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Question

Isohyet is a line joining points having

The correct answer is Equal rainfall depth of given duration

Understanding Isohyets in Meteorology and Hydrology

The question asks about the definition of an Isohyet. An Isohyet is a specific type of isoline, which is a line on a map connecting points of equal value for a particular phenomenon.

Analyzing the Isohyet Definition

Let's examine the given options to understand what an Isohyet represents:

  1. Equal evaporation rate: A line joining points of equal evaporation rate is typically called an Isoevaporate or Iso-E line.
  2. Equal Barometric pressure: A line joining points of equal barometric pressure is called an Isobar. Isobars are commonly used on weather maps to show pressure systems.
  3. Equal height above MSL: A line joining points of equal height above Mean Sea Level (MSL) is called a Contour line or Isohypse. Contour lines are used on topographic maps to show elevation.
  4. Equal rainfall depth of given duration: A line joining points that have received the same amount of rainfall over a specific period (duration) is called an Isohyet. These lines are crucial in creating isohyetal maps, which are used to visualize the spatial distribution of precipitation.

Based on these standard definitions used in meteorology and hydrology, an Isohyet specifically connects points with equal rainfall depth for a defined period.

Why the Correct Option Defines Isohyet

The term "Isohyet" is derived from the Greek words "isos" meaning "equal" and "hyetos" meaning "rain". Therefore, it directly translates to a line of equal rain. Hydrologists and meteorologists use isohyets to draw isohyetal maps, which are essential for analyzing precipitation patterns, estimating average rainfall over an area (using the isohyetal method), and studying hydrological events like floods.

The option that correctly defines an Isohyet is the one that states it joins points having equal rainfall depth of given duration.

Comparing Different Isoline Types

It's helpful to distinguish Isohyets from other common types of isolines:

Isoline Type Quantity Represented
Isohyet Equal rainfall depth
Isobar Equal atmospheric pressure
Contour line (Isohypse) Equal elevation (height above MSL)
Isotherm Equal temperature
Isohel Equal duration of sunshine

Each type of isoline helps visualize the distribution of a specific variable across a geographic area.

Conclusion

An Isohyet is a line used on maps to connect geographical points that have received the same amount of precipitation over a specific interval of time. This makes option 4 the correct definition.

Revision Table: Key Hydrological and Meteorological Lines

Term Definition Relevant Field
Isohyet Line of equal rainfall depth Hydrology, Meteorology
Isobar Line of equal atmospheric pressure Meteorology
Contour Line (Isohypse) Line of equal elevation Cartography, Surveying, Geography
Isoevaporate Line of equal evaporation Hydrology, Meteorology

Additional Information: Using Isohyetal Maps

Isohyetal maps are essential tools in water resource management and climate studies. They are constructed by plotting rainfall data from various rain gauge stations on a map and then drawing lines connecting points of equal rainfall. The process often involves interpolation between stations.

  • They help visualize rainfall distribution over an area.
  • They are used to calculate the average precipitation over a drainage basin, which is crucial for hydrological modeling and flood forecasting. The Isohyetal method is considered more accurate than simpler methods like the arithmetic mean method or the Thiessen polygon method when rainfall distribution is uneven.
  • Changes in isohyets over time can indicate shifts in climate patterns.

Understanding isohyets is fundamental for anyone studying weather patterns, water resources, or environmental science.

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Important Questions from Precipitation

  1. Penman's equation is based on:
  2. Which of the following is a non-recording rain gauge?

  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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