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Time:2024-09-12 10:45:00 Popularity:17006
Rainfall measured in mm describes the equivalent depth of water over a horizontal surface, rather than a volume for an unspecified area. If the collected water were distributed evenly without losses, that depth would be the same millimetre value. This makes rainfall amounts comparable while allowing total volume to be calculated for a known area.

The most useful relationship is:
1 mm of rainfall = 1 liter of water per square meter (1 L/m²)
This makes rainfall easy to compare between locations of different sizes. Whether the rain falls on one square meter, one hectare or an entire watershed, the rainfall depth can still be expressed using the same millimeter value.
One millimeter of rainfall means that the precipitation would form a water layer 1 mm deep over a horizontal surface.
Because one square meter has an area of 1,000,000 mm², a water layer 1 mm deep has a volume of 1,000,000 mm³, which is equal to 1 liter.
| Rainfall Depth | Water per m² | Water per Hectare |
|---|---|---|
| 1 mm | 1 L | 10,000 L / 10 m³ |
| 5 mm | 5 L | 50,000 L / 50 m³ |
| 10 mm | 10 L | 100,000 L / 100 m³ |
| 50 mm | 50 L | 500,000 L / 500 m³ |
| 100 mm | 100 L | 1,000,000 L / 1,000 m³ |
Liters describe a volume of water, but the total volume depends on the size of the area.
For example, 10 mm of rainfall represents:
10 liters over 1 m²
1,000 liters over 100 m²
100,000 liters over 1 hectare
The rainfall event is the same in each case: 10 mm. Using depth therefore provides a standardized measurement that does not depend on the area being discussed.

A rain gauge collects precipitation over a known opening area. The amount collected can be converted directly into an equivalent water depth.
Rainfall events often involve relatively small depths, so millimeters provide a convenient level of resolution without requiring decimals in meters.
A measurement of 25 mm means the same rainfall depth whether it is recorded at a small farm, a city weather station or a hydrological monitoring site.
Because 1 mm equals 1 L/m², rainfall depth can be converted easily into total water volume when the area is known.
Millimeters provide a standardized metric unit for recording and comparing precipitation data across meteorological, agricultural and hydrological applications.
If the rainfall depth and surface area are known, the total water volume can be estimated using:
Water Volume (liters) = Rainfall (mm) × Area (m²)
For example:
20 mm rainfall × 500 m² = 10,000 liters of water
For one hectare:
20 mm × 10,000 m² = 200,000 liters = 200 m³
This is useful in agriculture, reservoirs, irrigation planning and water-resource calculations. However, the calculated rainfall volume is not the same as the amount of water that remains available to plants because runoff, infiltration, evaporation and drainage also affect the final water balance.
Some countries and weather services also report rainfall in inches.
| Millimeters | Inches |
|---|---|
| 1 mm | 0.0394 in |
| 10 mm | 0.394 in |
| 25.4 mm | 1 in |
| 50 mm | 1.97 in |
| 100 mm | 3.94 in |
The conversion is:
1 inch = 25.4 mm
A rain gauge has a known collection area. Rain entering this area is collected or detected and converted into an equivalent rainfall depth.
Different instruments use different measurement methods:
Manual gauges collect water for direct reading.
Tipping bucket gauges count calibrated volumes of water.
Weighing gauges measure accumulated precipitation mass.
Piezoelectric sensors estimate rainfall from raindrop impacts.
For more detail, see How Does a Rain Gauge Work?
The NiuBoL NBL-W-RS tipping bucket rain gauge is available with a 0.2 mm rainfall resolution. This means each calibrated bucket tip represents 0.2 mm of rainfall.
| Bucket Tips | Rainfall |
|---|---|
| 1 | 0.2 mm |
| 5 | 1 mm |
| 25 | 5 mm |
| 50 | 10 mm |

The tipping events can be recorded through pulse output or processed through an RS485 Modbus transmitter, depending on the rain gauge configuration.
For agriculture, rainfall depth provides a convenient indication of natural water input.
For example, 15 mm of rain theoretically corresponds to 15 liters of water per square meter. However, not all of this water necessarily remains in the crop root zone.
Actual crop water availability also depends on:
Soil texture
Infiltration rate
Runoff
Drainage
Evaporation
Root depth
Existing soil moisture
For irrigation management, rainfall data is therefore more useful when combined with soil-moisture measurements and crop information.
In hydrology, rainfall depth provides a standardized input for analysing catchments, river flow, reservoirs and flood conditions.
When rainfall depth is combined with catchment area, engineers can estimate the total precipitation volume falling over that region.
Rainfall volume is not a direct prediction of river discharge. Infiltration, vegetation interception, evaporation and storage affect event runoff, while routing and water already stored in the catchment also affect the observed flow. Keep the measured precipitation input distinct from the resulting catchment response.
A rainfall value of 10 mm does not mean individual raindrops are 10 mm in diameter. It refers to accumulated water depth.
A rainfall measurement represents precipitation received, not the actual depth of standing water after infiltration, runoff and drainage.
It means 10 liters per square meter. Total volume depends on the surface area.
A rain gauge with 0.1 mm resolution is not automatically more accurate than a 0.2 mm instrument. Resolution describes the smallest reported increment, while accuracy describes closeness to the reference rainfall amount.

A1. Because rainfall is expressed as an equivalent water depth over a horizontal surface. Millimeters provide a convenient and standardized unit for this depth.
A2. It means the rainfall would form a water layer 1 mm deep. This is equivalent to 1 liter of water per square meter.
A3. Ten millimeters of rainfall equals 10 liters per square meter, or approximately 100 cubic meters over one hectare.
A4. One inch of rainfall equals 25.4 mm.
A5. Rainfall is normally reported as depth. If the area is known, that depth can then be converted into a total water volume.
A6. No. It represents precipitation depth. The actual standing water depends on infiltration, runoff, drainage and evaporation.
A7. A rain gauge is used to measure rainfall. Common types include manual, tipping bucket, weighing and electronic rainfall sensors.
A8. It means the rain gauge reports rainfall in increments of 0.2 mm. For a 0.2 mm tipping bucket gauge, each completed tip represents 0.2 mm of rain.
A9. Millimeters provide a convenient level of detail for typical rainfall amounts. Using centimeters would require more decimal values for smaller rain events.
A10. Yes, rainfall depth can be converted into water volume, but irrigation decisions should also consider soil moisture, runoff, infiltration, drainage, crop demand and evapotranspiration.
NBL-W-ARS-Tipping-bucket-rain-gauge-instruction-manual.pdf
NBL-W-RS-Rain-sensors-instruction-manual-V4.0.pdf
NBL-W-DRS-Double-Tipping-Bucket-Rain-Sensor-Instruction-Manual.pdf
Rainfall in millimetres is a depth, with 1 mm equal to 1 L/m². Use area to calculate incident water volume, and keep that volume distinct from root-zone water or catchment runoff. NiuBoL tipping bucket rain gauges provide a measured rainfall input for appropriately configured monitoring systems.
For product selection, provide the required rainfall resolution, output signal, quantity, cable length, installation environment and whether a data logger, 4G communication, solar power or private-server integration is required.
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