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Question

A contour of constant rainfall is known as

The correct answer is isohyet

Understanding Contour Lines in Meteorology and Geography

Contour lines are fundamental tools used in various fields like geography, meteorology, and cartography to represent spatial variations of a specific variable. These lines connect points that have the same value of the variable being mapped.

The question asks for the specific term used for a contour line that connects points of constant rainfall. Let's look at the options provided:

Analyzing the Options for Constant Rainfall Contour

  • Isopleth: This is a very general term for a line connecting points of equal value for any variable on a map. While an isohyet is a type of isopleth, 'isopleth' itself is not the specific term for constant rainfall.
  • Isochrone: This term is used for a line connecting points that are equidistant in time or represent equal travel time from a specific point. It is not related to rainfall.
  • Isopluvial: This term is related to rainfall ('pluvial' refers to rain). It is sometimes used synonymously with isohyet or specifically for lines of equal rainfall depth. However, 'isohyet' is the more commonly accepted and widely used term for contour lines of constant rainfall amount.
  • Isohyet: This term comes from the Greek words 'isos' (equal) and 'hyetos' (rain). An isohyet is specifically defined as a line on a map connecting points that receive equal amounts of rainfall over a given period (e.g., a storm event, a day, a year). This perfectly matches the description in the question.

What is an Isohyet?

An isohyet is a type of isoline (a line connecting points of equal value) used on maps to show the geographical distribution of rainfall. By drawing isohyets, meteorologists and hydrologists can visualize areas that received similar amounts of precipitation. The spacing between isohyets indicates the rainfall gradient – closer lines mean a rapid change in rainfall amount over distance, while widely spaced lines indicate a more gradual change.

Isohyetal maps are crucial for various applications, including:

  • Water resource management
  • Flood prediction and analysis
  • Agricultural planning
  • Climate studies

Comparing Related Terms

It's helpful to understand other common isolines found on maps:

Term Connects Points of Equal...
Isohyet Rainfall
Isobar Atmospheric Pressure
Isotherm Temperature
Isobat Water Depth (Bathymetry)
Isohypse (or Contour Line) Elevation above sea level
Isochrone Time (e.g., travel time)

Based on the definitions, the contour of constant rainfall is correctly known as an isohyet.

Revision Table: Key Contour Lines

Term Represents Constant Value of Related Field
Isohyet Rainfall Amount Meteorology, Hydrology
Isobar Atmospheric Pressure Meteorology
Isotherm Temperature Meteorology, Climatology
Isohypse Elevation Topography, Cartography

Additional Information on Isohyetal Mapping

Isohyetal mapping is a method used to estimate the average rainfall over a specific area. This method involves drawing isohyets on a map based on rainfall data collected from various rain gauges within and around the area. The area between two consecutive isohyets is considered to have received rainfall that is the average of the values of the two bounding isohyets.

Steps typically involved in creating an isohyetal map:

  1. Plot the locations of rain gauges on a map.
  2. Write the recorded rainfall amounts next to each gauge location.
  3. Interpolate between the points to draw lines connecting points of equal rainfall, much like drawing contour lines for elevation.
  4. Label each isohyet with its corresponding rainfall value.

This technique provides a visual representation of rainfall distribution and helps in calculating the total volume of water received over a region, which is vital for hydrological studies and water resource planning.

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Important Questions from Infiltration

  1. Lysimeter is used to measure

  2. The rain waterholes in the parapet or in edging is called as

  3. Calculate the evaporation (mm) from a pond, if the pan evaporation is 45 mm. The pan coefficient is 0.70.

  4. For a large catchment, contours joining points of equal monthly rainfall values were plotted. The plot is known as:

  5. Which type of drainage system will collect the rainwater?

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