rainfall figure - translation to English
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rainfall figure - translation to English

MATHEMATICAL MODEL
Rainfall-runoff; Rainfall runoff conversion; Rainfall-runoff relations; Rainfall-runoff model; Runoff hydrograph; Rainfall runoff model; Reservoir hydrograph; Reservoir runoff model; Runoff reservoir model; Rainfall runoff relation; Rainfall runoff relationship; Rainfall-runoff relation; Rainfall-runoff relationship; Rainfall runoff relations; Surface water recharge; Rainfall runoff transformation; Runoff model; Rainfall- runoff; Surface runoff model; RainOff model; Recharge (hydrology)
  • Figure 1. A linear reservoir
  • Figure 2. A non-linear reservoir
  • Figure 4. Actual and simulated discharge, Rogbom valley
  • Figure 6. Non-linear reservoir with pre-reservoir for recharge
  • Figure 5. Rainfall and recharge, Rogbom valley
  • Figure 7. Runoff from the water balance
  • The Nash Model uses a cascade of linear reservoirs to predict streamflow. Software for this model exists.<ref>Software description for the Nash cascade hydrological model. On line: [https://www.waterlog.info/nashmod.htm].</ref>

rainfall figure      
(n.) = índice de precipitación
Ex: The lower monthly rainfall figures for July are made much worse by the incidence of strong westerly winds causing high evaporation rates.
rainfall         
  • Standard rain gauge
  • Black Rain Clouds
  • Rainfall distribution by month in [[Cairns]] showing the extent of the wet season at that location
  • NASA]]
  • rain dance]] being performed in [[Harar]], [[Ethiopia]]
  • Rainfall estimates for southern Japan and the surrounding region from 20 to 27 July 2009.
  • Convective precipitation
  • Heavy rain in [[Zapopan]]
  • Long-term mean precipitation by month
  • Rain, depicted in the 1493 ''[[Nuremberg Chronicle]]''
  • Sources of acid rain
  • Twenty-four-hour rainfall accumulation on the Val d'Irène radar in Eastern Canada. Zones without data in the east and southwest are caused by beam blocking from mountains. (Source: Environment Canada)
  • Rain falling on a road
  • The shape of raindrops depending upon their size
  • Streets in [[Tampere]], [[Finland]] watered by night rain.
  • Example of a five-day rainfall forecast from the [[Hydrometeorological Prediction Center]]
  • Orographic precipitation
  • Band of thunderstorms seen on a [[weather radar]] display
  • Isolated towering vertical desert shower
  • Rain falling on a field, in southern [[Estonia]]
  • A raindrop on a leaf
  • }
LIQUID WATER IN THE FORM OF DROPLETS THAT HAVE CONDENSED FROM ATMOSPHERIC WATER VAPOR AND THEN PRECIPITATED
Rainfall; Rainstorm; Rain storm; Rained; Rainwater; Raining; Heavy rain (meteorology); Hyetal; ⛆; Rainy; Rainiest; Rain measurement; Rain water; Wettest spot on Earth; Pluviophile; 🌧; Torrential rain; 🌦; Wettest places on Earth; Rainfall intensity; Rain rate; Rainfall rate; Millimetre of rain
(n.) = lluvia, precipitaciones
Ex: This will help scientists expand their understanding of erosion, deforestation and desertification, and whether there have been any shifts in rainfall levels and shoreline changes.
----
* rainfall figure = índice de precipitación
figure of speech         
INTENTIONAL DEVIATION FROM ORDINARY (LITERAL) LANGUAGE, CHOSEN TO PRODUCE A RHETORICAL EFFECT OR FOR OTHER PURPOSES, SUCH AS METAPHOR, METONYMY, SYNECDOCHE, PERSONIFICATION OR SIMILE
Figures of speech; Figure of Speech; Figurative Speech; Language techniques; Forms of speech; Figurative speech
(n.) = figura retórica, metáfora
Ex: The same spelling may arise by a figure of speech such as metonymy or synecdoche, in which we use part of a description to mean the whole = La misma ortografía puede ocurrir en las figuras retóricas como, por ejemplo, la metonimia o el sinécdoque, en donde utilizamos parte de una descripción para referirnos al todo.

Definition

red-figure
¦ noun a type of ancient Greek pottery in which the background is painted black, leaving figures in the red colour of the clay. Compare with black-figure.

Wikipedia

Runoff model (reservoir)

A runoff model or rainfall-runoff model describes how rainfall is converted into runoff in a drainage basin (catchment area or watershed). More precisely, it produces a surface runoff hydrograph in response to a rainfall event, represented by and input as a hyetograph. Rainfall-runoff models need to be calibrated before they can be used.

A well known runoff model is the linear reservoir, but in practice it has limited applicability. The runoff model with a non-linear reservoir is more universally applicable, but still it holds only for catchments whose surface area is limited by the condition that the rainfall can be considered more or less uniformly distributed over the area. The maximum size of the watershed then depends on the rainfall characteristics of the region. When the study area is too large, it can be divided into sub-catchments and the various runoff hydrographs may be combined using flood routing techniques.