripping into the rain gauge after a rain, resulting in inaccurate readings.

The rain is not pouring down.

Annual precipitation refers to the total amount of rain, snow, sleet, and hail that falls in an area over the course of a year. It is typically measured in millimeters or inches. This value helps to understand the climate patterns and water availability in a region.

A clapper bridge is an ancient form of bridge found on the moors of Devon (Dartmoor and ... They are often situated close to a ford where carts could cross. ... Some larger clapper bridges, such as at Dartmeet and Bellever, have collapsed – their slabs swept away by floods, or raided for building or wall construction. However ...

The amount of rainfall received in the ocean varies greatly depending on the location and ocean currents. On average, the global ocean receives about 40 inches (1,016 mm) of rainfall per year. Areas near the equator tend to receive more rainfall, while regions closer to the poles generally receive less.

Turbidity in river water during flash floods is mainly caused by sediment erosion and resuspension. As the rushing water carries debris, silt, and soil into the river, these particles remain suspended in the water column, causing it to appear cloudy and murky. Additionally, organic matter, pollutants, and other suspended solids can also contribute to turbidity levels during flash floods.

Monsoons bring heavy rainfall to the Philippines, particularly between June and September, which can lead to flooding and landslides. However, they also provide much-needed water for agriculture and replenish freshwater sources. Strong winds accompanying monsoons can also affect coastal areas with storm surges and rough seas.

Relief rainfall occurs when moist air is forced to rise over elevated terrain, such as mountains. As the air rises, it cools and condenses, leading to the formation of clouds and eventually precipitation. The leeward side of the mountain range often experiences a rain shadow effect, where the air descends and warms, resulting in drier conditions.

During the summer months, solar energy heats rock and soil on land more rapidly than it heats water in the ocean as a result air overland becomes warmer than air over the adjacent ocean. The air overland therefore expands and rises so the air pressure overland at the earths surface becomes less than that over the ocean. Resulting pressure gradient causes moist air to flow from the ocean over the land. Once over the hot surface of the land the air warms becomes buoyant and rises. The rising moist air produces thunderstorms a drenched the land leading to the common association with the word monsoon the flooding.

Rain that falls on land can either be absorbed by the soil and taken up by plants (infiltration), flow along the surface into bodies of water like streams and rivers (runoff), or evaporate back into the atmosphere.

Water stops soaking into the ground in the saturated zone because the soil pores are already filled to capacity with water. When saturation occurs, the soil becomes completely saturated, preventing any additional water from infiltrating. This can lead to water pooling on the surface or running off instead of soaking into the ground.

Precipitation occurs when water vapor in the atmosphere condenses into liquid or solid forms and falls to the Earth's surface. The type of precipitation that falls (rain, snow, sleet, or hail) is determined by the temperature of the atmosphere at different altitudes. Warmer temperatures typically result in rain, while colder temperatures lead to snow or other frozen forms of precipitation.

The term for heavy continuous rainfall is "downpour." It refers to a sudden and heavy rainstorm that can cause flooding and other water-related issues.

Acid precipitation contains rain, sleet, or snow with a high concentration of acid that comes from sulfur dioxide (SO2) and nitrogen oxides (NOx) emissions from burning fossil fuels such as coal and oil.

Surface water.