A contour of constant rainfall is known as
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:
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:
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.
| Term | Represents Constant Value of | Related Field |
|---|---|---|
| Isohyet | Rainfall Amount | Meteorology, Hydrology |
| Isobar | Atmospheric Pressure | Meteorology |
| Isotherm | Temperature | Meteorology, Climatology |
| Isohypse | Elevation | Topography, Cartography |
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:
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.
Lysimeter is used to measure
The rain waterholes in the parapet or in edging is called as
Calculate the evaporation (mm) from a pond, if the pan evaporation is 45 mm. The pan coefficient is 0.70.
For a large catchment, contours joining points of equal monthly rainfall values were plotted. The plot is known as:
Which type of drainage system will collect the rainwater?