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Question

Which of the following is a non-recording rain gauge?

The correct answer is

Simon’s rain gauge

Understanding Rain Gauges and Precipitation Measurement

Rain gauges are important meteorological instruments used to measure the amount of precipitation (rain, snow, hail, etc.) over a specific period. Measuring precipitation is crucial for various applications, including water resource management, flood forecasting, agricultural planning, and climate studies.

Rain gauges can be broadly classified into two main types based on how they record data:

  • Non-Recording Rain Gauges: These gauges simply collect precipitation, and the total amount is measured manually at specific intervals (e.g., daily). They do not provide continuous records of precipitation intensity over time.
  • Recording Rain Gauges: These gauges provide a continuous record of precipitation amount and/or intensity over time. They automatically record the data, eliminating the need for frequent manual measurements.

Analyzing Rain Gauge Types

Let's look at the types of rain gauges mentioned in the options:

  • Weighing Type Rain Gauge: This is a recording type of rain gauge. It measures the weight of accumulated precipitation in a receiver bucket. The weight is recorded continuously on a chart or electronically, providing a record of cumulative precipitation over time.
  • Tipping Bucket Rain Gauge: This is also a recording type of rain gauge. It consists of a seesaw-like container divided into two compartments. When a small, calibrated amount of precipitation (e.g., 0.25 mm) collects in one compartment, it tips, empties the water, and brings the other compartment into position. Each tip is recorded electronically, providing data on both the amount and intensity of precipitation.
  • Simon’s Rain Gauge: This is a classic example of a non-recording rain gauge. It is a simple cylindrical container with a funnel at the top. Precipitation collected in the container is measured manually using a graduated measuring cylinder at regular intervals. It only provides the total precipitation depth over the collection period.
  • Float Type Rain Gauges: This is a recording type of rain gauge. Precipitation is collected in a chamber containing a float. As the water level rises, the float moves up, and its movement is recorded on a chart or electronically, providing a continuous record of cumulative precipitation.

Identifying the Non-Recording Rain Gauge

Based on the analysis of the different types, we can determine which one is a non-recording rain gauge:

Rain Gauge Type Recording or Non-Recording? How it Works
Weighing Type Recording Measures weight of accumulated precipitation
Tipping Bucket Recording Tips and records when a fixed volume is collected
Simon’s Rain Gauge Non-Recording Collects precipitation for manual measurement
Float Type Recording Uses a float to record water level changes

Therefore, among the given options, Simon’s rain gauge is the one that does not automatically record the precipitation data over time; it requires manual measurement.

Revision Table: Types of Rain Gauges

Type Characteristics Output Data
Non-Recording (e.g., Simon’s) Simple design, manual reading Total precipitation over a period (e.g., 24 hours)
Recording (e.g., Weighing, Tipping Bucket, Float) Automatic recording mechanism Continuous record of cumulative precipitation or intensity over time (hyetograph)

Additional Information on Precipitation Measurement

Precipitation measurements are essential for hydrological modeling and water resource management. The accuracy of these measurements can be affected by factors such as wind, evaporation, and splash. Standard practices are followed to minimize these errors, such as installing rain gauges in open areas away from obstructions and at a standard height above the ground.

While non-recording gauges are simpler and cheaper, recording gauges provide more detailed information that is crucial for understanding rainfall patterns, peak intensities, and their impact on runoff and flooding.

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Important Questions from Precipitation

  1. Penman's equation is based on:
  2. Isohyet is a line joining points having

  3. In Symons rain gauge, the rim of the collector is set in a horizontal plane at a height of ________ above the ground level.

  4. The total rainfall in a catchment area 1200 km2 during a 6 hours storm is 16 cm. While the surface run-off due to storm is 1.2 × 108 m3. The φ index is

  5. Which rain gauge is NOT able to gives a plot of a mass curve of rainfall?

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