Do you know the types of precipitation? Well, it’s not only rainfall. Precipitation is when water falls from the clouds in different forms back to the earth. The water that falls during precipitation can be in liquid or solid forms.
For example, rain is a liquid form of water, and hail is a solid form of water that falls on the ground. During monsoons, you must have witnessed rainfall or snowfall. So, that is nothing but precipitation.
Without any doubt, we can say that precipitation is a crucial step in the hydrological cycle, as it delivers or replenishes water to the earth.
Precipitation occurs in different forms like rain, drizzle, snow, sleet, hail or graupel. Among these, rainfall occurs predominantly. This post explains the definition and various types of precipitation in hydrology.
Content: Types of Precipitation in Hydrology
- What is Precipitation?
- Types of Precipitation
What is Precipitation?
Meaning: In hydrology, precipitation is when the water in the atmosphere returns back to the earth in liquid or solid forms. Hydrology deals with the study of water properties, its movement on and below the earth’s surface, and the impact of human activity on water availability.
What are the Types of Precipitation?
There are three categories of precipitation based on the form of water that falls on the ground.
- Liquid-water: The water vapours condense into liquid droplets. Liquid forms of precipitation include rain and drizzle.
- Freezing water: The liquid water freezes in contact with the cold surface. Freezing forms of precipitation involve “freezing rain” or “freezing drizzle”.
- Ice: Water droplets freeze into ice crystals at higher altitudes. Frozen forms of precipitation include snow, sleet, hail, and graupel.
When Precipitation Occurs?
Clouds undergo precipitation when many water droplets or ice crystals coalesce to produce large water droplets or snow pellets. Once the size of water droplets or ice crystals becomes large enough, they fall off from clouds.
Precipitation is generally caused by the condensation of vapours into bigger and bigger water droplets. Rainfall and snowfall are expressed as depth, either mm or cm.
- A rain gauge measures the liquid precipitation or rainfall.
- A snow gauge measures the solid precipitation or snowfall.
The intensity, amount and type of precipitation differ as per the changing seasons and geographical locations. Sometimes, acid rain is produced when gaseous pollutants contaminate water droplets before falling on the ground.
Why do we sometimes get rain and sometimes get snow? It is due to the condensation of vapours at different altitudes. Water vapours at low altitudes produce rainfall, and water at high altitudes makes snowfall.
Why is Precipitation Important?
- People rely on precipitation for irrigation and drinking purposes. It also replenishes wild vegetation, moistens the air, and refills different water bodies and water table.
- Its distribution helps in deciding what the climate would be. The varying magnitude of precipitation helps in remodelling the occurrence of extreme hydrological conditions such as floods, famines and droughts.
- Precipitation purifies the air and reduces atmospheric heat by cooling the air through evaporative cooling.
- It delivers fresh water to the earth. It also regulates the global energy flow, i.e. the movement of heat.
Types of Precipitation
It is a type of precipitation that falls as water droplets over the ground. Rainfall contributes significantly to the earth’s water resources and the ecological cycle.
The size of raindrops is larger than a drizzle. But, their size may vary from big, heavy drops to light, little specs.
Tiny raindrops are cloud droplets with a spherical shape and a radius of less than 0.5 to 1 mm. In contrast, large droplets can reach up to the size of 3 mm, or in rare cases, the diameter is even more.
How Does Rain Fall?
Many water droplets of size (>0.5mm) collide and grow in size to produce a large drop (3 mm). This large drop has a flat bottom and an indented middle portion. Once the diameter of raindrops becomes 4-5 mm, they fall apart.
The intensity and duration of rainfall are inversely related. High-intensity storms produce rain for a short course. Low-intensity storms produce rain for an extended period.
- Light rainfall occurs at an intensity of 2.5 mm/h.
- Moderate rainfall has an intensity of 2.5 – 7.5 mm/h.
- Heavy rainfall has an intensity of >7.5 mm/h.
Drizzle is light liquid precipitation. It falls in the form of water drops smaller (between 0.2-0.5 mm) than the size of raindrops. Low stratiform clouds and stratocumulus clouds produce drizzles.
Sometimes, drizzle evaporates mainly due to its small size before reaching the surface and is undetectable on the ground. Thus, the precipitation rates from drizzle are 0.04 inches/day or less on the earth.
Due to the air current, the drizzle drops appear to float in the sky. Often, drizzle go along with fog but differs in the way that it falls to the ground. DZ is the METAR code for drizzle.
- Light drizzles fall up to 0.01 inches per hour.
- Moderate drizzles fall up to 0.01 to 0.02 inches per hour.
- Heavy drizzles fall greater than 0.02 inches per hour.
Freezing Raindrop and Freezing Drizzle
Both involve liquid precipitation above the surface in subfreezing temperatures and freeze on contact. But, the process of their formation is entirely different.
Freezing rain first releases from the clouds as snowflakes, which turn into a liquid when passed through a warm layer above the ground. Later, the raindrops again freeze once they strike with frozen ground. Nimbostratus is a cloud commonly associated with the production of freezing rain.
Freezing drizzle contains much smaller droplets. Unlike freezing rain, the droplets do not pass through a warm layer. Instead, they fall directly on the ground. So, drops of supercooled drizzle may freeze when they strike the cold ground. Low-level stratus clouds produce freezing drizzle.
The glaze is the resulting ice that coats the exposed surfaces by accumulating a thickness of several centimetres. FZRA is the METAR code for freezing rain. FZDZ is the METAR code for freezing drizzle.
Snowfall is a kind of precipitation common in colder and polar regions. It is a kind of precipitation that results from deposition, a transition of water vapours directly into ice.
So, snow precipitation is when the clouds release snow crystals to the ground. Snow has a complex structure with an average density of 0.1g/cc. First, the water vapours condense into ice crystals.
When enough ice crystals accumulate within the clouds, they cluster to produce snowflakes. During snowfall, the nimbostratus clouds give off many soft snowflakes. Snowfall is usually calm, not disastrous like a hailstorm.
Are all snowflakes unique? The answer is yes because each ice crystal travels a unique path towards the ground with varying temperatures and humidity levels.
It gives different patterns and shapes to the ice crystals due to the different journeys to the ground. So, individual snowflakes differ in a certain way.
It forms when the raindrops pass through the air at subfreezing temperatures. First, the snowflakes travel through a warm layer of air and turn into raindrops.
Then, raindrops move down toward a below-freezing layer of air at the earth’s surface. The liquid refreezes into ice pellets, called sleet. The temperature inversion first melts the snow and then refreezes it.
So, sleets are frozen raindrops. They fall as small, globose, clear ice pellets with a diameter of 5 mm or less. They are a result of the freezing of melted snowflakes or raindrops. It is different from snow, hail, and freezing rain.
It is a type of precipitation that occurs in the form of small ice balls called hailstones. Hail is associated with violent thunderstorms.
Unlike snow, hailstones are hard and 5 mm or more in diameter. The size of hailstones is like small rocks that can weigh more than a pound.
Hail sizes of 2.5 cm or more imply severe thunderstorms. Hailstones fall as frozen irregular lumps of ice. Cumulonimbus clouds are responsible for producing hail.
Such clouds produce thunderstorms that uplift water droplets above the atmosphere’s freezing layer. There, water droplets encounter more supercooled water and freeze into the ice particles.
The process repeatedly occurs, causing ice particles to grow big enough to produce ice balls or hailstones. So, this alternate freezing adds another layer of ice to the tiny bits of ice particles.
Soft hail, hominy snow, or snow pellets are the alternative names for the term graupel. It falls as the crisp, non-transparent rime balls of size 2-5 mm.
Graupel forms through riming, in which supercooled water droplets freeze on encounter with snow crystals at a temperature below 0°C. Graupel is different from hail in terms of formation and appearance.
You can distinguish graupel from hail by the shape, texture and circumstances in which it falls. Hailstones are hard, large, uniform and fall only during thunderstorms.
Unlike hail, graupel has a soft texture, small size, and it falls typically during winter thunderstorms. GS is the METAR code for graupel.
Thus, we can say that there are different types of precipitation based on different temperature and humidity levels in the atmosphere.